Digitized by tine Internet Arcinive in 2007 with funding from IVIicrosoft Corporation http://www.archive.org/details/elementsofphysicOOcolericli 0^xi-eii£.^l-^^>.t.-'^^.-^^ ^-t^c>^3^^^ ^^ .). The water does not rise to fill the 3 4 Matter and Force tumbler, being prevented from doing so by the confined air ; but, when the tumbler is slowly inclined, the air escapes in a succes- sion of bubbles, and water enters at the same time to take its place. The experiment shows that a body of air confined in any space tends to keep other bodies out of that space ; and this is true of all gases. But it is well known that, after a bicycle tire is fully inflated, much air must still be pumped in to make it hard. Now air can be forced into the fully inflated tire only by compressing the air already in it into a smaller space ; and experience teaches that the compression of the confined air can be carried just as far as the strength of the tire or of the operator will permit. The great compressibility of air can also be shown by a simple experi- ment with a bicycle pump or other compression pump. The piston can be pushed in a considerable distance although the confined air is prevented from escaping by closing the outlet with the finger. The force required to push the piston in rapidly increases, the farther the piston is pushed ; and, when it is re- leased, it is instantly pushed back by the expansion of the compressed air (Exp.). All gases are highly compressible and expansible, like air. When any quantity of gas, however small, is put into an otherwise empty space, it expands so as to fill the space completely. {^Experiments ivith air pump.) All liquids and most solids are only very slightly compressible. In fact, any change of volume with either increase or decrease of pressure upon them is so slight as commonly to elude observa- tion ; and, for all practical purposes, liquids are regarded as incompressible. Hence gases are distinguished from solids and liquids by their great compressibility and expansibility. Most gases are colorless and invisible, but not all. 6. Fluids. — Since the parts of both liquids and gases move over one another freely, or flow, they are both called fluids. The fluidity of gases is very easily illustrated with carbonic acid gas ; which will extinguish a lighted candle when poured upon it from a vessel {Exp.). Force and Inertia 5 7. Summary. — Solids have both definite form and volume, which they tend to preserve. Liquids have definite volume ; but have no form of their own, since their parts move readily over one another. Gases have neither definite form nor volume. They are highly compressible, and, with decrease of pressure, tend to expand indefinitely. II. Force and Inertia 8. Force. — The vf 0x6, force ^ as used in physics, means a push or a pull. The following are familiar examples of forces : the pull exerted by a horse upon a wagon ; the push or pull by which a door is opened or closed ; the very brief but strong push exerted by a hammer upon a nail in driving it ; the continuous pressure of a book lying upon a table ; the pressure of the table upon the book, by which the book is supported ; the pressure of a liquid against the bottom and sides of the containing vessel. 9. Inertia. — We learn from our daily experience that a body at rest remains at rest unless some other body exerts a force upon it, or, in other words, that a body cannot acquire motion without the action upon it of an applied force. For example, a ball is sent flying through the air by the push of the hand in throwing it or by a blow with a bat ; a high velocity is imparted to a rifle ball by the pressure of the gases from the powder exploded behind it ; and a loaded wagon is started by the pull exerted by the horses upon it through the traces. It is also a matter of common observation that moving bodies come to rest more or less slowly after the forces that start them cease to act. A book slides over a table when started with a sud- den push, but quickly stops ; a ball can be made to roll a long dis- tance over a smooth, level surface, as a sidewalk, but gradually loses speed till it comes to rest ; and a wagon goes only a short distance after the horses cease to pull. This behavior of moving bodies is not due to any tendency of the bodies 'themselves to come to rest, but is the effect of opposing forces developed by the rubbing of 6 Matter and Force surfaces as they move over one another. Such a force is called friction. Friction acts as a resistance to motion, and tends to bring moving bodies to rest. The smoother the surfaces are, the less friction becomes ; hence a body slides farther on a smooth surface than on a rough one. For example, after skaters are once in rapid motion, they can go a long distance without further effort, the friction between skates and smooth ice being very slight. Rolling friction is in general much less than sliding friction ; hence the use of wheels on vehicles of all sorts. Ball bearings reduce the friction still further by substituting rolling for sliding friction at the axle. Another hindrance to motion is the resistance of the air. This resistance is small upon a body moving slowly, but rapidly increases with the velocity. For high velocities, such as those of an express train or a rifle ball, it is very great. Bodies can, of course, be stopped by other forces than friction. The general truth illustrated by the above examples may be stated as follows : A body remains at rest or, if in motion, con- tinues with uniform motion in a straight line, unless it is compelled to do othenvise by forces acting upon it from without. This is true of all matter, solid, liquid, and gaseous; and the property of passiveness thus exhibited is known as the inertia of matter. The inertia of water can be shown by moving the hand quickly to and fro in a tub of water. A strong push must be exerted by the hand to impart motion to the water that is driven before it. The inertia of the air is similarly shown by moving a large fan rapidly to and fro, first flatwise, in the usual manner, then edge- wise. Comparatively little effort is required in the second case, as the fan cuts through the air, moving but little of it. (Try these experiments.) Force is also required to stop a body of air or water. The resistance offered by a house is sometimes insufficient to stop or turn aside the air that strikes it during a violent storm, and the house is blown down. Similarly, the inertia of a stream of water from a fire hose or even from a garden hose is shown by its power to break or overturn obstacles against which it is directed. Force and Inertia 7 10. Action of Forces with and without Contact : Weight. — All the forces considered in the preceding article are exerted by direct or indirect contact of the body exerting the force and the body upon which the force is exerted. Thus a horse in drawing a wagon pushes on the collar with his shoulders, and the collar pulls on the traces, and the traces pull on the wagon. Certain forces, however, act without visible or material connection between the bodies concerned. The forces exerted by a magnet are of this sort. Pieces of iron move toward a magnet from a greater or less distance, depending upon the size of the pieces and the strength of the magnet {Exp.). We know from the behavior of the iron that it is acted upon by a force whose direction is toward the magnet, although there is nothing whatever to show how this force is exerted. Similarly, the fact that a body falls unless supported indicates that it is acted upon by a force whose direction is vertically down- ward. This force is in some way due to the earth ; hence we think of the earth as exerting a pull or a/traction by which it tends to draw bodies toward its center. The attraction exerted by the earth upon any body is called the weight of the body.* 11. Balanced and Unbalanced Forces. — A force acting alone on a body always sets it in motion or changes its existing motion. A stone moving through the air with a moderate velocity is a good illustration ; for its weight is practically the only force acting on it, the resistance of the air being inappreciable. The weight of the stone causes a continuous decrease of velocity if the stone is rising vertically, a continuous increase of velocity if it is falling vertically, and a continuous change of direction if it is moving obliquely. Two or more forces acting on the same body at the same time may neutralize each other in such a way that the body remains at rest or, if moving, continues with uniform motion in a straight line. Forces so neutralizing each other are said to balance each other or 1 The weight of a body is very slightly less than the earth's attraction for^it, except at the poles, as explained in Art. 128. 8 Matter and Force to be /// equilibrium^ and are called balanced forces. The follow- ing are illustrations : A cart remains at rest when two boys pull equally on it in opposite directions. The weight of a body at rest or in motion on a level surface is balanced by the upward pressure of the surface ; the weight of a body suspended by a cord is balanced by the upward pull of the cord. In both cases the sustaining force is equal and opposite to the weight of the body. These examples illustrate the simplest case of balanced forces : namely, that of two equal forces acting in opposite di- rections along the same line. An example of three forces in equi- librium is illustrated in Fig. i. A body is supported by two cords. Each cord pulls obliquely upward upon the body, and the two forces together balance the weight of the body. A single force acting on a body is always unbalanced ; two or more forces acting together may be either balanced or unbalanced. The study of balanced forces acting on bodies at rest and of both balanced and unbalanced forces acting on bodies in motion con- stitutes the greater part of the subject-matter of mechanics, and is continued in the following chapters. 12. The Mutual Action of Two Bodies. — Whenever one body exerts a force upon another, the second body exerts at the same time an equal and opposite force upon the first. This opposite action of two bodies upon each other is often evident from the effects produced upon the bodies. For example, when one mar- ble strikes another, the latter is set in motion, and, at the same time, the motion of the first marble is stopped or checked by the opposite force exerted upon it by the other marble. The mutual action between a ball and a bat is a similar case. When a bullet strikes a board, the force that it exerts makes a hole in the board ; the equal and opposite force exerted by the board stops the bullet. The equality of the force exerted by each of two bodies on the other can be illustrated by two hardwood or ivory balls of equal Force and Inertia size, suspended as shown in Fig. 2. One of the balls is drawn aside and released. It falls, strikes the other ball, and instantly stops ; while the other swings out as far (or very nearly as far) as the first ball would have gone if its motion had not been hindered. Since the balls are ex- actly alike and the one loses as much motion as the other gains, it follows that the forces which they exert upon each other are equal {Exp.). The forces exerted between two bodies at rest are also equal and opposite. Thus, when the hand is pressed against a wall, the wall exerts an equal pressure on the hand. A book lying on a table exerts a downward pressure equal to its weight ; the resistance offered by the table acts as an equal upward pressure on the book. To distinguish between the action of one body on another and the action of the second body on the first, one is called the " action " and the other the " reaction." Either may be called the action, and the other will then be referred to as the reaction ; but, if one of the bodies is at rest and the other in motion before their mutual action, it is customary to say that the moving body acts on the one at rest and that the latter reads on the former. Fig. 2. PROBLEMS 1. Describe and account for the motion of the occupants when a carriage is started or stopped very suddenly. 2. In what direction is an inexperienced person likely to fall on alighting from a rapidly moving car ? Why ? 3. What forces are acting on a wagon when drawn at a uniform rate on a level road ? Are they balanced or unbalanced ? 4. What balanced forces are acting on a stone when at rest on the ground? 5. A boy exerts a lifting force of 75 lb. on a stone weighing 200 lb. (a) Is this a balanced or an unbalanced force ? {b) What balanced forces are acting on the stone ? • lo Matter and Force 6. Is it the forces exerted by or upon a body that affect its state of rest or motion ? 7. Account for the " kick " or recoil of a gun. 8. Why cannot a boy lift himself by standing in a tub and pulling on the handles ? III. Measurement 13. Measurement and Units of Measurement. — Experimental work ill physics consists largely in measuring the different kinds of physical quantities, as length, surface, volume, force, velocity, mass, etc. A quantity of any kind is measured by finding how many times it contains a certain fixed amount of that kind of quantity. This fixed amount is called a /////// and there are various units in common use for measuring each kind of quantity. Thus there are many units of length, among which are the inch, foot, meter, and centimeter. The amount of any quantity is expressed by naming the unit in which it is measured, preceded by the number of times it con- tains this unit, — as a volume of 3.7 cu. in. The name of the unit in which a physical quantity is measured should not be omitted either in oral or written statement. On account of the great simplicity of the metric system of meas- ures, it is almost exclusively used by scientists ; and it is the only one that we need consider here. 14. Extension. — Extension is that property of matter by virtue of which it occupies space, or has length, width, and thickness. The amount of space occupied by any portion of matter is called its size, hulk, or volume. 15. Units of Extension. — The fundamental unit of length in the metric system is the meter. It is defined as the distance be- tween two lines on a certain metallic rod preserved in the archives of the International Metric Commission at Paris. It was origi- nally intended to be one ten-millionth of the distance on the earth's surface from the pole to the equator ; but it is not exactly this fraction. The meter is now an arbitrary standard, just as the Measurement 1 1 yard is. Its advantage over the latter unit lies in the fact that its subdivisions are decimal fractions. (See Table I of the Appendix.) A decimeter (dm.) is a tenth of a meter (m.), a centimeter (cm.) is a hundredth of a meter, and a millimeter (mm.) is a thousandth of a meter. The centimeter is the customary unit of length for scientific purposes, and is the only one that the pupil will ordina- rily use in the laboratory. Thus a length of 3 dm. 5 cm. 7.5 mm. is written 35.75 cm. It will be useful to remember that the meter is equal to 39.37 inches, and the inch very approximately to 2.5 cm. (See Table II of the Appendix for exact relative values of the English and metric units.) The square centimeter (scm.) and the cubic centimeter (ccm.) are the customary units of surface and volume respectively. Since a square decimeter (sdm.) is 10 cm. in length and in width, it con- tains 100 scm. ; and since a cubic decimeter (cdm.) is 10 cm. in each of its three dimensions, it contains 1000 ccm. A cubic deci- meter, when used as the unit of liquid measure, is called a liter. It is slightly greater than a quart. 16. Weight. — The weight of a body (Art. 10) is constant at any one place on the earth, but decreases slightly with increase of alti- tude above the general level of the earth (as when a body is carried up a mountain or up in a balloon) and also with increase of depth below the surface (as when a body is taken down into a mine). A body at the earth's center would have no weight, being attracted equally in all directions by the earth. Weight also varies slightly with latitude, increasing continuously upon any body as it is taken from the equator toward either pole. The reasons for these variations in weight will be considered later. 17. Mass. — If any two bodies at the same place have equal weight, they are said to contain equal quantities of matter^ or to have equal mass. Using the term " quantity of matter " in this sense, the mass of a body may be defined as the quantity of matter in it. Although the weight of a body is affected by change of lati- tude or altitude, its mass is not. A body would contain identically 12 Matter and Force the same matter, and would therefore have the same mass, if it were transported to some region in space where it would be free from the attraction of the earth on any other body, or to the sun, where its weight (the sun's attraction) would be nearly twenty-eight times as great as upon the earth. 18. Units of Mass and of Force. — The mass of a cubic centi- meter of distilled water at the temperature of its greatest density (4° Centigrade) was originally taken as the fundamental unit of mass in the metric system, and is called the gram. As in the case of the meter, the gram is now defined with reference to a standard kept at Paris ; but for the purposes of elementary physics the above definition is the only one of importance. The mass of a cubic centimeter of water pure enough for domestic use, either cold or tepid, differs so little from one gram that the difference may always be disregarded in elementary physics. The earth's attraction for the unit of mass affords a very con- venient unit of force. From what has been said concerning the variation of weight, it is evident that such a unit of force differs appreciably at different latitudes ; but the variation is so slight as not to be a matter of practical importance. The unit of mass and the corresponding unit of force have the same name. Thus any force equal to the earth's attraction for a mass of 7 g. would be called a force of 7 g. To distin- guish between the units, they are sometimes called the gram mass and the gram iveight respectively ; but it is always possible to de- termine from the context whether mass or force is intended. In the English system the pound mass and the pound weight are the fundamental units of mass and force respectively. 19. Measurement of Mass (Weighing). — The equal attraction of the earth for equal masses at the same place is utilized in deter- mining the equality of two masses by the familiar process of weigh- ing with an equal-arm balance (Fig. 3). The horizontal bar of the balance is called the beam, and either half of it is called an arm. When equal pressures are exerted upon the two pans, the beam Measurement 13 Fig. 3. comes to rest in a horizontal position. Hence, when the beam assumes this position under the pres- sure of bodies in the two pans, these bodies have equal mass. The reason- ing is as follows : — (i) The balancing of the beam in- dicates equal pressures upon the pans. (2) Since the bodies exert equal pressures, they have equal weight; that is, the earth attracts them equally. (3) Since the bodies have equal weight, they have equal mass. The mass of a body is therefore found by placing it in one pan and balancing it with standard masses in the other. This process is called weighing, and the quantity found is commonly called the weight of the body. The standard masses are called weights. 20. Density. — The density of a substance is the mass of a unit volume of the substance. In the metric system it is usually ex- pressed as the number of grams in a cubic centimeter of it (g. per ccm.) ; in the English system, as the number of pounds in a cubic foot of it (lb. per cu. ft.). The density of any substance is found by measuring the mass and the volume of any convenient portion of it, and computing from these measurements the mass of one cubic centimeter. Laboraioty Exercises J and 2. PROBLEMS 1. Would the " weight " of a body, as determined with an equal-arm bal- ance^ differ in different latitudes and at different altitudes? Give the reason for your answer. 2. Is the density of a body affected by its latitude or its altitude ? 3. Is a pound of iron heavier than a pound of wood ? What is implied in the statement that " iron is heavier than wood "? Show that the statement " iron is denser than wood " leaves nothing to be implied. The more definite form of statement is to be preferred. 1 Cl 14 Matter and Force 4. The volume of a stone is 630 ccm.; its mass is 1575 g. Find its den- sity. 5. WTiat is the volume of 1000 g. of mercury ? of icxx) g. of brass ? of 1000 g. of aluminum ? (See table of densities in the Appendix.) 6. What is the mass of i cdm. of lead ? of i cdm. of marble ? 7. Find the densities of water, quartz, and gold in pounds, per cubic foot, from the densities in grams per cubic centimeter given in the table. (See also the table of equivalents in the Appendix.) 8. The density of (luartz is how many times that of water in the metric system ? in the English system ? How do these answers compare ? "Why ? 9. From the known densities of ice and water, show whether water ex- pands or contracts in freezing. CHAPTER II THE MECHANICS OP LIQUIDS I. Pressure produced in Liquids by their Weight 21 o Transmission of Pressure. — Suppose a number of books to be placed in a pile, one above the other. Beginning at the top, the first book presses upon the second with a force equal to its weight. The second book transmits this pressure to the third, and adds to it a pressure equal to its own weight. Hence the third book sustains a pressure equal to the weight of the first two books. Similarly, the third book exerts a pressure upon the fourth equal to its own weight plus that of the books above it, and so on to the last, the pressure of which upon the table is equal to the combined weight of all. The entire pile is supported by the up- ward pressure of the table, which is equal to the pressure of the bottom book upon it (equal action and reaction) ; and any por- tion of the pile, beginning at the top, is supported by the upward pressure of the book next below. If we consider the leaves of each book separately, instead of the book as a whole, we have an illustration of pressure due to weight, increasing regularly and continuously from top to bottom and exerted vertically up and down, the upward and downward pressures at any depth being exactly equal. The weight of a pile of shot causes each shot to crowd in be- tween its neighbors, thus exerting a pressure sideways as well as upward and downward, as is shown by the tendency of the pile to spread outward at the bottom. To make the sides of the pile vertical, supporting surfaces must be provided to sustain the lateral pressure. 15 \ u 1 6 The Mechanics of Liquids Similarly, the weight of a liquid causes lateral and oblique as well as vertical pressures within it. These pressures are more fully developed in liquids than in a pile of shot, for the particles of a liquid are free to move over one another, while in shot there is considerable friction. Hence shot remains in a sloping pile, and liquids do not. 22. Pressure in Liquids due to Weight. — The pressure produced within a liquid by its weight can be studied experimentally with various forms of apparatus. Cilass tubes of small diameter and equal length (about 60 cm.), closed air-tight at the top and shaped at the lower end as shown in Fig. 4, serve very well for the purpose of illustration, but are not adapted to exact meas- urement. When one of the tubes is lowered into a tall glass jar filled with water, the water enters its lower end a short distance. This is due to the compression of the confined air by the pressure Fig. 4. that the water exerts upon it. The distance to which the water enters the tube increases as the tube is lowered, showing that the pressure increases with the depth {Exp.). This is due to the fact that the pressure at any depth is caused by the weight of the water above that level. When the different tubes are inserted to the same depth, the water enters an equal distance in all, showing that the pressure of the water at a given depth is the same in the various directions in which it enters the tubes {Exp.), Since each particle of water is free to move in any direction, it would not remain at rest if it were not pressed upon equally from all sides. Laboratory Exercise j". 23. Laws of Liquid Pressure. — The facts concerning pressure in liquids at rest are found by accurate measurement to be as follows : — I. The pressure at any point in a liquid at rest is equal in all directions. II. The pressure of a liquid at rest is perpendicular to any surface upon which it acts. Pressure in Liquids 17 III. At any point ill a liquid^ the pressure due to its weight is proportional to the depth of the point below the free surf ace of the liquid. IV. The pressure is the same at all points in the same horizontal plane. V. At the sattie depth in different liquids, the pressure due to weight is proportional to the density of the liquid. These statements are known as the laws ^ of liquid pressure. The first two hold for all pressures in liquids at rest, whether due to their weight or to applied pressure, i.e. to pressure exerted upon them in closed vessels. As stated in the preceding article, the first law is a consequence of the freedom of movement of the particles of a liquid. This is true of the second law ; for, if a liquid pressed obliquely against a surface, it would move along the surface instead of remaining at rest. The reasons for the other laws are considered in the following articles. 24. Intensity of Pressure. — The pressure at any point in a liquicj is defined as the pressure that the liquid would exert upon a hori- zontal surface of ////// area at that depth in the liquid. The pres- sure upon each unit area of a surface is sometimes called the intensity of pressure or the rate of pressure to distinguish it from the /^/^/ pressure on the surface. Pres- sure (/.ecific gravity of the liquid ? 8. A body weighs 300 g. in air and 140 g. in alcohol, the specific gravity of which is .82. What is the volume of the body ? 9. Find the specific gravity of a litjuid from the following : — Weight of bottle = 40 g. Weight of Iwttle filled with water = 120 g. Weight of bottle filled with the licjuid = 150 g. 10. A piece of iron weighs 1000 g. ; its specific gravity is 7.2. What will it weigh in water ? 1 1. A stone weighs 25 lb. in air and 16 lb. in water. What is its spe- cific gravity ? 12. Find the weight of a cubic foot of lead from its specific gravity. CHAPTER III THE MECHANICS OP GASES I. Atmospheric Pressure 37. Weight of Air. — A vessel full of air is appreciably heavier than the same vessel after the air has been partially removed by means of an air pump {Exp.). The difference, although small, is very noticeable if the vessel is of considerable size (a liter or more) and the weighing is done on a sensitive balance. This proves that air has weight. By accurate measurement (the neces- sary allowance being made for the portion of the air remaining after exhaustion), the weight of a liter of air at ordinary tempera- tures is found to be very nearly 1.2 g. ( = .0012 g. per ccm.). 38. Pressure of the Atmosphere. — The weight of the atmos- phere causes it to exert pressure, since each horizontal layer sus- tains the weight of all the air above it and adds its own weight to the pressure transmitted to the next lower layer. It is a curious fact that, although the pressure of the atmosphere amounts to a total of about 35,000 pounds on a person of average size, we are unconscious of its existence under the ordinary circumstances of life. The existence of atmospheric pressure is proved by the following experiments. 39. Experiments proving the Existence of Atmospheric Pres- sure. — A sheet of thin rubber is tied over the top of an open receiver of an air pump (Fig. 17). As the air is exhausted from the receiver, the rub- ber is depressed more and more, and soon bursts with a loud report, caused by the sudden entrance of the air 3» 32 The Mechanics of Gases {Exp.). Before the air is exhausted, it exerts a pressure equal to that of the outside air, and the rubber remains flat. With each stroke of the pump some air is removed, and the pressure of the remaining air is correspondingly diminished. The rubber is therefore pushed inward by the greater pressure of the atmosphere. If the hand be placed over the receiver instead of the rubber, it can be removed only with difficulty after a few strokes of the pump, so firmly will it be held in place by the pressure of the air {Exp.). The flesh of the pahii will be distended into the re- ceiver, and will seem to be pulled in. This sensation is entirely deceptive ; the flesh is pushed in by the pressure of the liquids and gases within the body. Since the pressure within the body sustains and balances the pressure of the atmosphere, the two must be equal. Hence, when the external pressure upon any part of the body is diminished, that part will be distended by the greater pressure from within. Two hollow brass hemispheres (Fig. i8), fitting air-tight, can easily be pulled apart so long as none of the air has been removed from the space they inclose ; but after a considerable portion of this air has rated only with great difficulty (/t;f/.). Before the air is exhausted the pres- FiG. 18. sure from within is equal to that without and balances it; hence the hemispheres are separated without hindrance from atmospheric pressure. The removal of a portion of the air diminishes the pres- sure from within proportionally, and the pressure upon the outside pushes the hemispheres together with great force. This apparatus was invented about the middle of the seventeenth century by Otto von Guericke, burgomaster of Magdeburg, Germany. The large copper globe that he used for the first trial was not strong enough to withstand the great pressure upon it, and suddenly collapsed with a loud report, terrifying all the spectators. The apparatus is still known as the Magdeburg hemispheres. '^1^ Atmospheric Pressure 33 40. Laws of Gas Pressure. — Pascal's law (Art. 28) holds for gases as well as for liquids, and for the same reason — their mobility. The equal pressure of the atmosphere in all direc- tions can be shown with the apparatus represented in Fig. 19. Thin sheet rubber is fastened over the large end of a thistle tube, and a rubber tube is attached to the other end. On exhausting some of the air with the mouth, the rubber is pushed in by atmos- pheric pressure ; and, for a given exhaustion of the tube, the depression of the rubber remains the same in whatever direction the tube is turned. The law of proportionality between depth and pressure (Law III, Art. 23) does not hold for the atmosphere, since its density increases rapidly with the depth, gases being very compressible. The height to which the atmosphere extends is unknown, but is variously estimated at from one hundred to two hundred miles. It is known to extend above fifty miles ; yet the density decreases so rapidly with increase of altitude that the pressure at a height of 3.4 miles is only one half as great as at sea level. From this we know that one half of the atmosphere lies below an elevation of 3.4 miles above sea level. Men have ascended to higher altitudes than this upon moun- tains and in balloons. If the atmosphere were of the same density throughout as at sea-level, it would extend only to a height of about five miles. 41. Measurement of Atmospheric Pressure. — Figure 20 represents a tall U-tube about half full of mercury. The mercury stands at the same level in the two arms under the action of its weight and the equal pressure of the air upon its two surfaces. If a rubber tube be attached to one arm and some of the air exhausted by means of an air pump or by applying the mouth, the pressure in that arm will be diminished and the greater pressure of the atmosphere in the open arm will force the mercury down in 34 The -Mechanics of Gases Fig. ai. that arm and up in the other until equilibrium is restored ^^^^ (Fig. 2i) {£x/>.). When the mercury comes to ^rTfl rest, the portion of it below the level ac is in m * equilibrium under the action of the downward m pressure of the atmosphere on the surface a and ■ the equal downward pressure at c. This pressure I at r is the transmitted pressure of the air remain- ■ ing above d, increased by the pressure due to the weight of the mercury column //c. Hence the pressure due to the weight of the column measures the difference between the pressure of the atmos- phere and the pressure of the air remaining in the closed arm. For example, when the dilference of level of the two surfaces is lo cm., the pressure of the atmosphere exceeds the pressure in the closed arm by lo x 13.6 or 136 g. per scm. If all the air were removed from the closed arm, there would be no pressure upon the surface of the mercury in it ; and the mercury would rise in this arm until the pressure at r, due to the weight of the column /fc, was equal to the J pressure of the atmosphere. This important fact is util- ized in the mercury barometer, an instrument for measur- ing atmospheric pressure. Figure 22 represents a siphon barometer, so called from its shape. The straight part of the tube is 80 cm. or more in length and its upper end is sealed. It is first completely filled with mercury so as to expel all the air. When turned into an upright position, the mercury falls until it reaches a position of equilibrium, leaving an empty space {vacuum) at the top. The differ- ence of level of the columns, he, is called the hei^t^ht of the barometer. This height multiplied by the density of mercury measures the pressure (per scm.) of the column at c ; and consequently measures the equal pressure of the atmosphere. Thus, when the height of the barometer is 76 cm., the atmospheric pressure is 76 x 13.596, or 1033.3 g. per scm. y Fig. 22. Atmospheric Pressure 35 ^Z' \ Another form of barometer is represented in Fig. straight tube about 85 cm. in lenglh and closed at one end, is completely filled with mercury, and, with a finger held tightly over the open end, is inverted, and the open end inserted in a cup of mercury. The height of the column is measured from the sur- face of the mercury in the cupt (Why ?) 9 ? J Atmospheric pressure is gener- ally expressed in terms of the height of the barometer, measured in centimeters or inches; as a pressure of 75.3 cm. {of mercury) is understood. The pressure of the atmosphere, in grams per l-i,: square centimeter, is equal to the weight of a vertical column of air one square centimeter in cross- section, extending from the place where the pressure is taken to the upper limit of the atmosphere. Laboratory Exercises JO and li. 42. The Barometer. — The barometer was invented by Evange- lista Torricelli (1608-1647), an Italian mathematician and scientist, in 1643, some years before Guericke's celebrated experiments at Magdeburg. The space above the mercury in a barometer is called a Torricellian vacuum in honor of the inventor. That the barometer column is sustained by the pressure of the atmosphere was conclusively proved by Pascal, under whose direc- tion the height of the barometer was determined at the foot and at the summit of Puy de Dome, a high mountain in France. The height of the mercury fell nearly 8 cm. during the ascent of about 900 m. The effect of decrease of atmospheric pressure upon the height of the barometer can be more conveniently shown by 23- 36 The Mechanics of Gases exhausting the air from a tall receiver under which a barometer tube has been placed. The mercury continues to fall as long as the process of exhaustion is continued {£xp.). Barometer tubes are mounted in a variety of ways, and pro- vided with scales and other devices for convenience and accuracy in reading. Before the tube is mounted, the mercury in it is boiled to expel all air and moisture. 43. Uses of the Barometer. — It is a well-established fact that different conditions of the weather are accompanied or preceded, with considerable regularity, by certain changes of atmospheric pressure, as determined by the height of the barometer. (Gener- ally speaking, the barometer is low in stormy weather and high in clear weather ; hence the approach of a storm is indicated by a fall, and the approach of Hiir weather by a rise, of the barometer. The difference between high and low barometer rarely exceeds two or three centimeters. This knowledge is used in predicting changes in the weather ; but the forecasts made by the Weather Bureau are based on other sources of information as well, including temperature, direction and velocity of the wind, the course and progress of storms up to the time when the forecast is made, and the existing state of the weather ; all of which are reported to the central office by the different stations distributed over the country. The problem of forecasting the weather is thus a very complex one. The barometer is also used for measuring altitudes. The change of pressure due to a given change of altitude being known, the height of a mountain can be computed from the reading of a barometer at its base and at its summit. The height to which a balloon ascends is determined in the same way. For moderate altitudes above sea level, it is approximately correct to compute the change of altitude at the rate of 900 ft. for a fall of the barometer of one inch. PROBLEMS 1. Explain the process of drinking through a straw. 2. When the mercury barometer stands at a height of 76 cm., what will Atmospheric Pressure 37 be the height of a barometer the liquid in which has a specific gravity of 1.6? 3. When the barometer stands at 76 cm., a hter of air at 0° C. weighs 1.293 g. At the same temperature and pressure, what will be the weight of the air in a room 9 m. by 7 m. and 4 m. high ? 4. Compute the weight of i cu. ft. of air at 0° C. and 76 cm. pressure (sp. gr. of air = .001293). 5. What weight of air at this temperature and pressure is contained in a room 20 by 30 ft., and 12 ft. high ? 6. In ascending a mountain will the fall of the barometer during each thousand feet of ascent be greater or less than for the preceding thousand feet? Why ? 7. (a) The weight of the atmosphere is equal to the weight of an ocean of mercury covering the entire surface of the earth to what depth ? (/v) What would be the depth of water covering the entire surface of the earth and having equal weight ? 8. The surface of the body of a man of medium size is about 16 sq. ft. Assuming this value and also that the pressure of the atmosphere is 14.7 lbs. per sq. in., compute the total pressure that a man sustains upon the surface of his body. II. Boyle's Law 44. The Elastic Force of Gases. — Let A (Fig. 24) represent any portion of the air. It may be thought of as distinct from the surrounding air, although no bounding sur- face actually exists. The surrounding air presses inward upon all sides of A, as indi- cated by the arrows pointing inward. These pressures are balanced at every point by an equal outward pressure exerted by A upon the surrounding air (equal action and reac- P^^' ^ tion). This pressure exerted by A is not the result of its weight, but of its tendency to expand; just as a com- pressed spiral spring or a compressed piece of rubber exerts an outward pressure that is independent of its weight. IVAy gases tend to expand is a question that will be considered later (Art. 182). The fact may be accepted for the present without explanation. The pressure (per unit area) exerted by any body of gas is 38 The Mechanics of Gases called its elastic force. The English physicist, Robert Boyle, who was among the first to study the mechanics of the air, called this elastic force the spring of the air. The appropriateness of the term will be evident if one suddenly pushes down the piston of a small compression pump (such as a bicycle pump), at the same time keeping the tube closed to prevent the escape of the air {Exp.), The pressure exerted by the confined air rapidly increases as the piston is pushed farther in, and this pushes the piston back again when it is released. In fact, the confined air acts as a spring would if put in its place. The experiment shows that the elastic force of a gas is increased by compression. At the same temperature and density, the elastic force of the air in a closed vessel is equal to that of the atmosphere. (Which of the preceding experiments of this chapter have shown this to be true?) 45. Measurement of the Elastic Force of Gases. — A pressure gauge, or manometer ^ is an instrument for measuring the elastic force of a gas in a closed space. An Open Manometer (Fig. 25) is commonly used for the meas- urement of pressures only slightly greater or less ^0j^ than one atmosphere. It consists essentially of a ^T glass U-tube partly filled with water or mercury, K t, with a rubber tube attached to one arm for mak- ■ ing connections, and a scale for measuring the height of the li(|uid in the two arms. On con- necting such a manometer with the gas pipes and turning on the gas, the liquid will be pushed down in the arm in which the gas is admitted. The pressure of the gas upon the surface a is equal to the pressure at the same level, c, in the other arm ; and the latter pressure is the sum of the atmospheric pressure upon d, and the pressure due to the weight of the column of liquid dc. Hence the pressure due to the weight of l>c meas- ures the dijference between the pressure of the gas and the pressure Fig. 25. Boyle's Law 39 of the atmosphere. For example, if the liquid in the manometer is water and the difference of level 8 cm., the pres- sure of the gas exceeds that of the air by 8 g. per scm. The Closed Manofneter. — A short siphon barom- eter with a rubber tube attached to the open arm (Fig. 26) is used to measure the pressure in partially exhausted vessels. Since there is no air or other gas in the closed arm, the mercury completely fills it when under atmospheric pressure. While the air or other gas is being pumped from a vessel to which a closed manometer is attached, the mercury continues to fill the closed arm for some time, if the original ^ pressure was more than sufficient to sustain the full height of the column. It is only after the mercury begins to fall that the difference of level of the columns measures the pressure. 46. Units for the Measurement of Pressure. — The pressure of gases may be measured in any of the following units : — In grams per square centimeter or pounds per square inch. In centimeters or inches of mercury or of water. In atmospheres. An atmosphere is the pressure of a column of mercury 76 cm. high. This unit is approximately the average pressure of the atmosphere at sea level. It is constant and is not to be confounded with the actual atmospheric pressure, which varies from day to day and is different at different altitudes. The pupil should be able to formulate rules for finding the value of a given pressure in each of these units when its value in terms of any one of them is known. 47. Boyle's Law. — The English physicist, Robert Boyle (1627- 1691), discovered a simple relation between the volume of a gas and the pressure upon it. This relation, known as Boyle's law, has been found to be approximately true for all gases. It is as follows : — The temperature remaining the same, the volume of a given body of gas varies inversely as the pressure upon it. For example, if the pressure upon any body of gas is doubled, 40 The Mechanics of Gases the volume of the gas will be decreased one half; or, if the pressure is reduced to one fifth of its original value, the volume will be- come five limes as great as at first. If the volume of a mass of gas is Kj when the pressure upon it is Pi (g. per scm.) and K when the pressure is F^y then, ac- cording to the law, /j : /^ : : K^ : l\. From this proportion we obuin Pxy\ = PiVt'i that is, at a constant temperature, the prod- uct of the volume of a given body of gas and the pressure upon it is constant. It has been found that Boyle's law is not perfectly exact for any gas ; but the departure from the law is so slight that it can be detected only by very accurate measurement, unless the pressure is so great that the gas is near the point of condensation. The law does not hold if the change of pressure is accompanied by a change of temperature ; for a rise of temperature will itself cause an increase of pressure or of volume {Exp,). Laboratory Exercise J J, 48. The Relation between the Density and the Pressure of a Gas. — It follows from lioyle's law that — The temperature remaining the same^ the density of a gas is pro- portional to the pressure upon it. Thus if the pressure upon a quantity of gas is increased three- fold, its volume will be one third as great as at first ; and, since the entire mass occupies one third its former volume, its density will be three times as great as at first. The increase of the elastic force of a gas with increase of density is well illustrated by the effect of the air in a bicycle tire. After the tire is fully inflated, a further supply of air causes a proportionate increase in its density; and, as is well known, this makes the tire " harder." Laboratory Exercise 14, PROBLEMS I. A cubical vessel 20 cm. in each dimension is full of air at a pressure of one atmosphere. What is the total pressure exerted by the confined air upon the walls of the vessel ? Applications of Atmospheric Pressure 41 2. Does the vessel support this pressure when it is surrounded by air under equal pressure ? 3. What would be the total pressure tending to burst the vessel if it were placed under a receiver from which half the air was exhausted (none of the air being removed from the vessel) ? 4. Find the weight of air contained in the vessel, assuming that its den- sity is .(X)i2 g. per ccm. 5. {a) At what depth in fresh water is the pressure due to its weight equal to one atmosphere ? {b) At what depth in salt water ? 6. From what depth in water must a bubble of gas start in order that its volume may be doubled on reaching the surface ? 7. {a) What is the pressure in pounds per square inch at a depth of 3 miles in the ocean ? {b) What is the total pressure at that depth upon a fish the surface of whose body has an area of 25 sq. in. ? 8. A cubic decimeter of gas is under a pressure of 100 cm. of mercury. What will be its volume at the same temperature under a pressure of 30 cm. of mercury ? 9. A liter of gas is taken under a pressure of one atmosphere. What will be its volume at the same temperature under a pressure of 100 cm. of mercury? 10. Two liters of gas under a pressure of one atmosjihere will have what volume when the pressure is reduced to 900 g. per scm. ? III. Applications of Atmospheric Pressure 49. The Air Pump. — A simple form of air pump is represented in Fig. 27. The pump consists of a metal cylinder in which fits an air-tight piston operated by the handle. There are two valves, a and bj the former in the piston and the latter at the entrance of the tube, at the bottom of the cylinder. The valves open in one direction only, as shown in the figure. The simplest form of valve consists of a piece of flexible leather, placed so as to cover the hole and fastened at one edge. The valve closes the opening air- tight when pressed against it, and leaves it open when pushed in the opposite direction. The pump is connected by a tube to an opening, (9, at the center of a flat metal plate, PQ, upon which stands a receiver, R. Suppose the piston to be at rest at the bottom of the cylinder. Both valves will be closed, being held down by their weight. 42 The Mechanics of Gases During the up stroke of the piston, the small amount of air beneath it expands and fills the increased space, and its pressure Fig. 27. decreases proportionally. The atmospheric pressure upon the top of valve a being now greater than the pressure from beneath, this valve is firmly closed. When the downward pressure upon d is sufficiently diminished, the pressure of the air in the tube beneath this valve lifts it, permitting some of the air in the receiver to escape into the space below the piston. As soon as the piston stops rising, the lower valve is closed by its own weight. On pushing the piston down, the air beneath it is compressed. This air cannot escape through the lower valve, since the increased pressure only closes this valve more tightly. When the amount of compression is such that the density of the confined air is slightly greater than that of the atmosphere, the upper valve is forced open, permitting the air to escape. These processes are repeated with every stroke of the piston, thus gradually removing the air from the receiver. The limit of Applications of Atmospheric Pressure 43 possible exhaustion is reached when the pressure of the air re- maining in the receiver is insufficient to Hft the lower valve, or when the quantity of air that enters the cylinder with the up stroke is so small that it cannot be compressed enough to raise the upper valve. Pumps for obtaining a more nearly perfect vacuum are pro- vided with metal valves or stoj)cocks, operated automatically by a simple mechanism attached to the piston or to the piston rod. 50. The Compression Pump. — If the valves of the pump repre- sented in Fig. 27 were made to open in the opposite direction, the pump, when operated, would force air into the receiver. A pump made to force air or any gas into a closed vessel is called a compression pump. A pump such as is represented in Fig. 28 may be used either for exhaust- ing or compressing gases. On operating the pump, air enters it through A and leaves it through C. Hence if a closed vessel be attached to C, air will be forced into it ; if attached to Ay the air will be exhausted from it. A bicycle pump is a compression pump of very simple construc- tion. It has but one valve, the entire piston serving this purpose. The valve in the tube of the bicycle tire takes the place of the outlet valve in the pump. (Examine a bicycle pump and explain its action.) A bellows is a form of compression pump. It is provided with two valves, a and b (Fig. 29), the former opening inward, the latter outward. (Explain its action.) Fig. 28. Fig. 29. 44 The Mechanics of Gases 51. The Lifting Pump. — The lifting or suction pumpy used for pumping water, is similar to an air pump in its construction and action. The valves open upward, as shown in the figure. A pipe extends from the cylinder or barrel of the pump to some distance below the surface of the water in the well or cistern. The piston is operated by means of a lever, called the handle. Starting with the pump " empty," it first acts as an air pump to exhaust the air from the pipe (see Art. 49). During this process the pressure of the air within the barrel and the pipe decreases and the greater pressure of the air upon the water in the well forces some of it up Fig. 30. Fig. 31. Fig. 32. into the pipe ; the pressure due to the weight of the column of water thus sustained being equal to the difference between the atmospheric pressure and the pressure of the air remaining in the pump. After the pump is filled with water, the water below the piston follows it during the up stroke, being pushed upward through the lower valve. When the piston begins to descend, the lower valve closes, preventing the return of the water into the pipe. The valve in the piston is forced open at the same time, and the water flows through it into the space above. At the beginning of the Applications of Atmospheric Pressure 45 up stroke, the valve in the piston falls and the water above it is lifted out. Since the entire pressure of the atmosphere can sustain a col- umn of water only to a height of about 10.3 m. (34 ft.), the lower valve would have to be within that distance of the water in the well even if the pump were capable of producing a perfect vacuum. The actual limit of distance is about 28 or 30 ft. 52. The Force Pump. — In the force pump the second valve is placed at the entrance to the discharge pipe, B (Fig. 32). There is no valve in the piston. The action of the pump during the up stroke of the piston is the same as in the lifting pump. (Which valve is open ? Which closed ?) With the down stroke of the piston the water is forced into the discharge pipe. The height to which water can be forced in the discharge pipe depends only upon the strength of the pump, being in no way affected by atmospheric pressure. Force pumps are generally provided with an air chamber, D, connected with the discharge pipe. During the down stroke of the piston the water is forced into the chamber, compressing the air above it. The elastic force of the compressed air maintains the flow from the air chamber during the up stroke of the piston, making the flow continuous. The force pump is used to force water to considerable heights, and to deliver it under great pres- sure, as in fire engines. 53. The Siphon. — A bent tube or pipe for transferring liquids over an elevation from a higher to a lower level is called a siphon (Fig. 33). Either a rigid or a flexible tube will serve the purpose. To start a small siphon, it may be held with the bend down and filled, then, with a finger over each end, inverted and placed in position ; or it may be placed in position and the air then exhausted by applying the mouth to the lower end. Siphons are generally provided with a suction tube for this purpose, so that the liquid will not flow into the mouth. 46 The Mechanics of Gases The liquid will continue to flow as long as one end of the siphon is covered by it, and the other end is below the level of its surface, />. below ab in the figure ; but if the outlet of the siphon is also immersed, the flow will cease as soon as the liquids in the two vessels reach the same level. To explain the action of the siphon we may suppose it to be stopped by closing the outlet, r, with the finger. The liquid will then be at rest, and the laws of pressure for liquids in equilibrium will hold. At points a and b in the tube, on a level with the sur- face of the liquid, the pressure is the same as that of the atmos- phere. The pressure at c is equal to this plus the pressure due to the weight of the liquid column be. Hence, when the finger is removed, this pressure of the column be acts as an unbalanced force u|X)n the liquid in the siphon, causing it to flow. The liquid is held in a continuous column by the pressure of the atmosphere, acting at the ends of the siphon ; otherwise the liquid would part at the top and run out at both ends, leaving the siphon empty. It is, in fact, the transmitted pressure of the atmosphere that forces the liquid up the short arm. Laboratory Rxereise 12. 64. Respiration. — In breathing, the size of the chest cavity is alternately increased and diminished by muscular action. The pressure of the air in the lungs causes them to expand so as always to fill the space afforded them ; hence, when the chest is raised and the diaphragm depressed in inhaling, the expansion of the air already in the lungs diminishes its pressure and more air is pushed into the lungs by the greater pressure of the outside air. The familiar expression " drawing in a breath " is misleading in that it implies a pulling force. When the chest is contracted in exhaling, the air in the lungs is compressed and some of it is forced out. 55. Buoyancy of the Air. — A body of considerable size and of small specific gravity weighs appreciably more under a partially exhausted receiver than it does in air. This fact may be illustrated with the apparatus shown in Fig. 34. A hollow globe, closed air- Applications of Atmospheric Pressure 47 FIG. 34. tight, is exactly balanced in air by a solid brass weight. When the apparatus is placed under the receiver of an air pump and the air exhausted, the globe descends, showing that it is now heavier than the weight {Exp.). The experiment proves that air exerts a buoyant force. The globe and the solid body have equal weight in air ; but the buoyant force of the air is greater upon the globe, since it is much the larger of the two. Hence, with partial exhaus- tion of the air in the receiver, there is greater loss of buoyancy upon the globe, and it therefore sinks. The law of buoyancy for gases is the same as for liquids and for the same reasons (Art. 31). The amount of the buoyant force of the air upon solids and liquids is relatively very small, and in the affairs of daily life may be disregarded.^ The true weight of a body is its weight in a vacuum ; its weight in air in called its apparent weight when it is necessary to distinguish between the two. The difference between the true and the apparent weight of a body is, of course, the buoyant force of the air upon it. The buoyant force of the air upon gases is relatively large. In fact, upon gases less dense than air it exceeds their true weight. Such a gas tends to rise, just as a cork does in water. The weight of a gas is always understood to mean its true weight. 56. The Balloon. — A balloon is sustained by the buoyant force of the air, the gas with which it is filled being lighter than air. Hydrogen is best adapted to the purpose, being the lightest of gases ; but illuminating gas is generally used, as it is cheaper and more easily obtained. Hot air was used in the balloons first in- 1 The buoyant force of the air upon i ksj. (i liter) of water is the weight of a liter of air, or about 1.2 g, ; upon i kg. of lead the buoyant force is about .1 g. 48 The Mechanics of Gases vented. A balloon will rise if the buoyant force upon it is greater than its true weight, including the weight of the gas with which it is filled and the weight of the car and its load. A balloon is not fully inflated at the start, space being left for the expansion of the gas as the atmospheric pressure upon it dimin- ishes during the ascent. As long as this ex- pansion continues, the buoyant force upon a balloon remains constant, for the increase in the volume of the displaced air offsets the de- crease in its density. As a balloon rises after becoming fully distended, the buoyant force decreases until it is no greater than the true weight of the balloon and all it carries. The balloon then ceases to rise, unless lightened by throwing out sand, a supply of which is carried for that purpose. When the aeronaut wishes to descend, he opens a valve at the top of the balloon and some of the gas escapes. Fig. 35. PROBLEMS 1. Orer how great an elevation can water be siphoned ? Why ? Over how great an elevation can mercury be siphoned ? Would a siphon work in a vacuum ? Explain. 2. (a) At ordinary temperatures and under a pressure of one atmosphere, a cubic meter of air weighs about 1.2 kg., a cubic meter of hydrogen about .083 kg., and a cubic meter of illuminating gas about .74 kg. Assuming these values, what is the buoyant force upon a balloon containing 500 cu. m. of hydrogen ? (d) How great a weight will this buoyant force sustain in addition to the weight of the hydrogen ? 3. With what volume of illuminating gas must a balloon be filled to rise, if the empty balloon, the car, and the occupants together weigh 500 kg. ? 4. Will the true weight of a body be greater or less than its weight in air when weighed on an equal-arm balance with brass weights (a) if the density of the body is the same as that of brass? (^) if its density is less? (<•) if its density is greater ? CHAPTER IV STATICS OP SOLIDS I. Concurrent Forces 57. Mechanics. — Mechanics is the branch of physics that treats of the action of forces upon bodies. It is divided into statics and dynamics or kinetics. Statics is the mechanics of balanced forces (Art. ii) ; it treats of the relations that must exist among the forces acting upon a body at rest in order that the body may remain at rest. The statics of fluids is the subject of the two preceding chapters. The subject of the present chapter is the statics of solids. Dynamics^ or kinetics, is the mechanics of unbalanced forces (Art. 1 1 ) ; it treats of the effects of unbalanced forces in produc- ing and changing motion. The dynamics of solids is the subject of the following chapter. 58. Equilibrium of Two Forces. — The relations that must exist among two or more forces in order that they may balance each other are called the conditions necessary for equilibriutn^ or, simply, the conditions of equilibrium. The conditions of equilibrium for two forces can be studied by means of two drawscales and a board supported upon three Fig. 36. marbles lying on a table (Fig. 36). Cords are attached to nails at A and B. Horizontal forces are applied to the board through 49 50 Statics of Solids these cords and are measured by the drawscales. If these forces are in equiUbrium with each other, the board will remain at rest ; if they are not in equilibrium, it will move, since the friction is inappreciable. By trial with the apparatus it will be found that : ( I ) When equal forces are applied in opposite directions but not along the same line, the board will not be in equilibrium, but will rotate until the lines of action of the forces coincide (Fig. 37). Fig. 37. The board will then be in equilibrium. (2) When the applied forces are opposite and have the same line of action, but are unequal, the board will be pulled in the direction of the greater force. (3) When the forces are either equal or unequal but not opposite in direction, the board will not be in equilibrium The experiment shows that fwo forces balance each other only when they are equal in magnitude^ opposite in direction^ and have the same line of action. A and B are the points of application of the forces respectively. A force produces the same effect when it is applied at any other point in the same line of action. Thus, if either of the equal and opposite forces be applied at C (Fig. 37) instead of at A or B, they will still be in equilibrium. 59. Elements of a Force. — The effect of a force depends upon its magnitude^ its direction, and \\.% point of application (or line of action) . These are called the elements of a force. They must all be considered in describing and comparing forces, and in discuss- ing their effects. 60. Representation of Forces. — In studying the relations of a set of forces to one another, it is often convenient to make use of >B Concurrent Forces 51 a diagram in which each force is represented by a line. The direction of the force is represented by the direction of the line, with an arrow- head placed on it ; the magnitude of the force, by the length of the line; and its point of application, by the point from which the line is drawn. The method is illustrated in Fig. 38, which represents two forces having a common point of application, O, and differing in direction by a right angle. The force represented by OB is twice as great as the other. The magnitude of a force can be represented on any scale desired. Thus i cm. may represent a force of 10 g., 100 g., 500 g., etc. But the same scale must be used for all forces in the same figure. 61. Resultant and Components. — In many cases where two or more forces act upon a body at the same time, a single force can be found which, acting alone, would produce the same effect upon the body as the given forces. This one force is called the result- ant of the forces to which it is equivalent, and the latter are called the cojnponetits {i.e. parts) of the resultant. The resultant of any number of forces acting along the same line in the same direction is their sum. Thus, if a boy pulls on a cart with a force of 15 lb., and another boy pulls with him, exerting a force of 25 lb., the effect upon the cart will be the same as that of a single force of 40 lb. acting in the same direction. The resultant of two forces acting in opposite directions along the same line is their difference, and its direction is that of the greater component. The resultant of two equal forces acting in opposite directions along the same line is zero, since the two forces exactly neutralize each other (Art. 58). The resultant of any set of balanced forces is zero, for the same reason. The process of finding the resultant of two or more given forces is called the composition of forces. In the case of forces acting along the same line, composition is effected by adding all the forces that act in one direction, and subtracting all that act in the oppo- 52 Statics of Solids site direction. Other methods are required for forces acting at an angle or along different parallel lines, as shown in the following articles. 62. Equilibrium of Three Concurrent Forces. — ^ Forces whose lines of action meet in a point are called concurrent forces. A simple form of apparatus for studying the conditions of equilibrium for three concurrent forces is shown in Fig. 39» Three cords are tied to a ring and a drawscale is attached to each. The scales are adjusted so that all exert a considerable force at the same time. The ring will be in equilibrium under the action of the three forces, all of which lie in the Fig. 39. same plane. These forces are concurrent at the center of the ring; their directions are outward from this center in the directions of the cords ; and their magnitudes are given by the readings of the scales. In order to deter- mine the relations that exist among the forces, they are represented in magnitude and direc- tion by the lines , and is pulled in a horizontal direction till A is drawn 20 cm. from the vertical through O, Find the tension upon AO and upon AF. 8. Find the resultant of three concurrent forces of 5, 16, and II lb., respectively, the first two acting in opposite direc- tions, and the third at right angles to them (Fig. 45). 9. A weight of ico lb. is suspended at the middle of a rope, ACB (Fig. 46), 20 ft. long. The ends of the rope are fastened at points A and B at the same height. What is the tension of the rope when CD is 3 ft. ? when CD is I ft.? when CD is i inch ? 10. (a) A brick lies on the ground. What is the equilibrant of the weight of the brick ? {b) What is the reaction of the pressure of the brick upon the ground ? 11. How does the reaction of a force differ from its equilibrant ? Men- tion examples to illustrate. 12. If any number of forces and their equilibrant together act upon a body, what is their combined effect ? r Fig. 45. II. Parallel Forces 67. Equilibrium of Three Parallel Forces. — Parallel forces are forces having parallel lines of action. It is found by experiment that if three parallel forces acting upon the same body are in equilibrium, the following conditions are always fulfilled : — 56 Statics of Solids I /• I. 754^ three forces ^f^^f^^ andf^ (Fig. 47), are in one plane. 2. The two outside forces act in the same direc- T- tion and the inside force in the opposite direction, j[=^ 3. The inside force is equal to the sum of the other tuto, 4. The outside forces are ittversely proportional to the distances * of their lines of action from the Fig. 47. line of cu tion of the inside force ; that is, — < fi : fi :: di I ^„ orfdi =f^t. It will seem that the inside force is nearer the larger of the other two ; but if the latter are equal, it is midway between them. The points of application of the three forces need not lie in a straight line. Any one of the three forces may be regarded as the equili- brant of the other two. Laboratory Exercise 16. 68. Resultant of Two Parallel Forces acting in the Same Direc- tion. — When three parallel forces are in equilibrium, the two outside forces together balance the third force; hence their resultant would also balance it. t/j This resultant {R, Fig. 48) must, therefore, have the same line of action as the third force, and must be ^" ^ ' equal to it in magnitude and opposite in direction; hence, — Tlu resultant of two parallel forces acting in the same direction is equal to their sum ; it acts in the same direction, and its line of action divides the distance between them into parts inversely pro- portional to the forces, PROBLEMS 1. Two boys, A and B, carry a load between them suspended from a pole 5 ft. long. The load is 2 ft. from A's end. What fraction of it does A carry ? 2. If the load weighs 161 lb., where must it be hung in order that A may carry 92 lb. of it ? 1 The distance between two lines or from a point to a line is always understood to mean the perpendicular distance. R o Moments of Force 57 III. Moments of Force 69. Tendency of a Force to cause Rotation. — A force applied to a body may tend to cause it to turn round or rotate about some line as an axis. The simplest case is represented in Fig. 49. A slender stick (meter rod) is supported on a horizontal axis, as a nail, through a hole so situated that the rod will come to rest in a horizontal position. A weight attached on either side of the axis will cause rotation. '^' '^^' Two weights, either equal or unequal, can be attached, one on each side of the axis, at such points that the rod will remain in equi- librium {Exp^. The experiment shows that the tendency of a given force to produce rotation is increased by applying it farther from the axis, and that the rod will be in equilibrium only when the product of one force and its distance- from the axis is equal to the product of the other force and its distance. If/i andy^ denote the weights, and ^i and a^ their distances from the axis respectively, then the condition for equilibrium will be expressed by the equation /i «i =/2 5^^^^^fe j t^ F^^:=d of the body and ^the ~^" ~ / , Fig. 66. center of buoyancy. When a floating body is displaced from its position of equilibrium, the lines of action of weight and buoyancy no longer coincide, and the two forces constitute a couple whose effect is to restore equi- librium, if the equilibrium was stable, or to carry the body still farther from that position, if the equilibrium was unstable. When the rectangular block represented in the figure is tilted from its first position, the center of buoyancy shifts toward the deeper displacement, while the position of the center of gravity remains unchanged. This establishes a couple which tends to restore the body to its former position. Equilibrium in the first position is therefore stable. The third part of the figure represents the posi- tion of unstable equilibrium {Exp.). (Illustrate this in a figure showing the body slightly displaced.) i 66 Statics of Solids The equilibrium of a floating body is always stable when the center of gravity of the body is below the center of buoyancy ; when it is above the center of buoyancy, the equilibrium may be either stable or unstable, depending upon the shape and position of the body, as illustrated above. The equilibrium is neutral if the centers of gravity and buoyancy remain in the same vertical line when the l)ody is disturbed, as is the case with a sphere or a long cylinder with its axis horizontal {Exp.), 84. Stability of Floating Bodies. —The stability of a floating body of given shape is increased by lowering its center of gravity ; for this increases the arm of the couple, which tends to right the body when displaced. It is for this reason that a vessel witho'ut a cargo carries ballast. PROBLEMS I. In what direction does a person lean when carrying a heavy load in one hand ? Why ? 2. Show that when a homogeneous hemisphere is inclined {A^ Fig. 67), its weight tends to bring it into the position shown in B. In what kind of e(|uilibrium is it in the second position ? Is it in unstable equi- librium in the first position ? Give reasons. 3. (a) Oil cans are made of the shape shown in Fig. 68, and are weighted with lead at the bottom. Such a can rights itself when tipped. Explain. (^) Does the can really rise or fall when it rights itself? fiG. 68. 4. Why does a person always lean forward before attempting to rise from a chair ? 5. A pencil with a knife attached can be balanced, as shown in Fig. 69. Try it. ^^^lat is the evidence that the equilibrium is stable ? Where is the center of gravity of the pencil and knife regarded as one body ? 6. Show by means of figures that the .moment of the weight of a sphere is zero upon a horizontal surface, but not upon an inclined plane. 7. If a body that will not roll remains at rest when placed on an inclined plane, three forces act to hold it in equilibrium. Two Fig. 69. of these forces are its weight and the pressure of the plane. What Equilibrium of Bodies 67 is the third force, and in what direction does it act ? Draw a figure correctly representing the direction and the relative magnitude of the three forces. 8. Two spheres weighing 50 kg. and 15 kg., respectively, are connected by a rod so that the distance between their centers is 80 cm. Disregarding the weight of the rod, where is the center uf gravity of the whole considered as one liody ? 9. The average distance between the centers of the earth and the moon is about 240,000 miles ; the mass of the earth is 80 times that of the moon. How far is their common center of gravity from the earth's center? 10. Two men, A and B, carry a board 30 ft. long and of uniform cross- section. A holds at one end ; where must B hold in order to carry .6 of the load? 11. A boy weighing 40 lb. wishes to seesaw alone on a plank weighing 70 lb. The plank is 24 ft. long, and the center of gravity of the boy is i ft. from an end of the plank. How far from that end must the plank be sup- ported ? 12. Why is it an advantage to spread the feet when standing upon a sur- face that is moving unsteadily, as the deck of a vessel ? 13. What would happen to the leaning tower of Pisa (Fig. 75) if the vertical through its center of gravity fell without the base of the tower ? 14. Is the stability of a boat greater when the occupants are standing or sitting ? Why ? 15. Why is it difficult to walk on stilts ? 16. A uniform stick oC timber 10 ft. long balances on an axis 3 ft. from one end when a weight of 20 lb. is hung from that end. Find the weight of the stick. 17. Why cannot one stand with hb heels against a wall and lean forward without falling ? 18. Two boys, A and B, carry a uniform plank 24 ft. long, weighing 120 lb. A holds at one end and B 4 ft. from the other end. What load does each carry ? CHAPTER V DYNAMICS I. Motion 85. Motion. — Motion is continuous change of position. The line along which the center of gravity of a body moves is regarded as the path of the body. The motion of a body is completely known when we know its path and the rate of motion at every point of the path, or the rate and direction of motion at every instant during the motion. Rate of motion is called speed. Velocity includes both rate and direction of motion. The distinction in meaning between the two words is frequently useful, but it is not strictly adhered to. Thus the word velocity is frequently used to signify merely rate of motion, its direction not being a matter of importance for the purpose under consideration. 86. Uniform Motion. — The motion of a body is uniform if the body passes over equal portions of its path in equal intervals of time, however short these intervals may be. If the motion of a body is imiform, its speed is constant, and is measured by the distance that the body moves over in a unit of time. Speed is measured in various combinations of units of distance and of time, as centimeters per second, meters per second, feet per second, miles per hour, etc. In the definitions that follow, the second will be named as the unit of time, since it is the only one that is used in scientific work. The whole distance passed over by a body moving with constant speed is equal to the product of the speed and the time occupied in traversing the distance. Hence, letting d denote the distance, 68 Motion 69 V the (magnitude of the) velocity, and / the time, we have for uniform motion : — d—vt'. also V = -, and /= -• (i) 87. Variable Motion. — The expression "the velocity of a body " has no definite meaning unless the velocity is constant. If it is variable, qualifying terms are required, as indicated in the following definitions : — T/ie velocity of a body at any instant (or at any point of its path) is the distance that it would pass over during the next second (or other unit of time) if its velocity continued unchanged from that instant. Thus when we say that a train is running at the rate of 30 miles per hour, we mean that it would run 30 miles in an hour if it continued at its present rate for one hour. The average velocity of a body during any interval of time (or between any two points of its path) is the uniform velocity that would be required to pass over the same distance in the same time. Average velocity is therefore equal to the distance divided by the time. Representing average velocity by z>, its definition is expressed by the formula, d—vt) from which v = -* (2) For example, if an automobile runs 108 mi. in 6 hr., its average rate is 18 mi. per hr., since this is the uniform rate required to run the given distance in the given time. The actual rate may vary from o (during intervals of stopping) to 40 or 50 mi. per hr. 88. Representation of Velocities. — A velocity may be repre- sented in both magnitude and direction by a b.^ straight line, just as a force may be. Thus if OA (Fig. 70) represents a velocity of 3 ft. per sec. east, then OB represents a velocity of 2 ft. o' ■ ^^ per sec. north. ^^''' 7°- 89. Composition of Velocities. — A body may have two or more independent motions at the same tinae {Exp.). Thus a boat 70 Dynamics rowed across a stream has a motion imparted by the rowing, and also a motion due to the current and equal to it. Suppose the boat to be constantly headed directly toward the opposite shore, and let O (Fig. 71) represent the starting point. OB would be the path of the boat if there were no current. OC is the distance the stream flows while the boat is crossing. The actual motion of the boat is the resultant of these two motions ; its path is represented by OA, If OB and OC be taken to represent the component ve/ocitieSt then OAf the concurrent diagonal of the paral- lelogram constructed on OB and OC as sides, will represent the actual, or resultant, velocity upon the same scale. Velocities are, in fact, compounded by the same rules as forces (.\rts. 63 and 64). The construction is called the parallelogram of velocities. 90. Resolution of a Velocity. — A velocity, like a force, can be resolved into components in any chosen directions. The con- struction is the same as for the resolution of a force (Art. 66). For example, a vessel is sailing 30° north of east at the rate of 1 2 Fig. 71. mi. per hr. At what rate is it advancing north- ward and at what rate eastward ? It is proved in geometry that in a right triangle having an acute angle of 30° the hypothenuse is twice the shorter ^^^- 7a- leg. Hence ON (Fig. 72), the northerly component of the velocity, is 6 mi. per hr. ; and OE, the easterly component, is Fig. 73. V12* — 6* = 10.4- mi. per hr. As a further illustration, let us consider how the boat mentioned in the preceding article must be rowed in order to reach the opposite bank at B instead of at A. The resultant motion is now rep- resented by OB, The component OC, due to the motion of the stream, is the same as before. Hence OB is the diagonal of a parallelogram of which Motion 71 one side is OC. The other component motion is therefore repre- sented by OA^ (Fig. 73). This means that the boat must be con- stantly pointed in a direction parallel to 0A\ and that it would take as long to reach B as it would to row the distance OA' in still water. (In the preceding problem of Art. 89 would more time be required to cross to A than to cross to B in still water ?) PROBLEMS 1. A ball rolls 53 m. in ii sec. Find its average velocity. 2. A train runs with an average velocity of 23 m. per sec. In what time does it run a kilometer ? 3. From a train running at the rate of 9 m. per sec, a mail bag is thrown at right angles to the track with a velocity of 4 m. per sec. Compute the resultant velocity of the bag at the instant it leaves the hand, and draw a fig- ure to show its direction. 4. From a train running at the rate of 12 m. per sec. a mail bag is thrown so that its resultant velocity is equal to that of the train and at right angles to it. What is the magnitude and direction of the velocity imparted in throwing the bag ? 5. An arrow is shot directly backward from the rear of a train with a velocity (relative to the train) equal to that of the train. What is the motion of the arrow ? 6. The rotation of the earth carries its surface eastward at the rate of about \ mi. per sec. (in temperate latitudes). When a ball is thrown up, why is it not left behind (to the west) by the earth in its rotation ? 7. Four boys, A, B, C, and D (Fig. 74), on the deck of a moving vessel, pass a ball round in the order of the letters. What allowance for the motion of the vessel, if any, must be made by each of the boys in throwing ? Give reasons. ' '^ 8. A vessel sails due N.E. at the rate of 15 mi. per hr. Compute the northerly and easterly components of its velocity. 9. A boat is rowed so that it crosses a stream 100 m. wide to a point directly opposite to the starting point (Fig. 73). The stream flows .8 m. per sec, and the boat is rowed at the rate of 1.2 m. per sec. in still water. How long is the boat crossing the stream ? 91. Acceleration. — The velocity of a body is said to be accel- erated when it is increasing, and retardedy or ?iegative/y accelerated, when it is decreasing. The rate of change of velocity is called the 72 Dynamics acceUration. Thus, if a body starting from a state of rest has a velocity of 3 m. per sec. at end of the first second, 6 m. per sec. at the end of the second second, 9 m. per sec. at the end of the third second, etc., its velocity increases 3 m. per sec. every second ; i.e, its acceleration is 3 m. per sec. per sec. This is a case of uniformly atceUraUd motion^ or constant acceleration^ the increase of velocity being the same for each second. When the velocity of a body decreases by the same amount during each second, its motion is said to be uniformly retarded^ or to have a constant negative acceleration. It more frequently happens that the acceleration of a body is variable. This is the case, for example, with a street car. As its speed increases, the rate of increase diminishes. When its speed is the greatest, the increase of speed, or acceleration, is zero. There are, however, important cases of constant acceleration ; and it is only these that we shall consider quantitatively. Motion is accelerated when it changes in direction, even if the speed remains constant. This, however, is reserved for later con- sideration (Art. 119). 92. Formulas for Uniformly Accelerated Motion. — In the case of uniformly accelerated motion in a straight line, the accel- eration is measured by the constant change of speed that occurs during each second. If a body moves with a constant accelera- tion of a cm. per sec. per sec, starting from rest, its velocity at the end of I sec. will be a (centimeters per sec), at the end of 2 sec it will be 2 /7, at the end of / sec. it will be / a. This is expressed by the formula v^at, (3) in which a denotes the constant acceleration and v the velocity at the end of / sec. after starting. This is usually called the final velocity. Since the velocity increases from zero at a uniform rate, the average velocity, z>, during the time /, is one half of the final veloc- ity ; t^.v=—. The entire distance traversed by the body is the Motion 73 product of its average velocity and the time (Art. 87) ; hence, letting d denote this distance, . -, at ^ at^ d=vt = —Xt = — ; 2 2 .0 / ^ that is, d= — ; and /=\/ (4) V From equation (3), /=-. Substituting this value of / in equa- tion (4), we have 2 2 a zr' that is, d= — -, and v^y/tad, (5) 2a This formula expresses the relation between the constant accel- eration of a body starting from rest, the distance that the body has traversed, and its velocity at the end of that distance. If any two of the quantities in formula (3), (4), or (5) are given, the value of the third quantity can be found by substituting the given values in the formula. 93. Laws of Uniformly Accelerated Motion. — The following laws of uniformly accelerated motion in a straight line, for bodies starting from rest, are contained in the above formulas : — I. The velocity at any instant is proportional to the time during which the body has been in motion. (Formula 3.) II. The velocity acquired in a given time is proportional to the acceleration. (Formula 3.) III. The average velocity during the whole time is half the final velocity. IV. The distance passed over is proportional to the square of the time. For, if the body traverses the distance d^ in t^ sec. and the distance d., in /o sec, both measured from the instant of start- ing, then, from formula (4), /?i = — ^, and 4= — ^. Dividing each 2 2 74 Dynamics member of the first equation by the corresponding member of the second, we get . = tj » hence, d,'d^.'. A* : i,\ (6) V. Thf distance trm^ersed in a given time is proportional to the acceleration. (Formula 4.) VI. The acceleration is numerically equal to twice the distance trax>ersed during the first second. For, when /= i, formula (4) becomes d= -. 2 PROBLEMS 1. A ftreet car rant with a constant acceleration of 1.2 m. per sec. per sec. for 8 sec. after starting, (a) What is its velocity at the end uf that time? (^) What was its average velocity during the 8 sec? (r) How far does it ran in the 8 sec.? 2. A stone falls with a constant acceleration of 980 cm. per sec. per sec. In what time will it acquire a velocity uf 35 m. per sec. ? 3. A body moves with a constant acceleration a. (a) How far does it go in the first second ? (^) What is its average velocity during the first second? (r) What is the average velocity during the first 6 sec? (. the weight of the body) is unbalanced. It is well known that a feather or a sheet of paper falls less rapidly than a stone, and that some bodies — a balloon, for example — rise instead of Falling Bodies 75 falling. From such familiar facts as these false conclusions are fre- quently drawn ; but the truth can be gathered from a careful study of a few simple experiments. We know that a balloon rises because its weight is less than the buoyancy of the air, leaving an unbalanced force acting upward. Since, however, the buoyant force of the air upon solids and liquids is relatively very small (Art. 55), it cannot appreciably affect their rate of fall. If we take two sheets of paper exactly alike and roll one of them into a tight wad, it will be found, on dropping them simul- taneously from the same height, that the wad falls much faster than the open sheet {Exp.). The difference in their rate of fall is due to the friction of the air, which is greater upon the open sheet, since it has the greater surface exposed. Buoyancy is evi- dently not the cause of the difference, since the buoyant force upon the sheet is the same whatever its shape. If two pebbles of very unequal size are held, one in each hand, above the head at the same height, and dropped at the same in- stant, they will reach the ground together. (Try it.) In this experiment the friction of the air is too small to produce an appreciable effect upon either body ; hence their observed motion may be regarded as due to their weight alone. This experiment illustrates the interesting fact that all bodies not appreciably affected by the resistance of the air fall at the same rate, regard- less of their weight. The pupil should test this further by compar- ing in pairs the rates of fall of a number of different bodies. Actual differences in the observed rates of fall may be assumed to be due to friction of the air ; and the pupil should discover by experiment the approximate effect of friction upon bodies of widely different density, by trying simultaneously stone, wood, cork, wad of paper, etc. The result of greater or less compact- ness of form can be observed by dropping together a wad of paper and an open sheet, a block and a very thin board or a leaf, etc. The effect of the air for greater velocities is easily tested by dropping the bodies out of a second or third story window. 76 Dynamics 95. HistoricaL — Experiments similar to the above were first tried, so far as is known, by Galileo Galilei (i 564-1 642), an Italian mathematician and scientist. For two thousand years no one had thought to question the doctrine of the Greek philoso- pher Aristotle, who taught that the rate of fall of bodies was pro- portional to their weight. Galileo, who more fully appreciated the value of experiment than any of his predecessors, discovered ^B^ the falsity of this doctrine, and proved the J^^L correctness of his view to the citizens of Pisa H^^B by dropping simultaneously a one-pound ball ^^^^t and a one-hundred-pound ball from tlie top ^^^^m of the leaning tower (P'ig. 75). The two ^^^^H balls reached the ground together. -^^^^K l'^^^ Any difference in the rate of fall of .'^'^^^BHB^ bodies is due to the resistance of the air was ^^ clearly proved, after the invention of the air pump, by causing such bodies as a coin and a feather to fall together from one end to the other of a long glass tube from which the air F»«- 7S« had been exhausted. The feather was found to fall as rapidly as the coin. The experiment is known to the present day as the guinea and feather experiment Laboratory Exercise 2t. 96. Acceleration of Falling Bodies. — Our daily experience teaches that the speed of bodies continually increases as they fall ; />. bodies fall with accelerated motion. Since all bodies fall equal distances in equal times, unless appreciably affected by the resistance of the air, it is evident that gravity, acting alone, ac- celerates all bodies equally. It can be shown by a number of experimental methods that this acceleration is uniform. One of the simplest and most accurate methods by which the motion of a falling body can be studied is that known as Whit- ing's pendulum method (Lab. Ex. 21). In this experiment the distances . its weight) is as many times greater than that on the smaller as the mass of the one is greater than the mass of the other. Thus the two forces cause equal accelerations be- cause they are proportional to the masses of the bodies upon which ihey act. This important law holds for all forces. Thus, if the mass of one street car and its load of passengers is twice that of another, twice as great a force will be required to give the same accelera- tion to it as to the other. It should be noted that weight is not Falling Bodies 79 involved in this illustration, for the entire weight of both cars is supported by the track. 102. Motion of a Sphere on an Inclined Plane. — When a ball is on an inclined plane but is otherwise unsupported, its motion down the plane is due to the component of its weight acting parallel to the plane (Art. 66). Since this component is constant during the descent of the ball, the motion is uniformly accelerated (Art. 99) ; but the acceleration is less than that of falling bodies, since only part of the weight is effective. By diminishing the inclination of the plane the acceleration can be made as small as desired, thus making it possible to determine with considerable accuracy the distances traversed by the ball in successive seconds {Exp.), It will be found by trial that these distances are in the ratio of the numbers i, 3, 5, 7, etc. That is, if x denotes the distance traversed in the first second, the distances traversed during the second, third, and fourth seconds are 3^, 5 -r, and 7 Xj respectively. The whole distance traversed in i sec. is x, in 2 sec. 4 ;c, in 3 sec. 9 jc, in 4 sec. 16 AT, etc. It is evident that the whole distance is proportional to the square of the time ; and a further analysis of these results leads to all the laws of uniformly accelerated motion. This method was first employed by Galileo in studying the laws of falling bodies. PROBLEMS 1. How far does a body fall during the first second? Account for the fact that this distance is equal to half the acceleration. 2. (a) What is the velocity of a falling body at the end of the first second ? (/J) How far does it fall during the second second? (r) Account for the difference between these numbers. 3. What is the velocity of a falling body at the end of the fifth second ? 4. How far does a body fall («) in 5 sec? {b) in 6 sec? (<:) during the sixth second ? 5. (a) \Vhat is the difference between the distance fallen during the sixth second and the velocity at the beginning of that second? {b) Is this differ- ence equal to that found in the second problem? Why? 6. A stone dropped from a cliff strikes the foot of it in 3.5 sec What is the height of the cliff ? 8o Dynamics 7. Why b it that the increased weight of a body when taken to higher latitudes causes it to fait faster, while at the same place a heavy body falls no faster than a light one? 8. When a train is leaving a station its acceleration gradually decreases to zero, although the engine continues to pull with the same force as at the start. Explain. 9. Would you expect the motion of equally smooth and perfect spheres of different weight and material to be equally or unequally accelerated on the same inclined plane? Give reason for your answer. Try the experiment. m. Projectiles 103. Projectiles. — Any body moving through the air and hav- ing a component velocity not imparted by its weight is called a projectile. A bullet fired from a gun, an arrow shot from a bow, and a ball that has been thrown or batted are examples of pro- jectiles. The velocity of a projectile at the instant when the force that set it in motion ceases to act is called its initial velocity. Thus the initial velocity of a bullet is its velocity at the muzzle of the gun. The initial velocity of a ball when thrown is its velocity at the instant it leaves the hand of the player. 104. Forces acting upon Projectiles. — The weight of a projec- tile does not act as an unbalanced force until after the force that imparts the initial velocity ceases. Thus, while a bullet is being driven toward the muzzle of the gun by the pressure of the expand- ing gases, it is constrained by the barrel of the gun to go in a straight path ; but as soon as it leaves the muzzle, it is freed from this restraint, and its weight acts to change its speed and direction of motion. The* resistance of the air very appreciably affects the motion of a swiftly moving projectile, as a rifle ball ; but in the cases considered in this boolc it is disregarded. It must be remembered that the force that imparts the initial velocity is not in existence during the flight of a projectile. It ceases at the instant the projectile is launched. Disregarding the resistance of the air, the weight of the projectile is the only force Projectiles 8i acting upon it during its flight, and is, therefore, the sole cause of change of motion. 105. Effect of Unbalanced Weight. — The eff'ect of weight upon the motion of projectiles is illustrated experimentally by releasing two bodies simultaneously at the same height, — one with a con- siderable horizontal velocity imparted by a sudden push or blow, and the other without initial velocity, being dropped from a state of rest (Fig. 76). The two bodies will always be found to reach the floor at the same instant {Exp). The experiment illustrates A Fig. 76. the fact that gravity causes the same acceleration in its own direc- tion whether acting upon a body initially at rest or upon a body already in motion. This is true whatever the direction of the initial velocity may be ; but it is direcdy evident by experiment only when the initial velocity is horizontal. A projectile has, in fact, two component motions, namely: (i) the initial motion, which is constant in magnitude and direction, since there is no force acting to change it ; and (2) the uniformly accelerated motion due to gravity. The direction of the first is the direction of projection ; the direction of the second is always vertically down. Neither of these component motions interferes in the slightest degree with the other. 82 Dynamics "^ a' \ b' \ c» > \ Fig. 77. 106. Graphic Representation of the Path of a Projectile. — The path of a projectile can be represented graphically by compoiind- j B c D ^^^ its two motions as illustrated in Figs. 77 and 78. In the first case the direc- tion of projection is horizontal, in the second it is obliquely upward. In both figures OA denotes the initial velocity g and Oa denotes - on the same scale. 2 The points a\ b\ c\ etc., represent the position of the pro- y) jectile at the end q^ of successive sec- onds. A smooth ^' curve drawn through these points repre- sents the path of the projectile. This construction indicates that if the velocity of the projectile at any |K)int of its path be resolved into two components, — one in the direction of projection and the other vertical, — the first component will be the initial velocity, and the second will be the same as that of a body start- ing from rest and falling vertically for the same time. This is illustrated in the fig- ures at b\ 107. Projection vertically Upward. — While rising vertically, the velocity of a projectile decreases at a rate equal to its rate of increase in falling, provided the resistance of the air is not appre- ciable. Hence the times of rise and fall are equal ; and both the time and the distance can be computed by the formulas of Art. 97. For example, if a stone is thrown vertically upward with an initial velocity of 49 m. per sec, its velocity at the end of i sec. is 49 — 9.8, or 39.2 m. per sec. ; and at the end of 2 sec. it is Fig. 78. The Laws of Motion 83 49 — 2 X 9.8, or 29.4 m. per sec. Its time of rise is 49 -^ 9.8, or 5 sec. ; for at the end of that time its velocity would be zero. This is the time it would take to acquire a velocity of 49 m. per sec. in falling. The distance that the stone will rise is found by computing the distance it would fall in the same time, starting from rest. PROBLEMS 1. (a) What is the force that causes the initial velocity of an arrow? (6) How long does it act? (c) How is it known that this force is many times greater than the weight of the arrow? (rtion o o "^ * 200 : 800 :: a : 980. 112. Relation between Force and Mass ; Acceleration Constant. — Tke {unbalanced) force necessary to produce a given acceleration is proportional to the mass of thf body upon which the force acts. Expressed algebraically the law is fx'.ft'.'. /«i : Wj. (acceleration constant) (13) The equal acceleration of falling bodies (Art. 101) serves as the simplest and best illustration of this law, since weight is always proportional to mass. But experiments in which the acceleration is not due to gravity are instructive, even if they do not prove the definite relation expressed in the law. The following experiment is of this sort. Suspend a lead or an iron ball an inch or more in diameter by a cord one or two meters long, and suspend a cork of about the same size by a cord of equal length. With a swift horizontal swing of the arm, strike the cork with the open palm. Strike the lead ball in the same way, with equally rapid motion of the hand. (A small board may be placed a foot or more beyond the ball to stop The Laws of Motion 87 it.) The force exerted upon the ball is very considerable, while that upon the cork is almost inappreciable, although it is started with equally accelerated motion. It is evident that the difference is not due to the greater weight of the lead ball, for, in the vertical position, its weight is entirely supported by the cord. Neither is the difference due to friction or any other force. The lead ball requires the greater force to start it because its mass is greater. Having greater mass it has greater inertia, and this requires pro- portionally greater force for an equal acceleration. 113. The Comparison of Masses by the Inertia Test. — It follows from the law stated in the preceding article that, if equal forces act upon unequal masses, the acceleration of the smaller mass will be the greater. The acceleration will, in fact, be in- versely proportional to the masses. Hence, if equal forces impart equal accelerations to two masses, the masses are equal {Exp.). This is the inertia test or acceleration test of the equality of two masses. Masses that are equal by the inertia test are, of course, equal by the usual weight test also. The inertia test is more fundamental and scientifically more significant, — a fact that can hardly be appreciated by students of elementary physics ; but the weight test is more accurate and much more convenient, and hence is used exclusively in scientific work as well as in daily life. Laboratory Exercise 20. 114. The Element of Time in the Effect of Force. — Since change of velocity is proportional to the time during which a given acceleration continues {v = at), it follows that the- change of velocity produced by a constant force is proportional to the time during which the force acts. Some forces are very great, but act for an extremely short time, as the blow of a hammer, or the force exerted by a bullet in penetrating a board. The time is so extremely brief in the latter case that a bullet fired through a door standing ajar will scarcely disturb it, although it can be swung with a light push of the finger. These ideas are illustrated by a simple experiment with a small coin and a calling card. The friction between them when the coin 88 Dynamics is placed on the card is sufficient to impart the motion of the card to the coin when the card is moved slowly about ; but, when it is very suddenly started, the coin is left behind. This is neatly shown by placing the card and coin on a finger (Fig. 79) and suddenly snapping the card in a horizontal direction. If the blow is successfully aimed, the card will fly from under the coin, leaving it at rest on the finger, friction being insufficient to impart appreciable motion to the coin in so short a time. (Try the experiment.) Fig. 79. PROBLEMS 1. The acceleration of any falling body is proportional to its weight in different latitudes and at different altitudes (Art. 98) ; but all bodies at the same place fall with equal acceleration, whatever their weight (unless re- tarded by the air). Explain. 2. A bullet fired through a plate glass window will often make a smooth hole without cracking the glass. Explain. 3. A nail can be driven by striking it with a hammer, but not by pressing the hammer steadily against it. Explain. 4. Gravity upon the moon is one sixth as great as upon the earth. G)m- pute the acceleration of a falling body upon the moon. 5. Gravity upon the sun is 27.6 times as great as upon the earth. Com- pute the acceleration of a falling body upon the sun. 6. How far would a body fall during the first second (a) upon the moon ? (^)upon the sun? 7. (a) Would the mass of a given body be the same upon the sun or the moon as upon the earth? (6) Would its inertia be the same? 8. Would it take less powder to fire a cannon ball with a given velocity upon the moon than it would upon the earth ? 9. Is it harder for horses to start a loaded wagon or to keep it in uniform motion? Give reasons. 10. Why does a ball player move his hands quickly backward in the act of catching a swift ball ? 11. An unbalanced force of 25 g. acts on a mass of 80 g. What is the acceleration ? 12. WTiat force is required to impart an acceleration of 15 cm. per sec. per sec. to a mass of 100 g.? The Laws of Motion 89 115. The Law of Inertia. — Since change of motion results only from the action of an applied force, in accordance with the pre- ceding laws, matter is said to be passive or inert, and the property thus manifested is called inertia^ (Art. 9). The law of inertia is as follows : — Every body continues in its state of rest or of uniform motion in a straight line unless compelled to change that state by an external force. This law follows as a corollary from the law stated in Art. 1 1 1 ; for the acceleration must be zero when the unbalanced force is zero, since the two are proportional, and, with zero acceleration, motion remains constant both in magnitude and direction. It is impossible to prove the law of inertia by direct experiment, since no body can be freed from the action of all forces ; but the indirect evidence of its truth is conclusive (see Art. 9). Astronomical observations on the motions of the moon and the planets confirm all the laws of motion as well as the law of gravitation. 116. The Law of Mutual Action. — To every action there is an equal and opposite reaction ; or, the mutual actions of two bodies are ahvays equal and in opposite directions. Illustrations of this law were considered in Art. 12, and there have been numerous applications of it in the study of fluids and the statics of solids. The law holds for all forces, whether bal- anced or unbalanced. Force exists only through the mutual action of two bodies (or two parts of the same body, which amounts to the same thing). Thus every force is one of a pair of equal and opposite forces, exerted by each of two bodies on the other. The two forces do not balance each other, since they act upon different bodies ; but either or both may be balanced by other forces. For example, the pressure exerted by a bat upon a ball in striking it is unbalanced and imparts motion to the ball. The reaction of the ball upon the bat is also unbalanced and checks the motion of the 1 The pupil should avoid the misconception that the inertia of matter is an active agent opposing and, in some sense, neutralizing the effect of force. Inertia is not force, nor does it ever balance a force. 9© Dynamics bat. ^Vhen a piece of iron placed on an anvil is struck with a hammer, the blow of the hammer is balanced by the equal and opposite pressure of the anvil, both acting on the piece of iron ; hence the iron remains at rest. When a person jumps from a boat, the reaction on the boat is unbalanced and pushes the boat in the opposite direction from that in which the person jumps ; but, in jumping from a rock, the reaction upon the rock is balanced by the friction between it and the ground, and it remains at rest. It is often supposed that the motions of animals and self-pro- pelling machines are independent of applied force, since they *' make themselves go." The motion of all matter, animate or inanimate, is in accordance with the same laws of motion. The real difference between the conditions of motion of a stone and an animal or an engine, is that the latter can cause the applied forces that move them, and a stone cannot. For example, when a boy jumps, he pushes vigorously with his feet downward and backward, against the ground with a force much greater than his weight. The ground reacts with an equal and opposite force upon the boy, and it is this reaction that enables him to spring upward and forward. A similar reaction of the ground takes place with every step in running. The runner also leans forward, in which position his weight pulls his body forward, as in the act of falling. When one attempts to start, stop, or turn quickly while walking on ice, friction is too slight to cause the necessary reaction upon the feet, and this results in a fall. A bird in flying pushes the air doAWiward and backward with its wings ; the reaction of the air upward and forward sustains the bird in its flight. The mutual action between the driving wheels of an engine and the rails is different from that between the car wheels and the rails, as is shown by the fact that the former sometimes slip, spinning round and round, while the latter never do. A driving wheel exerts a strong backward push on the rail, and slipping is prevented only by friction ; the forward reaction of the rail on the wheel is essen- tial to the motion of the engine, and is an external force. The Laws of Motion 91 117. Relative Velocities due to Unbalanced Action and Re- action ; Momentum. — When the mutual actions of two bodies are unbalanced, their accelerations are inversely proportional to their masses, since the forces exerted by each upon the other are equal (Art. 113, first paragraph) ; and, if the bodies are initially at rest, their velocities will also be inversely proportional to their masses. Thus when a man jumps from a boat that weighs three times as much as himself, the boat is pushed back with a velocity one third as great as the forward velocity of the man. A rifle " kicks " when fired, because the gas from the burned powder presses back on the rifle, as well as fonvard on the bullet, and with equal force. The velocities of the rifle and the bullet are inversely proportional to their masses. Let nty and W2 denote the masses of two bodies initially at rest, and Vx and v.^ their respective velocities imparted by mutual action, the bodies being free to move ; then nti -.m^wv^: z/i, or tn-^Vx «= W2?v The product of the mass of a body and its velocity is called its momentum. Hence bodies initially at rest and free to move acquire equal momenta in opposite directions as a result of their mutual actions. Thus the momentum of a rifle in its recoil is equal to the momentum of the bullet as it leaves the muzzle. When a moving body strikes a body at rest, and their mutual actions are unbalanced, the one loses as much momentum as the other gains. 118. Newton's Laws of Motion. — The fundamental laws of motion considered in the preceding articles are restated here for convenient reference : — I. Every body continues in its state of rest or of uniform motion in a straight line^ except in so far as it is compelled by external forces to change that state. II a. The acceleration of a body is proportional to the unbalanced force acting upon it^ and is in the direction of that force ; or, f'.fi'.'.ai'.a^. (mass constant) II b. The unbalanced force necessary to produce a given accelera- 92 Dynamics tion is proportional to the mass of the body upon which the force €Uts ; or, fx'fi'' '"i • '"s« (acceleration constant) III. To nrr}' action there is an equa/ ami opposite reaction ; or the mutual actions of two bodies are always equal and in opposite directions. The laws numbered I and III are known as Newton's first and third laws of motion respectively ; Ila and lib are together equiv- alent to his second law of motion. These laws constitute a com- plete statement of the relation between matter and force. The first and second were discovered by Galileo in studying the motion of falling l>odies and projectiles. The third law was also known to others before Newton. They are called Newton's laws because he was the first to state them in their present form. Note to the Teacher. — The second law of motion as stated by Newton can be derived Irom II a and lib as follows: According to II a, /oc a (/« = con- stant) ; according to II b, /ac m (a = constant). Hence /oc ma, and _/?oc mat. When the initial velocity is zero, the latter may be written //« mv. The equality of ft and mv requires the introduction of the dyne as the unit of force. With the gravitational unit of force, the equations are /= — and ft = These equations express the second law in mathematical form. Stated in words, it is : Change of momentum is proportional to the appHed force and to the time during which it acts, and takes place in the direction of the force. PROBLEMS 1. Two boys, A and B, are pulling upon the ends of a rope. A pulls B along. Is he pulling harder (/.^., with greater force) than B? Explain. 2. Two boats are afloat some distance apart, and at rest. A man sitting in one of them hauls in a rope attached to the other. Describe and explain the motions of the boats, assuming them to be {a) of equal mass (including the mass of whatever is in the boats; ; (Z^) of uneciual mass. 3. Why does stamping remove mud from the shoes ? 4. Why does beating a carpet remove dust from it ? 5. Why can the handle be tightened in the head of an ax (a) by striking the end of the handle against a log? (/') by holdingthe ax at rest and strik- ing the end of the handle with a hammer ? Curvilinear Motion 93 6. Two battle ships are in an engagement, with one in pursuit of the other. Does the reaction of the guns in liring aid or hinder the speed of the pursuer? of the pursued? 7. How should a person handle his body to avoid a fall when alighting from a rapidly moving car ? , Explain. V. Curvilinear Motion 119. Cause of Curvilinear Motion. — We have learned that the weight of a projectile causes its path to curve downward, unless the motion is vertical. Any unbalanced force acting upon a body at an angle to its direction of motion produces a similar effect ; i.e. causes the path of the body to curve toward the direction in which the force acts. A stone tied to a string and whirled in a circle round the hand is a familiar illustration. The motion of the stone in a circle is (Uie to the continued inward pull of the string upon it. If the stone is released at any point of its path, it con- tinues in the direction of its motion at the instant of release, except in so far as its motion is then affected by its weight. The following experiment affords a better illustration : A wooden ball tied to a string is rolled round in a circle on the top of a large table or on the floor. When released at any point of its path, it continues in the direction in which it was moving at that instant. Thus, if released at A (Fig. 80), its path will be AB, a line tangent to the circle at A {Exp.). The law illustrated by the experiment is general. A body moves in a curved path only when acted ^^' °* upon by an unbalanced force directed toward the inside of the curve. A force acting upon a body so as to change its direction of mo- tion is called a centripetal force, because it acts toward the center of the curved path (from the Latin centrum, center, ^n^petere, to seek). A centripetal force may act at right angles to the direc- tion of motion, or obliquely forward or backward. The three cases are illustrated at M, N, and L respectively in Fig. 81, which represents the path of a projectile. Strictly speaking, the centripe- 94 Dynamics / Fig. 8i. tal force at L and N is the component of weight acting at right angles to the path, />. the component/. The tangential compo- nent, Ty acts opposite to # ^^ ^v,^^ the direction of motion at Z, causing decrease of speed, and in the direc- tion of motion at W, caus- ing increase of speed. The centripetal compo- nent at L and N and the entire weight at M cause change of direction only. Uniform motion in a circle is due to a constant centripetal force, which always acts toward the center of the circle and at right angles to the direction of motion. 120. Laws of Centripetal Force. — It can be shown either by experiment or by mathematical analysis based on the second law of motion that centripetal force is (i) proportional to the. mass of the body, (2) proportional to the square of the velocity, and (3) inversely proportional to the radius of curvature of the path. The effect of the mass of the body can be shown by whirling unequal masses with equal rapidity, using strings of equal length ; and the effect of velocity, by whirl- ing the same body more and less rapidly. (Try it.) 121. Illustrations of Centripetal Force. — If a ball or other object is suspended by a string from a fixed support and started in a horizontal circle (Fig. 82), it will continue to revolve in a slowly diminishing circle (more accurately a spiral) for sev- eral minutes {Exp.). The decrease in the size of the circle is due to friction, chiefly of the air, and may Fig. 83. Curvilinear Motion 95 be disregarded. If all friction could be removed, the motion would continue indefinitely without change. Disregarding fric- tion, the ball is acted upon by two forces ; namely, its weight, IV, and the tension, T, of the cord. The vertical component of the tension, v, is equal to IV and balances it ; the horizontal component, /, is unbalanced, and is directed toward the center of the circle. The component / is the centripetal force that causes the circular motion of the ball. Since this force acts at right angles to the direction of motion, it has no effect on the speed (Art. 119, last paragraph). In rounding a curve a bicycle rider brings the necessary cen- tripetal force to bear upon his body by leaning toward the inside of the curve. Let C (Fig. S^) denote the cen- ter of the curved path of the rider and wheel, and OB the inclination of the wheel. The wheel exerts an oblique pressure upon the ground in the direction OB (as is shown by the fact that when a wheel slips in turning a curve it always slips outward). The reaction of this force is an equal pressure of the ground against the wheel in the direction BO, and is denoted in the figure fig. 83. by OPy as if it were applied at the center of gravity. This oblique inward pressure of the ground may be considerably greater than the weight of the wheel and rider, which is denoted by OIV. The vertical component of OP is equal to the weight of the rider and wheel and balances it. The horizontal compo- nent,/, is the centripetal force upon the rider and wheel. 122. Inertia shown in Curvilinear Motion. — The tendency of moving bodies to move in a straight line, as stated in the law of inertia, is shown by the fact that curvilinear motion continues only so long as a centripetal force acts to maintain it. From the instant that centripetal force ceases to act upon a body, it con- tinues in a straight line, or, to use a familiar expression, it " flies off at a tangent." Thus motion in a curve is explained by describ- ing the centripetal force that causes it ; while " flying off at a 96 Dynamics tangent " is accounted for by noting the absence of centripetal force, this behavior being merely a result of the inertia of matter. To illustrate : When a carriage is driven round a corner, its tend^cy is to continue in a straight line ; hence the wheels tend to slip over the ground toward the outside of the curve. Ordi- narily friction is sufficient to prevent the shpping, and this causes the ground to react with an inward pressure on the wheels. But, since the wheels cannot slide, the tendency of the carriage to continue in a straight line results in a tendency to overturn out- ward. This tendency is opposed by the weight of the carriage, which, under ordinary circumstances, acts as a sufficient cen- tripetal force to bring the carriage safely round the curve. If, however, the motion is very rapid and the curve sharp, this cen- tripetal force may be insufficient ; in which case the carriage will overturn, not because of a force acting to oi'erturn it, but because thf centripetal component of weight is insufficient to p?vduce the necessary change of direction. The behavior of water on a rotating grindstone is a further illustration. The water is held to the stone by adhesion ; but when the speed reaches a certain value, the adhesion is no longer sufficient to carry the water round in the curved path, and it flies off. Mud flies from the wheels of a rapidly moving carriage for the same reason. 123. Centrifugal Force. — When a stone is whirled at the end of a string, it exerts an outward pull through the string upon the hand, which is the equal and opposite reaction of the pull that the hand exerts upon the stone. The reaction is called centrifugal force, since its direction is outward from the center (from the Latin centrum, ^xiA fugere, to flee). The centrifugal force is exerted upon the hand, and tends to pull it (not the stone) outward. It is a common but wholly mistaken idea that centrifugal force causes or tends to cause bodies to leave a curved path and fly off or overturn. When a carriage rounds a comer, the only cen- trifugal force in action is the outward pressure of the wheels upon the ground. Centrifugal force does not act upon the body mov- Curvilinear Motion 97 ing in the curved path; hence it cannot under any circumstances affect the motion of that body. The confusion of thought with reference to centrifugal force arises from the fact that the term was originally appHed to a fictitious force, and is still used in this sense in unscientific language. This fictitious force is supposed to act on the moving body and to be the cause of its tendency to " fly off at a tangent." No such cause exists, and the assumption that it does exist only leads to a misunderstanding of the whole subject. Centrifugal force in the only sense in which the word should be used, need not be mentioned in discussing curvilinear motion, for, although it is a real force, it does not act upon the body whose motion is under consideration. PROBLEMS 1. Why is the curvature of the path of a projectile the greatest at its highest point ? (See Fig. 8i.) 2. Explain what would happen if a bicycle rider failed to lean inward sufficiently. 3. Why are curves in bicycle race tracks steeply inclined toward the center ? 4. If a boy, while running, wishes to change his direction suddenly, as in dodging, how does he handle his body ? Explain. 5. A bucket of water can be whirled in a vertical circle, the bucket being inverted at the top of the circle, without any of the water spilling. (Try it.) Explain. 6. Draw three figures similar to Fig. 82 ; one representing the case where the deflection of the cord from the vertical is only a few degrees, one where it is 40*^ to 50^ and one where it is 70° to 80°. The angles need not be measured, but the forces are to be represented to the same scale in all. The tension must always be taken of such magnitude that its vertical component is equal to the weight of the ball. How does the centripetal force vary as the cord becomes more nearly horizontal? Would it be possible to swing the ball fast enough to bring the cord to a horizontal position? Give reason for your answer. 7. A ball weighing 2 kg. is suspended from a cord 50 cm. long, and made to revolve in a circle whose radius is 30 cm. Compute (^d) the centripetal force upon the ball and {b) the tension upon the cord, {c) Draw a figure representing the conditions, including the forces involved. 98 Dynamics VI. Universal Gravitation 124. Universal Gravitation. — The pupil is already familiar with the fact that the earth attracts all bodies at and near its sur- face, and that this attraction is directly evident as weight. There is, however, no familiar evidence that all bodies attract one another under all circumstances, yet such is the case. The attraction be- tween masses of even several hundred pounds is exceedingly small — so small, in fact, as to be far beyond any ordinary means of detecting it.* Nevertheless a number of experimenters have measured the attraction between masses of various substances varying in weight from a fraction of an ounce to several hundred pounds. These experiments not only prove the existence of gravitational attraction between bodies, but afford a measurement of it that is probably not in error by more than one per cent. The methods by which such exceedingly delicate measurements are carried out lie far beyond the range of elementary physics. Sir Isaac Newton (1642-17 2 7), a noted English physicist and mathematician, proved that the planets are held in their orbits by the attraction of the sun, and the moon in its orbit by the attrac- tion of the earth ; and that the motions of the planets are slightly modified by their attractions for one another. He also discov- ered that the attractions of the sun and the planets for one another and the attraction of the earth for bodies upon its surface are all in accordance with the same law. This law is called Nev^'ton's law of gravitation, and is as follows : — Every particle of matter in the universe attracts every other particle with a force whose direction is that of the line joining them, and whose magnitude is directly proportional to the product of their masses, and inversely proportional to the square of the distance between them. 1 Two spheres of cast iron each 1.8 m. in diameter would attract each other with a force of i g. when placed close together. Such spheres would weigh about 22,000 kg. or 22 metric tous each. Universal Gravitation 99 Gravitation is the general term applied to the force with which all bodies attract one another. The attraction of the earth for bodies at and near its surface is usually called gravity. 125. Illustrations of the Law. — Newton proved that the attraction between a sphere and any other body is the same as it would be if the entire mass of the sphere were concentrated at its center. Hence in considering the attraction of the earth for any body upon its surface, the distance stated in the law is the earth's radius. In considering the attraction between any two bodies of appreciable size, the distance between their centers of gravity is to be taken as the distance between the bodies. Let/ denote the attraction between two masses m^ and m^, and d the distance between their centers of gravity ; similarly, let F denote the attraction between two masses J/j and Mc^, and D the distance between their centers of gravity ; then, according to the /./r.. __.___. (14) The meaning of the law as expressed in this proportion will be more readily understood from the following examples : — 1. What is the relation between the masses of two bodies and their weights ? Let m\ and M\ denote the masses of the two bodies, and / and F their weights respectively. Since the second attracting body in each case is the earth, wo = M^ = the mass of the earth and = the radius of the earth. Hence the above proportion reduces to /:F::mi : Mi; that is, the weights of any two bodies are proportional to their masses — a fact with which the pupil is already familiar. 2. How does the weight of a body upon the moon compare with the weight of an equal mass upon the earth ? Let mi and Afi denote the equal masses upon the moon and the earth, and mo and Afo the masses of the moon and the earth respectively. Then d and D denote the radii of the moon and the earth, and /and 7^ the weight of the body upon the moon and upon the earth respectively. loo Dynamics Snce mi = Mu the proportion reduces to from which /h- /r= ^ X f - V- The radius of the earth is 3960 mi., the radius of the moon 1082 mi., and the mass of the moon ^ of the earth's mass. Substituting these values in the equation, we get f^F=i^x (3960 + io82)» = .1675 = \ (nearly). 3. How does the force of gravity at the distance of the moon compare with its value at the surface of the earth? The mean distance of the moon is almost exactly 60 times the earth's radius. Let D denote the radius of the earth ; then (.8) in which / denotes the period, and / the length of the pendulum, g the acceleration of a falling body, and tt the ratio of the circum- ference of a circle to its diameter (=3.1416). The formula includes the four laws of the pendulum already considered. The first two laws follow from the fact that the formula contains no factor depending upon amplitude, mass, or material. That the period is proportional to the square root of / and inversely proportional to the square root of g is evident from the formula as it stands. The formula holds for the compound pendulum provided the length be taken as defined in Art. 132. 138. Uses of the Pendulum. — The principal use of the pendulum is to regulate the motion of clocks. The mechanism by which this is effected is represented in Fig. 87. The pendulum rod passing between the prongs of a fork, A^ communicates its motion to a rod, B, which turns on a horizontal axis, C. To this The Pendulum 109 axis is fixed a curved piece, called the escapement, which has a projection at each end. These projections are alternately brought into contact with the teeth of the escape7nent wheel, D, by the motion of the pendulum. The escapement wheel is the last of the train of wheels in the clock and is driven by them ; but the escapement permits only one tooth to pass at a time, while the pendulum swings back and forth. The control thus exercised on the escapement wheel by the pendulum is com- municated through the entire train of wheels to the weight or spring that runs the clock and to the hands. As the escapement wheel turns, its teeth press upon the projections of the escape- ment. These slight impulses are transmitted to the pendulum and maintain its motion. The rate of a clock is controlled by means of a thread and nut at the lower end of the pendu- lum. The bob is raised or lowered by turning this nut. A compound pendulum of special construc- tion is used to determine the acceleration due to gravity at different places. The length and period of the pendulum are determined very accurately, and their values substituted in the pendulum formula, from which the value of ^ is then computed. PROBLEMS • I. How would the expansion of the rod of a pendulum in summer and its contraction in winter affect the rate of a clock if the height of the bob were not adjusted to compensate the expansion and contraction ? 2. What is the usual shape of the bob of a clock pendulum ? What is the advantage of this shape ? 3. What is the length of a pendulum that beats seconds (/ = i) at a place where the value of g is 980 cm? SuoGESTioN.— Substitute the values of / and g in the pendulum formula, and solve for /. Fig. 87. iio Dynamics 4. Find the lengths of the pendulums whose periods are .7 sec. and 1.5 sec respectively. Suggestion. — Substitute in the pendulum formula, assuming 980 cm. for g ; or substitute in formula 16, taking /^ = i, for /j the length of the seconds pendulum, and for t\ the given period. Solve for l\. 5. find the periods of pendulums whose lengths are 20 cm. and 250 cm. respectively. 6. What is the length of a pendulum that makes 70 vibrations per minute? 7. What is the length of the seconds pendulum on Mars? 8. At what point or points in the path of a pendulum bob is its speed greatest ? least ? increasing most rapidly ? constant ? Is the speed constant for any appreciable distance ? Is the increase of speed constant in any part of the path ? Si'GGESTiov. — The answers are all to be determined from a knowledge of the tangent^ force at any point of the path. CHAPTER VI ENERGY I. Energy and Work 139. Energy. — The word energy is used in science with a definite meaning which i:an be understood only by a study of the different forms in which energy exists. Energy is most generally recognized by the ability of bodies possessing it to cause motion in other bodies or to maintain their motion in opposition to friction or other forces tending to stop them. Thus the energy of a bent bow is shown by its ability to project an arrow, and the energy of a coiled spring by its ability to run a clock. The energy of the wind enables it to turn windmills, propel ships, uproot trees, etc. The energy of coal, wood, and oil is utilized by means of the steam engine in running mills, drawing trains, and propelling steamships. Energy, in fact, is manifested in one or more of its many forms in every phenomenon. 140. Kinetic Energy. — A moving body can impart motion to other bodies ; it therefore has energy. The energy that a body has by virtue of its mass and its velocity is called energy of motion or kinetic energy, 141. Work. — The transference of energy from one body to another is called work. The amount of energy transferred and the amount of work done are equivalent expressions. Energy is transferred from one body to another by means of the force that each exerts upon the other. For example, when one ball rolls against another, setting it in motion, the latter receives kinetic energy by means of the pressure exerted upon it while the two are in contact ; and, at the same time, the energy of the first ball 1 1 2 Energy is diminished by an equal amount by the reaction of the second ball upon it in the direction opposite to its motion. The first ball is said to do positive work upon the second, and the latter negative work upon the first. The work by which a body gains energy is called positive, and that by which it loses energy is called negative. To illustrate further : Positive work is done upon a train by the pull of the engine. This, if it were the only force acting on the train, would increase its kinetic energy ; but the retarding forces of friction are at the same time doing negative work upon the train. If the pull exceeds friction, positive work will exceed nega- tive, and the excess of positive work wjll result in increase of kinetic energy. If the two are equal (resultant force zero), the positive and the negative work will be equal and the energy of the train will be constant (the speed being constant) . After the engine ceases to pull, the only work done upon the train (provided the track be level) is the negative work due to friction, by which the train loses its energy and is stopped. 142. Conditions Necessary for the Transference of Energy. — Since one body does work upon another only by exerting force upon it, we commonly say that the force does the work. Although work is done only through the action of force, a force may act without doing work. When a horse pulls on a load without starting it, no work is done by the force exerted, for there is no transference of energy to the load. If the load is started, the force acts through a certain distance, and, in doing so, does work of acceleration in imparting motion to the load and work against resistance in over- coming friction.^ There is neither work of acceleration nor work against resistance without motion of the body upon which the force acts. A* force may also act upon a moving body without doing work. Whether work will be done or not depends upon the relative 1 Fricrion develops heat, and heat is a form of energy (Art. 148) ; hence to maintain motion against friction involves the transference of energy, or the doing of work. Energy and Work 1 1 3 direction of the force and the motion, as will be seen from the following illustrations. The weight of a projectile rising vertically constantly diminishes its kinetic energy by doing negative work of acceleration. The weight of a falling body does positive work of acceleration upon it, constantly increasing its kinetic energy. In both cases the line of action of the force (weight) \^ parallel to the direction of motion. As a pendulum vibrates, it is only the tangential component of the weight of its bob that does work of acceleration (Fig. 85), causing gain of kinetic energy during the first half of each vibration and loss of kinetic energy during the second half; and it is only this component that does work against the resistance of the air. The other component of weight, which acts at right angles to the direction of motion, does no work, for it neither changes the speed of the bob nor helps to maintain its motion against the friction of the air. The same is true of the tension of the thread. A force acting upon a body at right angles to its direction of motion does no work ; for it neither changes the speed of the body nor helps to maintain its motion against friction or other resistance. This is true whether the force is bal- anced or unbalanced. Thus, on the whole,^ no work is done upon the moon by the attraction of the earth, or upon the planets by the Fig. 80. attraction of the sun. In the case of oblique forces, as the weight of a pendulum bob, it is only the tangential component of the force that does work ; that is, tiie com- ponent whose line of action is parallel to the direction of motion. 1 Since the orbits of the moon and the earth are not quite circular but elliptical, the attraction is not exactly at right angles to the path except at two points {A and B, Fig. 88). As the planet movt-s from A to'B, the tangential component of the attraction causes decrease of speed, while from i? to ^ it causes an equal increase. Hence, on the whole, there is neither gain nor loss of kinetic energy. There is, of course, no work against resistance, for the planets move without friction. 114 Energy Fig. 89. 143. Measure of Work. — The work done by a force is meas- ured by the product of the force and the distance through which the force acts, the distance being always measured parallel to the bne of action of the force. For example, suppose we wish to find the work done by the weight of a ball while it rolls down an in- chned plane, AB (Fig. 89). Let ^denote the length of the plane, AB^ and h the height of the plane, BC. The part of w that does work is the component, /, acting parallel to the plane. The distance through which it acts is //, and the work that it does is measured by df. From similar triangles, f \ w \\ h \ d ) hence ■"c fd = wh. That is, the work done by the weight of the ball is also measured by wh. But, while the ball rolls down the plane the distance d^ it descends through the vertical distance h. Thus the work done by w is equal to the product of w and the displacement in its own direc- tion. In measuring the work done by an oblique force, it is immate- rial whether we take ( i ) the product of the whole force and the component of the displacement taken parallel to the line of action of the force {wh in the above example), or (2) the product of the whole displacement and the component of the force acting parallel to it {fd in the above example). Both methods are fully included in the above rule for the measure of work. The choice is a matter of convenience, determined by the nature of the problem. In the case where the applied force and the displacement have the same or opposite directions, the work done is simply the product of the two. If the force is variable, the average force exerted through the distance considered must be taken. The work done by a force, /, while acting through a distance, opular language ; but in science the word force is restricted to the meaning with which the pupil is already familiar from the previous work. universitV 1 Energy and Work \sAt 'rk^^^ throwing a ball, into potential energy of position in carrying a hod of bricks up a ladder, and chiefly into heat in sandpapering a board. Other transformations of energy are considered under the different subdivisions of physics. 152. The Dissipation of Energy. — Since the motion of all bodies is opposed in a greater or a less degree by friction (except in interplanetary space), motion necessarily involves the loss, or dissipation^ of mechanical energy by its transformation into heat. The energy thus transformed is said to be dissipated because it is no longer available for doing useful work ; it is not lost in the sense that it no longer exists. For example, if the hammer of a pile driver weighs looo lb. and the friction that must be overcome in lifting it amounts to loo lb., then, in raising the hammer 20 ft., the lifting force of iioo lb. will do 20,000 ft.-lb. of work against gravity and 2000 ft.-lb. of work against friction. The work done against gravity is useful, since, as a result of it, the hammer has 20,000 ft.-lb. of available potential energy. The work done against friction is transformed into heat while the hammer is being raised, and cannot be further utilized. The work done in moving wagons, street cars, and trains from one place to another (without change of elevation) is done against friction, including the resistance of the air ; and the energy thus expended is dissi- pated as heat. When the axle of a car wheel is not properly oiled to reduce friction, the amount of heat generated is so great that it causes a " hot box," and sometimes even sets fire to the car. When bicycles came into general use, personal experience of the waste of energy due to friction soon led to the invention of ball bear- ings. 153. Power. — The rate at which work is done or the rate at which an engine or other source of energy is capable of doing work is called power. The customary unit of power is the horse- power (H. P.), which is equal to 550 ft.-lb. or 76 kg.-m. of work per second. Thus a twelve-horse-power engine working at three fourths of its full capacity is doing work at the rate of 9 H. P., or 4950 ft.-lb., of work per second. 122 Energy PROBLEMS 1. Show from formula (20) that the kinetic energy of a body is propor- tional (l) to its mass, (2) to the square of its velocity. 2. Two bodies have equal kinetic energ)', but the velocity of the second is three times that of the first. How do their masses compare ? 3. A body is thrown vertically upward. (er is the ratio 0/ the arm 0/ the effort to the arm of the resistance {a: A). This ratio is frequently called the leverage, 158. Work done with a Lever. — Suppose a constant effort/, acting at the end of a lever of the first class (Fig. 98), to move the lever through a certain angle against ^' '^^ ^ " a constant resistance 7% applied at the _ — ,_ _ _ , „,.^ — "^-^^ ^i^^ other end. Suppose further that/" and ^ ""-'' act at right angles to the lever through- out the motion. I^t //denote the distance through which the effort acts and Z> the distance through which the resistance is overcome. Then fl is the work done by the effort and FD the work done against the resistance ; or, we may say, fl measures the energy transferred to the lever by the agent producing the motion, and FZ> measures the energy transferred by the lever to the object moved. Formula (21) is F:f::a:A and, by geometry, d: D::a: A; hence, F:f::d:Df or, fd=^FD. This means that, neglecting friction, the lever transmits energy from the agent to the body acted upon without gain or loss. This is easily proved to be true for levers of the second and third classes also; and it can be shown to hold in all cases, however the The Simple Machines 127 forces may vary in magnitude or direction. There may be a gain of force by the use of a lever ^ but never a gain of etiergy. There is always, in fact, a slight loss or waste of energy due to friction ; that is,// is slightly greater than /^Z?. PROBLEMS 1. In using scissors is greiater force required when the cutting is done near the tips df the blades or near the handles ? Why ? 2. Classify the following levers, and state in each case whether the effort is greater or less than the resistance : the wheelbarrow, oar, fishing rod, equal-arm balance, steelyard, nutcracker. 3. Use a pencil as a lever of the first class to move a book ; also as a lever of the second class. 4. In which class or classes of levers is the effort necessarily less than the resistance ? greater than the resistance ? In which may it be either greater or less ? 5. Prove that fit= ^D when a weight W is raised through a vertical distance D by means of a force / acting ver- tically through a distance .). 193. Adhesion. — There is no evidence of any difference in the nature of the attraction between molecules of the same kind and that between molecules of different kinds; but the former is generally called cohesion, and the latter adhesion. The distinction is convenient but unimportant. There are many familiar examples of adhesion between solids. 1 50 Some Properties of Matter Mud sticks, or adheres, to any object with vexing facility ; butter adheres to a knife and to the bread upon which it is spread. The adhesion of metals is utilized in gold and silver plating. Ordi- narily there is no appreciable adhesion between solids when brought in contact, unless one of them is plastic ; but this is only because their surfaces are not brought sufficiently close together. Adhesion between solids and liquids is also familiar. In a large majority of cases, when a liquid and a solid are brought in contact, the liquid clings to the solid and wets it. This is because adhe- sion between the two is greater than cohesion within the liquid. Thus when the finger is dipped in water and removed, the layer of water in contact with the finger is held by adhesion with suffi- cient force to tear it away from the adjacent molecules of water. In some cases a solid is not wet by a liquid. Water, for example, does not wet a surface covered with grease or wax, and mercury wets but few substances. In such cases the liquid clings together in somewhat flattened drops upon the surface of the solid (Fig. 115). This behavior of the liquid does not prove that adhesion is wanting. On the contrary, there is direct experimental iG. 115. evidence of adhesion ; and, between gla§s and mercury, it is even very considerable (Laboratory Ex. 3). The explanation is that, in such cases, cohesion in the liquid is stronger than adhesion, whatever the strength of the latter may be. Gases also adhere to solids, forming a very thin but dense layer upon their surface. In setting up a barometer, air adheres to the inner wall of the tube, and is driven off only by heating the mer- cury till it boils. The small bubbles of air that gather upon the side of a glass of water as it becomes warm are held there by adhesion with sufficient force to overcome the buoyancy of the water. 194. Cohesion and Gravitation Compared. — We know the law of gravitation, but not its cause (Art. 1 29). We know neither the law nor the cause of cohesion ; but it is evident that the law is very different from that of gravitation, for cohesion acts only at Surface Tension and Capillarity 151 insensible distances, and within such distances it is enormously stronger than gravitation between the same masses. Hence the strength of bodies in general depends practically entirely on cohe- sion, and gravitation becomes appreciable only in bodies of very great size. The strength of the earth depends almost wholly on gravitation. If we suppose the earth to be divided into hemi- spheres by any plane through its center, the gravitational attraction by which the hemispheres are held together is one hundred times as great as cohesion would be if the earth were made of solid steel. If there were a planet fifty miles in diameter having the same density as the earth and the tenacity of sandstone, gravi- tation and cohesion would be equally effective in keeping it together. IV. Surface Tension and Capillarity 195. Surface Tension. — A pin or a needle can be made to float on water, if carefully laid upon the surface so that neither end touches the water before the other. If the pin sinks and becomes wet, it should be dried by rubbing it between the fingers or in the hair, as this covers it with a coating of oil and diminishes the adhesion of the water to it {Exp.). The floating pin lies in a depression or trough which is several times larger than itself (represented in cross-section in Fig. 116). It is, in fact, sup- ported in much the same way as a person is when lying in a hammock ; the cords of the hammock are under tension, and this tension, ?^3§^^§Q acting obliquely upward on all sides, constitutes ~-^-f= :^^^r^£3-iEf the supporting force. Similarly, the floating of ^^^' ^^^• the pin is explained by supposing the surface of the water to be somewhat tough and in a state of tension. The properties of the surfaces of liquids can be studied to advantage by means of liquid films. It can be shown by a num- ber of simple experiments that soap films and soap bubbles are in 152 Some Properties of Matter a state of tension^ (Laboratory Exercise 4). A soap bubble is spherical, like a toy balloon, because the film of the bubble is in a state of uniform tension throughout, just as the rubber of the bal- loon is. Since a spherical surface is smaller than any other that incloses an equal volume, the film of a bubble assumes this shape in shrinking as much as possible. A drop of any liquid, when freed from the distorting effect of its weight, as in falling, is spherical. A drop of oil suspended in a solution of alcohol and water of its own density is an excellent illustration (Exp,). The spherical form of a drop is due neither to the mutual gravitation of its particles nor to cohesion acting throughout its mass, but to the tension of its surface. Its surface, like the film of a bubble, contracts as much as possible, and when thus contracted is spherical. Laboratory Exercise 4. 196. Cause of Surface Tension. — Each molecule of a liquid has hundreds, perhaps thousands, of neighbors near enough to attract it by cohesion, all of which are inclosed within a spheri- cal surface having the given molecule as a center and a radius equal to the greatest distance to which cohesion can act (a dis- tance of less than microscopic magnitude). Any molecule of a liquid whose distance from the surface is greater than the radius of such a sphere is attracted equally in all directions, since the molecules within the range of cohesion are uniformly disturbed around it. A molecule at the surface, however, is attracted inward, but not outward ; and any molecule whose distance from the sur- face is less than the range of cohesion is more strongly attracted inward than outward, since the greater number of the molecules that are near enough to attract it lie on the inside. The result is that the molecules at the free surface of a liquid exert a strong inward pressure, which tends to reduce the surface to the least possible area, the effect being the same as if the liquid were 1 Recipe for a good soap solution : Put 2 oz. of Castile or palm-oil soap, shaved thin, in i pt. of distilled or rain water. Shake, pour off the clear solution, add to it \ pt. of glycerine, and stir. Surface Tension and Capillarity 153 inclosed in a stretched, elastic membrane. Thus the surface tension of a liquid is due to the action of cohesion at its surface. 197. Surface Tension of Different Liquids. — The surface ten- sion of different liquids has been determined by experiment, and it has been found to be greater for water than for any other liquid except mercury ; hence the surface tension of water is diminished by mixing any other substance with it. This is readily illustrated by placing a drop of alcohol, ether, or oil on the surface of a tum- bler of water beside a floating sliver of wood. The bit of wood is quickly jerked away from the drop by the greater tension of the pure water on the other side {Exp.). 198. Surface Viscosity. — The surface of most liquids becomes more viscous than the interior mass after exposure to the air for some time ; and it is to this superficial viscosity, rather than to surface tension, that the strength of a liquid film is due. Only very small bubbles can be formed on the surface of pure water, and these quickly break, for the particles rapidly slip away from the highest part of the bubble, leaving it too thin to hold. The particles in a soap film move much more sluggishly, on account of their greater viscosity ; hence a much longer time elapses before any part of the film becomes so thin as to break, although 'the surface tension of the film is less than that of pure water. 199. Capillarity. — The combined action of surface tension and adhesion, when a liquid and a solid are in contact, gives rise to a class of phenomena, called capillary pheti07?iena because they are most conspicuous in tubes of small bore (Latin capilliis, a hair). Capillary action and capillarity are general terms for such phenomena. There are two types of cases to be considered, represented respectively by water and mercury, each in contact with glass. The surface of water in a clean glass vessel is turned sharply up at the edge in a smooth curve (Fig. 117); while the sur- face of mercury is curved downward at the edge (Fig. 118) 154 Some Properties of Matter (£x/.). In all cases where adhesion exceeds cohesion in the liquid (cases in which the liquid wets the solid), the edge of the liquid is drawn up against the surface of the solid ; in all cases where cohesion in the liquid exceeds adhesion (cases in which the solid is not wet by the liquid), the edge of the liquid is draw*?f'' inward and away from the surface of the solid. When small glass tubes of different bore are held vertically in water, the water rises in each above the level in the vessel, and stands higher in the tube of smaller bore {Exp.), The surface i (f) if mill Fig. 117. Fu;. lid. of the water in the tube is concave (viewed from above), and is curved throughout, forming a hemisphere, if the tube is not too large. This curved surface, like that of a soap bubble, exerts a pressure on the concave side, and thus partly sustains the pressure of the air upon it. The water therefore rises in the tube till equi- librium is restored. Atmospheric pressure, however, is not essential to capillary action. The water would stand at the same level in the tubes if the vessel and contents were placed in a vacuum ; for the concave surface in the tube would exert the same upward force as before, and would rise, carrying the column with it by cohesion. The greater elevation of the water in the smaller tube is due to Surface Tension and Capillarity 155 the fact that the curvature of its surface is greater (radius of curva- ture less) ; for it can be proved mathematically that the pressure (per unit area) exerted toward the concave side by a curved sur- face under a given tension is inversely proportional to the radius of curvature of the surface. Thus if the diameter of the smaller tube is one half that of the larger, the upward pressure exerted by the water surface in it will be twice as great and will support a column of water twice as high as that in the larger. Mercury stands at a lower level in capillary tubes than it does in the containing vessel, and the surface in the tubes is convex (Fig. 118) {Exp.). The pressure exerted by the curved surface is toward the concave side, as with water ; but it causes depression in this case, as the concave side is downward. The depression is inversely proportional to the diameier of the tube, for the reasons given in the case of capillary elevation. Experiments with other liquids and tubes of other materials would yield results agreeing with the cases considered, as expressed in the following laws : — I. If a liquid wets a capillary tube, its surface is concave and it is drawn up ; if it does not wet the tube, its surface is convex and it is depressed. II. The elevation or the depression in a capillary tube is in- versely proportional to the diameter of the tube. 200. Illustrations of Capillary Action. — The sensible pores of solids serve as capillary tubes in absorbing liquids. The absorp- tion of water by a sponge, of ink by blotting paper, and of coffee by a lump of sugar, are familiar examples. The flame of a lamp is fed by oil which is drawn up through the wick by capillary action. In dry weather the moisture is drawn up from a depth of many feet through the pores in the soil, and evaporates at the surface. Cultivation of the soil increases the size of the pores, and conse- quently checks the rise of water through the cultivated layer, thus diminishing the loss by evaporation at the surface. Capillary action would enable a short siphon having a capillary bore to work in a vacuum. 156 Some Properties of Matter PROBLEMS 1. What is the distinction between a theory and a law? between a theory and a fact ? Is a law a fact ? 2. What is the essential difference between a law of nature and a law enacted by a legislative body? 3. If a gas is heated but not permitted to expand, how is the pressure that it exerts affected ? Explain. 4. Capillary phenomena are sometimes said to be due to " capillary at- traction." What b capillary attraction? V. Properties due to Molecular Forces 201. Molecular forces give rise to different specific properties in different substances. One of these, tenacity, has already been considered (Art. 190). The list includes also elasticity, plasticity, brittleness, malleability,- ductility, and viscosity. 202. Elasticity. — Elasticity is the property of matter in virtue of which bodies resume their original form or volume when any force that has altered their form or volume is removed. Elasticity of volume is shown by recovery of volume after compression. It is a general property of matter and is due to molecular pressure. All fluids have perfect elasticity of volume ; />. however great the compression, they always expand to their original volume when the pressure is removed. Solids, however, may be permanently diminished in volume to a slight extent by the application of sufficient pressure. The rolling and stamping to which silver is subjected in the process of coining causes a decrease of volume amounting to about four per cent. Elasticity of form is a specific property possessed only by cer- tain solids. It is shown by recovery of form after distortion. An elastic solid is able to recover from distortion whether caused by compression, stretching, twisting, or bending. Rubber is a fa- miliar example. Solids, such as soft putty or clay, which have no power to recover from distortion, are called inelastic or plastic. 203. Limit of Perfect Elasticity. — An elastic solid has perfect elasticity only for distortion within a certain limit, called the limit Properties due to Molecular Forces 157 of perfect elasticity, or generally, the limit of elasticity. When a body is distorted beyond its limit of elasticity, it either breaks or takes a permanent set, i.e: undergoes a permanent change of form {Exp.). In the first case the solid is said to be brittle; in the second case tough, malleable, or ductile, according to the manner in which its form can be changed (Art. 207). It is a mistake to regard brittle substances as inelastic. A long, slender strip of glass or piece of glass tubing is quite flexible and springs back to its former shape when released {Exp.) ; within its limit of elas- ticity glass is perfectly elastic. Substances differ widely in their limits of elasticity. A piece of soft copper wire takes a permanent set before it is bent far, — its limit of elasticity is small. A piece of steel wire can be bent many times farther without a permanent change of form {Exp.). Rub- ber is remarkable for its large limit of elasticity. There is no limit to the elasticity of volume of fluids. However great the pressure to which a fluid may be subjected, recovery of volume is always complete when the pressure is removed. 204. Elastic Force ; Measure of Elasticity. — In common speech we say that a body is very elastic or highly elastic if its limit of elasticity is large (as rubber), or if it is highly compress- ible (as gases). In scientific usage these terms have an alto- gether different meaning. The elastic force of a body, or the force with which it tends to recover from compression or distor- tion, is the measure of its elasticity. The elasticity of a gas is measured by the pressure (per unit area) which it exerts upon the sides t>f the containing vessel, and is increased by compression (Art. 44). The elasticity of liquids is much greater than that of gases, and the elasticity of ivory, glass, or steel is very great compared with that of rubber. 205. Elastic Impact. — When an elastic sphere (rubber, ivory, steel, or hardwood ball, or glass marble) is dropped upon a smooth, rigid surface, as a large, flat plate of stone or steel, it rebounds nearly to the height from which it was dropped {Exp.). The rebound is explained as follows : The force of the impact flattens 158 Some Properties of Matter the ball very slightly before it is stopped ; but, being elastic, it instantly recovers its form, and, in doing so, // continues to press against the plate^ much as a boy pushes against the ground in the act of jumping, and with a similar result. Although the ball recovers its form completely, the force with which it does so is in all cases somewhat less than the distorting force. If the recovery of force \yere complete, the ball would rebound to the height from which it was dropped, but this is impossible, as some of the energy of the ball is transformed by the impact into heat and sound. The experiment proves the elas- ticity of bodies that are often regarded as perfectly rigid. More- over, by this test, the elasticity of glass is much more nearly perfect than that of nibber. (How shown?) 206. Stress and Strain. — Any force or combination of forces tending to change the shape or size of a body is called a stress. A rubber band is stretched by two equal and opposite pulls, con- stituting a tensiie stress. A tensile stress causes elongation. A stress consisting of equal and opposite pressures causes compres- sion. Any change of shape or size of a body, especially of a solid, produced by the action of a stress, is called a strain. A body in which a stress produces no appreciable strain is called rigid ; but no body is perfectly rigid, i.e. absolutely unyielding to stress. In the study of the mechanics of solids we have disre- garded the strains produced by the forces under consideration. 207. Plasticity; Malleability and Ductility. — The specific properties of bodies have no sharply defined limits ; on the con- trary, they merge insensibly into one another in numerous instances, and the names of such properties have, in consequence, a variable meaning. This is the case with the term plasticity, which, in the customary and narrow sense, is applied to bodies that can be molded by moderate pressure into any desired form. Soft putty and clay are typical examples. But gold and silver exhibit es- sentially the same property under much greater pressure, but at ordinary temperatures, when they receive the impression of the die or mold in stamping coins ; and are therefore, in a broader Properties due to Molecular Forces 159 sense, called plastic. In this sense all elastic bodies that are not brittle are plastic beyond their limit of elasticity. This form of plasticity is, however, generally called malleability or ductility. A substance is said to be malleable if it can be hammered or rolled into sheets ; duciiky if it can be drawn out into the form of a wire. In both cases ordinary temperatures are to be understood unless otherwise stated. Thus we should say that glass is brittle, not ductile ; but glass is very ductile when heated to redness {Exp^, Gold, silver, and platinum are the most ductile metals, gold the most malleable. Gold has been beaten into leaves so thin that six hundred of them placed one upon another, would have a thickness no greater than the paper upon which this is printed. 208. Viscosity and Mobility. — A substance is said to be viscous if its form changes more or less slowly under the action of its own weight. Shoemaker's wax, pitch, and molasses candy slightly warmed are examples of viscous solids. Such substances are sometimes classed as liquids, since, when unsupported at the sides, they slowly flatten out, or flow. Molasses and honey are examples of viscous liquids. The term is commonly applied only to those liquids that possess the property in a considerable degree, and liquids that flow readily, as water and alcohol, are called mobile. But all liquids and gases possess viscosity in some degree. Viscosity is that property, due to internal or molecular fric- tion, in virtue of which liquids, gases, and some solids offer re- sistance to an instantaneous change of their shape or of the arrangement of their parts, although they offer no permanent re- sistance to such change. The viscosity of water is shown by the behavior of a bowl or tumbler of water that has been stirred till it is rapidly rotating. If the motion of the different portions of the water is made visible by means of sawdust or other floating particles, it will be found that the rate of rotation steadily de- creases, and at any instant is greatest at the center and least at the sides of the vessel (^Exp.), The explanation is that friction i6o Some Properties of Matter against the sides of the vessel retards the layer of water in contact with it, and this layer in turn retards the more rapidly moving layer next within. This retarding action — due to inter- nal friction, as adjacent layers slip over one another in their un- equal motion — extends throughout the entire mass, and finally brings the whole to rest. The dividing line between viscous liquids and plastic solids is not clearly defined ; the two classes merge insensibly into each other. Molasses candy, in cooling, passes continuously from the stale of a viscous liquid to that of a plastic solid ; and, on cooling further, becomes hard and brittle. 209. Hardness. — A body is said to be harder than another if it can be used to scratch the latter but cannot be scratched by it. Diamond is the hardest substance known. Pure metals are softer than their alloys; hence gold and silver used for money and jewelry are alloyed with copper to increase their hardness. Steel is made very hard by sudden cooling after it has been raised to a high temperature. The process is called tempering. All cutting instruments are made of tempered steel. PROBLEMS 1. The top of a river flows faster than the bottom, and the middle flows faster than the sides. Why? 2. Write a list of all the general projierties of matter that have been con- sidered in this or in previous chapters. Write a similar list of specific prop- erties. CHAPTER VIII HEAT I. Heat and Temperature 210. The Caloric Theory. — Before the final acceptance of the present theory of heat (Art. 187) about the middle of the last century, heat was very generally supposed to be an invisible fluid without weight, which could of itself pass from a hotter to a colder body. This supposed fluid was called caloric (Latin calor^ heat). With the overthrow of the theory, the word itself has become obsolete ; but the root occurs in several words in common use, among which are calorie, one of the heat units ; caloritnetry, the art or process of measuring heat ; and calorimeter, a vessel in which substances are placed in measuring their gain or loss of heat. The use of these words does not imply any reference to the caloric theory; but, unfortunately, the terms latetit heat and radiant heat, which also owe their origin to the caloric theory, are distinctly misleading, for neither is heat at all. 211. The Mechanical Theory of Heat: Historical. — " The first prominent physicist who endeavored to overthrow the caloric theory of heat was Benjamin Thompson" (1753-1814), a native of Massachusetts. He is better known as Count Rumford, having received that title from the Elector of Bavaria, whose service he entered while still a young man. While engaged in the boring of cannon for the Bavarian government, he was surprised at the heat generated. " Whence comes this heat ? What is its nature ? He arranged apparatus so that the heat generated by the friction of a blunt steel borer raised the temperature of a quantity of water. In his third experiment, water rose in one hour to 107° 161 1 62 Heat Fahrenheit; in one hour and a half to 142° ; *at the end of two hours and thirty minutes the water actually boiled.' * It is difficult to describe the surprise and astonishment,' says Rumford, ' ex- pressed in the countenances of the bystanders, on seeing so large a quantity of cold water (i8| lb.) heated, and actually made to boil without any fire.' . . . The source of heat generated by fric- tion * appeared evidently to be inexhaustible.' The reasoning by which he concluded that heat was not matter, but was due to motion, we can give only in part. He says, * It is hardly neces- sary to add that anything which any insulated body, or system of bodies, can continue to furnish without limitation, cannot possibly be a material substance ; and it appears to me extremely difficult, if not quite impossible, to form any distinct idea of anything ca- pable of being excited and communicated in the manner in which heat was excited and communicated in these experiments, except it be motion.* " Rumford 's conclusion regarding the nature of heat was vigor- ously attacked by the calorists, but it was confirmed in 1 799 by Sir Humphry Davy. By means of clockwork he rubbed two pieces of ice against one another in the vacuum of an air pump. Part of the ice was melted, although the temperature of the re- ceiver was kept below the freezing point. From this he con- cluded that friction causes vibration of the corpuscles of bodies, and this vibration is heat." — Cajori's History of Physics. Notwithstanding the work of Rumford and Davy, but few physicists were convinced. In fact, the caloric theory was not completely discredited until after J. P. Joule, an Englishman, had proved, by a series of experiments extending over a period of ten years (1840 to 1850), that the amount of heat which can be generated by a given amount of mechanical work is invariable (Art. 270). 212. Sources of Heat. — All other forms of energy are capable of transformation into heat. Mechanical energy is transformed into heat by friction and impact, as we have already seen, and also by compression. Heat due to compression is appreciable Heat and Temperature 163 only in gases, and is familiar in the heating of a bicycle pump when in use {Exp.). The heating is not due to the friction of the piston, to any appreciable extent, but to the compression of the air. The heat thus developed is, in fact, the exact equivalent of the mechanical work done in compressing the air. Chemical action is the most important source of heat, with the exception of the sun. The burning of any substance is an exam- ple. When a substance burns, its molecules are broken up, and their parts (atoms) unite with oxygen from the air. New sub- stances are thus formed, which are in most cases gases. It is not surprising that, in this violent rearrangement of molecular struc- ture, the motion of the molecules should be greatly increased. Heat is also generated by other chemical processes. For exam- ple, when water is poured on quicklime, the two unite chemically, forming slaked lime, and the lime becomes very hot {Exp.). Similarly, when strong sulphuric acid is poured into water, the mixture becomes very hot {Exp.). The transformation of other forms of energy into heat is con- sidered in connection with other topics. 213. Temperature. — The relation between heat and tempera- ture is similar to that between quantity of water and water level. If two vessels containing water are in communication, we know that the flow will be from the one in which the water stands at the higher level to the other, whether the one or the other con- tains the greater quantity of water. Similarly, the transfer of heat between two bodies or between parts of the same body is always from the hotter to the cooler, whether the quantity of heat in the former be greater or less than that in the latter ; and this transfer- ence will cease as soon as both are at the same temperature. Temperature is therefore defined as the condition of bodies that determines the direction in which the transfer of heat can take place between them. Or, since the temperature of a body is higher the greater the amount of heat it contains, temperature may be defined as the ititeiisity or degree of heat (not the quantity of heat). 164 Heat 214. Temperature Sensations. — Our bodily sensations of heat and cold afford direct but inexact and often misleading infor- mation concerning the temperature of bodies ; they afford no information whatever concerning the relative amount of heat in different bodies (Art. 217). PROBLEMS 1. What is ihe meaning of the adjective cold? of the noun cold? 2. A body {x>sscsses heat as lung as it is capable of becoming colder. Is there any heat in ice? 3. (a) According to the theory of heat, what would be the molecular condition of a body having no heat? {h) Why could not such a body be a gas? 4. Mention any familiar instances in which ccjual temperatures do not cause equal temiierature sensations. II. The Transmission of Heat 215. The transference of heat as heat from one place to another takes place in two ways; namely, by conduction and by convection. Laboratory Exercise .?/. 216. Conduction. — Conduction is the transmission of heat from hotter to colder parts of a body, or from a hotter to a colder body in contact with it, without change in the relative positions of the parts of the body. It is the only process by which heat travels in solids. The heating of the farther end of a poker when one end is placed in a fire, and the heating of the handle of a spoon placed in a cup of hot tea are familiar examples. The kinetic theory suggests a mental picture of the process of heat conduction. When any part of a body is heated, its mole- cules are set in more rapid vibration. These molecules jostle their neighbors more violently, increasing the energy of their vibra- tion. The disturbance thus spreads throughout the body without change in the relative positions of the molecules themselves. In conduction, therefore, molecular energy is transmitted without the transmission of matter. Substances differ widely in their conductivity, i.e. their power of The Transmission of Heat 165 transmitting heat by conduction. The metals are the best con- ductors of heat ; other solids, with few exceptions, are better conduct- ors than liquids. Liquids, with the exception of mercury and mol- ten metals, are very poor conduct- ors. Water can be boiled at the top of a test tube for several min- utes, while the greater part of it remains cold (Fig. 119) (£x/>.). But wood and paper, especially the latter, are much poorer conductors than water (see table below). Gases are practically nonconduct- ors. In testing the conductivity of liquids and gases they must be heated at the top to prevent currents (Art. 218). The following table gives the conductivities of various substances referred to silver as the standard : — Fig. 119. Tad/e of Conductivities for Heat. (^Approximations^ Silver icxj Copper 74 Brass 27 Iron 12 Lead 8.5 Mercury 1.35 Ice 0.20 Glass 0.20 Marble 0.15 Water 0.14 . Wood 0.04 Writing paper 0.012 Wool 0.009 Air 0.005 217. Illustrations of Good and Poor Conductivity. — On a cold morning the ^oox feels colder to the bare feet than the carpet or a rug, and water that has been standing in the room over night feels colder to the face than the air. These and other objects in the room, which seem to be unequally cold, are all at the same tem- perature as the air. The difference in the sensations is largely due to the difference in the conductivities of the substances touched. If the body touched is a good conductor, heat is rapidly conducted to all parts of it from the hand \ and this continue^ a§ long as the 1 66 Heat hand remains in contact with it or until it becomes warm through- out. This rapid and continued loss of heat makes the hand cold. If the body touched is a poor conductor, but little heat is lost from the hand in warming the part of it that is touched. Similarly, if hot substances at the same temperature but of different conduc- tivities are touched, the best conductors feel the hottest because they conduct heat to the hand most rapidly, and hence make the hand hotter than the poorer conductors do. (The temperature sensation caused by a body depends also in part upon another property, called specific heat, which will be studied later.) The low conducting power of air is utilized in refrigerators and ice houses, which have double walls filled between with charcoal, sawdust, straw, or other loose, badly conducting material, which hinders the circulation of the air. The warmth of fur, feathers, and wool is partly due to the air entangled in them. PROBLEMS 1. What is the advantage of the poor conductivity of wood in using matches? 2. An overcoat is said to " keep out the cold." What is it that it really does? 3. Why is woolen clothing warmer than cotton or linen? 4. Would it l>e better to wrap a piece of ice in a woolen or a cotton cloth to keep it from melting? 5. What is the advantage of having the bottoms of tin teakettles and boilers made of copper? Laboratory Exercise 28. 218. Convection. — The transmission of heat in a liquid or a gas by currents due to unequal temperatures in its different parts is called convection , and the currents are called convection cur- rents. In heating liquids, the heat is applied to the lx)ttom of the vessel. The liquid at the bottom receives heat from the vessel by conduction and expands, thus becoming less dense. It is then displaced by the denser liquid at the top, producing convection currents. Radiation 167 Convection currents in air and other gases are due to the same cause. The strong ascending current above a bonfire is indicated by the leaping of the flames and the rapid rise of sparks and smoke. The fire is fed by inward-flowing currents near the ground. They occupy much more space than the ascending current, and hence move more slowly and are less noticeable. PROBLEMS 1. Would convection currents be caused by heating a liquid at the top? by cooling it at the top? l)y cooling it at the bottom? 2. What would be the general direction of convection currents in a room heated by a stove at one end of the room? Would the air be warmer near the floor or near the ceiling? 3. What convection currents are set up when a door is left open between a warm and a cold room ? 4. Why do openings at the top and bottom of a window provide better ventilation than a single opening of the same total area at either top or bottom? 5. A fire in a fireplace provides excellent ventilation for a room. Explain. 6. Docs an open fireplace provide as good ventilation whether there is a fire in it or not? 7. How is the flame of a lamp provided with the constant supply of oxygen necessary for combustion? III. Radiation Laboratory Exercise 2^ {l^ a and <5, and II, dr and b), 219. An Experiment on Radiation. — When the hand is held close besiWe a hot flame, as that of a Bunsen burner, the side of the hand turned toward the flame becomes hot. The hand is not heated by convection, for it is in the path of the currents of cold air moving toward the flame. When any object, as a sheet of paper, is placed as a screen between the hand and the flame, the hand instantly ceases to feel the heat, which shows that it could not have been heated by conduction, for three reasons: (i) be- cause the screen is at least as good a conductor as the air ; (2) if the process were conduction, the air must have been at least as warm as the hand and it could not instantly become cold on inter- 1 68 Heat posing the screen ; and (3) both sides of the hand would have been warmed, for convection currents would prevent any consider- able difference in the temperature of the air on the two sides. The conclusion is therefore certain that, when the hand is beside the flame with nothing interposed between, the side turned toward the flame becomes much hotter than the air at that distance, and that it is heated neither by conduction nor convection. The conditions of this experiment are repeated on a large scale when we stand near a bonfire in cold weather. Most people know by experience of the last situation what it means to " roast on one side and freeze on the other." 220. The Transformation of Heat into Radiant Energy and of Radiant Energy into Heat. — All hot bodies lose heat by a pro- cess called ratiiation, which is independent of conduction and con- vection and is totally different from either. But radiation is not a process by which heat is transmitted ; for the heat is transformed at the radiating body into another form of energy, called radiant energy^ and is transmitted as such until it meets some body capa- ble of transforming it back into heat. Tlie transformation of radiant energy into heat is called absorp- tion. Absorption takes place at the surface of some bodies, as at the surface of the hand in the preceding experiment ; in other cases it takes place within the body through which the radiant energy is passing. A body is heated only by the part of the radiant energy that it absorbs. Air absorbs comparatively little, hence is only slightly heated by radiation. The transformation of radiant energy into heat by absorption may l>e compared to the transfor- mation of the kinetic energy of a flying bullet into heat by impact against a steel target. Radiant energy is as distinctly dififerent from heat as is the kinetic energy of the bullet. 221. Luminous and Nonluminous Radiation. — Radiant energy is often called radiation ; thus radiation may mean either a form of energy or the process by which that energy is transmitted. Radiant energy includes luminous radiation, or lights as well as the Donluminous or dark radiation previously considered. The dis- Radiation 169 tinction between light and nonluminous radiation is a physiologi- cal rather than a physical one, and is due to the fact that the optic nerve is sensitive to the one and not to the other. The two kinds of radiation are the same form of energy. A hot body, as a piece of iron, gives out only dark radiation below a certain temperature ; at " red heat " or above it radiates light also. Light is due to the transformation of heat into radiant energy at sufficiently high temperatures ; and, like dark radiation, it is again transformed into heat by absorption. The energy of dark radiation is greater than that of light ; hence it causes greater heating when absorbed. Before heat was recog- nized as a form of energy (Art. 210) it was supposed that dark radiation was a form of heat and was essentially different from light ; it was therefore called " radiant heat," and its transmission was called the " radiation of heat." These terms are still com- mon ; but their use should be avoided, at least by the beginner. 222. Radiant Energy can be transmitted in a Vacuum. — Neither air nor any other form of matter that we have yet con- sidered is necessary for the transmission of radiation. This is evident from the fact that we receive radiant energy from the sun over a distance of 93,000,000 miles ; through all of which space, till the earth's atmosphere is reached, there is what we call a perfect vacuum. The incandescent electric light affords another illustration on a small scale. When the filament of the lamp is heated by the electric current, it sends out both luminous and nonluminous radiation, yet within the bulb there is a very nearly perfect vacuum. Hitherto we have found energy only in connection with matter ; in fact, matter is often called " the vehicle of energy." How, then, does energy travel in a vacuum ? The question is answered by the theory of radiant energy ; which, together with the laws of radiation, will be considered under the subject of light. One law of radiation was illustrated when the screen was interposed between the Bunsen flame and the hand : the radiation did not pass round the screen. Radiation is transmitted along a straight 170 Heat path in a vacuum and in all homogeneous substances capable of transmitting it. 223. The Radiometer. — The radiometer (Fig. 1 20) consists of four light vanes of mica or aluminum attached to a vertical axis, and inclosed in a glass bulb containing a small quantity of air under very low pressure. One side of each vane is bright, the other is coated with lampblack. When the instrument is placed in the sunshine or in the path of other radiation, the vanes rotate with their bright side in advance. The rotation of the vanes is explained as follows : The black surfaces absorb more radiation than the bright, and hence are warmer. The molecules of the rare- fied air that strike the blackened surfaces are heated, and rebound with greater veloc- ity than those that strike the bright sides. This causes a greater pressure upon the black side of each vane than upon the other ; hence the rotation. If the air in the bulb were not highly rarefied, there would be no rotation, for the collisions among the molecules would be so frequent as to equalize the pres- sures throughout the bulb. The rate of rotation of the vanes serves as a rough measure of the energy of the radiation falling upon them ; hence the instru- ment is very useful in the study of radiation (see Lab. Ex. 29). 224. Effects of Matter upon Radiation. — When radiant energy falls upon any substance, it may be (i) absorbed at the surface, (2) reflected by the surface, (3) transmitted through the sub- stance, or (4) wholly or partly absorbed by the substance during transmission. Generally two and often three of these effects occur simultaneously with different portions of the radiation. The study of these effects will be continued under the subject of light. 225. Reflection and Absorption at Surfaces. — In general, the Fig. laa Radiation 171 surfaces of substances that transmit no radiation reflect part and absorb the remainder ; they are heated only by the absorbed radiation. Lampblack is the best absorber known ; it absorbs practically all of the radiation that falls upon it, both luminous and nonluminous. Any polished metal reflects much the greater part of all radiation and absorbs the remainder. A piece of tin coated with lampblack or painted black on the side turned toward a flame will therefore become hot, while a piece of bright tin in the same situation will be only slightly warmed. A white surface reflects nearly all luminous radiation that falls upon it, a black surface re- flects almost none, a colored surface reflects part and absorbs part. 226. Selective Absorption. — Substances that transmit d^irk radiation, with but little absorption if any, are called diatherma- nous (Greek therme, heat) ; those that transmit little or none are called athennanous. The terms have the same meaning with respect to dark radiation that transparent and opaque have with respect to light. The power of most substances to transmit radiation depends very largely upon the temperature of the source of the radiation. Some substances that transmit light also transinit dark radiation,^ others do not. Clear glass transmits light and also a considerable portion of the radiation from bodies nearly red hot, but absorbs all or nearly all of the radiation from colder bodies. Thus solar radiation enters a sunny room in large quantities through the windows, and is absorbed by the objects upon which it falls. But, as the radiation from these bodies cannot penetrate glass, the solar energy is entrapped in the room, which may thus become con- siderably warmer than the air outside. This explains the accu- mulation of heat in greenhouses. Rock salt transmits all radiation, being highly transparent and diathermanous. A solution of iodine in carbon disulphide is perfectly opaque but diathermanous ; water in its three states is transparent but highly athermanous (Lab. Ex. 29). The unequal absorption of luminous and dark radiation by the same substance is called selective absorption. 172 Heat 227. Relation of Radiating and Absorbing Powers. — If two metal vessels of the same size and material, one highly polished and the other coated on the outside with lampblack, are filled with equal quantities of hot water at the same temperature and are allowed to stand for some minutes, it will be found that the tem- perature of the water in the blackened vessel is considerably lower than that in the other {Exp.). The difference in the rate of cool- ing is due to the more rapid radiation from the blackened surface. The experiment illustrates the fact that good absorbers of radiation are also good radiators, and poor absorbers poor radiators. 228. The Heating of the Atmosphere. — It is well known that the atmosphere is colder at higher than at lower altitudes. Aero- nauts always find intense cold at altitudes above three or four miles, and the tops of high mountains are covered with perpetual snow. The low temperature of high altitudes is due to the fact that the dry and rarefied air absorbs but little of the enormous quantity of radiant energy that passes through it. As the radiation approaches the earth, the rate of absorption rapidly increases, principally on account of the greater amount of water vapor ; for experiments have shown that the absorbing power of air containing the average amount of water vapor is seventy-two times as great as that of perfectly dry air of the same density. The absorption at lower levels is further increased by the dust particles in the air. But notwithstanding the loss by absorption on the way through the atmosphere, it is estimated that from two thirds to three fourths of the solar radiation reaches the earth. Much of this is absorbed by the surface of the land and the ocean ; the remainder is re- flected. The reflected radiation is partly absorbed on its way out through the atmosphere again. The absorbed radiation warms the surface of the land, and this in turn warms the air in contact with it. This is especially noticeable on a hot day in summer, when, if there is no wind, the air close to the ground is many degrees warmer than at a height of a few feet. The heating of the air at the bottom causes convection currents (winds), by which the heat Temperature and Expansion 173 is carried to considerable altitudes; but the temperature is, of course, highest at the source of the heat^ i.e. at the earth's sur- face. The earth is cooled at night principally by radiation. The loss is rapid on clear nights, especially when the atmosphere is very dry ; but is checked in a large degree by moisture, especially by clouds, which absorb the radiation before it has passed through them, thus serving as a blanket to the earth. Hence clear nights are, as a rule, the coldest At high altitudes, where there is but little hindrance to radiation either by day or by night, sheltered valleys are quickly warmed in summer by the early morning sun- shine ; and a sudden chill immediately follows the disappearance of the sun in the evening, the nights being often cold enough for frost. Thus we see that the atmosphere, or rather the moisture in it, performs an indispensable function in moderating the intensity of solar radiation by day and retaining the heat by night. PROBLEMS 1. Why does snow melt more quickly when covered with a thin layer of earth? 2. Why is Hght-colored clothing more comfortable in summer than black? 3. Why is the difference between the temperature in the sunlight and in the shade greater upon the top of a mountain than at a low elevation? 4. Why must those who climb snow-covered mountains take especial care to protect their faces?' IV. Measurement of Temperature and Expansion 229. Measurement of Temperature. — Any instrument for meas- uring temperatures is called a thermometer. In most forms of thermometers the effect of heat in changing the volume of some substance is utilized. Solids are rarely used, as their expansion is small and they are otherwise inconvenient. It is important that the substance chosen should have a uniform expansion ; i.e. equal 174 Heat quantities of heat should, cause equal increases of volume at all temperatures. Mercury fulfills this condition better than any other liquid, and has the further advantage of remaining a liquid through a very wide range of temperature. The apparent expansion of mercury in a glass vessel (/.<•. the difference between the expansion of mercury and glass) has therefore been adopted as the standard. For temperatures below the freezing point of mercury, alcohol thermometers are used, the freezing point of alcohol being — i3o°C. The air thermometer, in which the expansion of air is utilized, is adopted as the standard in the most accurate scientific work ; and it can be constructed of such form as to be of practical use in meas- uring temperatures above the boiling point of mercury, such as the temperatures of furnaces. 230. The Mercury Thermometer. — The mercury thermometer consists essentially of a capillary glass tube, called the stem, ter- minating in a bulb (Fig. 122). The bulb and a part of the stem are filled with mercury, and the expansion is measured by a scale engraved upon the stem or attached to it. In making a thermom- eter the mercury is heated to drive out all the air before the stem is sealed at the top ; hence the space in the tube above the mer- cury is a vacuum. 231. Determination of the Fixed Points. — Probably no two thermometers have bulbs of exactly the same capacity and tubes of exactly the same bore ; hence the readings of different ther- mometers would be entirely inconsistent with one another if they were provided with scales of equal length. The correct position and dimensions of the scale must therefore be determined sepa- rately for every thermometer. The first step in this process is to determine the " fixed points," called \k\^ freezing point diViA the boiling point. T\\^ freezing point is the temperature at which pure water freezes ; but since this is exactly the same as the temperature at which ice melts, whatever the surrounding temperature may be, it is most conveniently found by inserting the bulb of the thermometer in a dish of melt- Temperature and Expansion ^75 ing snow or crushed ice. The ice is packed about the bulb and stem, leaving the mercury just visible above it ; and a mark is made on the stem at the top of the mercury column after it comes to rest. The boiling point is the temperature at which pure water boils under a pressure of one atmos- phere. But, since the tempera- ture of the water is subject to appreciable changes from various causes while that of the escaping steam is constant, the thermom- eter is adjusted so as to be sur- rounded by the steam, as nearly as possible to the top of the mercury in the stem, and is not permitted to touch the water (Fig. 121). Since even a slight change in the atmospheric pressure causes an appreciable change in the tem- perature at which water boils (Art. 262), a correction must be applied to the observed height of the mercury in the stem if tlie barometric pressure is not 76 cm. when the boihng point is determined. 232. Centigrade and Fahrenheit Scales. — The distance between the fixed points is divided into equal parts called degrees. In the Centigrade scale the number of these divisions is 100, the freezing point being marked 0° and the boiling point 100°. The Centi- grade thermometer is almost exclusively used in scientific work. All temperatures referred to in this book are expressed in the Cen- tigrade scale unless otherwise indicated. In the Fahrenheit- scale the freezing point is marked 32° and the boiling point 212°, the interval between them being 180°. The Fahrenheit scale is the one in general use in this country. The scale of a thermometer may be extended to any desired distance beyond the fixed points. Temperatures below zero on either scale are indicated by the nega- tive sign, as — 15° C. Fig. lai. or THr 176 Heat c 00 F 212 3? ■a FlO. 122. Since the interval between the fixed points is loo Centigrade degrees or i8o Fahrenheit degrees, it follows that — I Centigrade degree = f Fahrenheit degrees, and I Fahrenheit degree = f Centigrade degrees. In changing a reading on either scale to the equivalent reading on the other, allowance must be made for the difference in the zero points. Example : 50° C. means 50 Centigrade degrees above the freezing point. This is equal to 50 x |, or 90 Fahrenheit degrees a dove the freezing pointy or to 122° F. 233. Linear Expansion of Solids. — With few exceptions, none of which are important, solids expand when heated and contract when cooled. Tiie total expansion or con- traction of any body depends upon its size and material as well as upon the change in temperature. The expansion of a solid takes place, of course, in its three dimensions ; but, in most cases, it is important only in the direction of its length. F^xpansion, when considered in one direction only, is called linear expansion. The expansion of a solid per unit of length when its tempera- ture rises one degree is called its coefficient of linear expansion. For example, the coefficient of linear expansion of oak is .000006, which means that each centimeter of its length increases to 1.000006 cm. with a rise of temperature of one degree Centi- grade. The coefficient of steel is .000012 — just twice that of oak ; hence the expansion of a piece of steel for any change of temperature is twice as great as that of a piece of oak of the same dimensions for the same change of temperature. The expansion of solids is so slight that some special device must be employed in order to measure with any degree of accu- racy the expansion of even a long rod for a considerable rise of temperature. The methods by which this is done are best studied in the laboratory. The computation of the coefficient from the Temperature and Expansion 177 data thus obtained is illustrated by the following example : A brass rod 90 cm. long expands .13 cm. when heated from 23° to 100°. Find its coefficient of linear expansion. The rise of temperature is 77 degrees; hence, assuming the expansion to be uniform^ the expansion of the rod for a rise of temperature of i degree is — cm., and the expansion of i cm. for a rise of temperature of i de- gree is — '—^ — , or .0000188 cm. ^ 77 X 90' The coefficient of linear expansion may equally well be re- garded as the ratio of the whole expansion to the whole length for a rise of temperature of one degree. Coefficients of Linear Expansion Zinc o.(xxx>294 Lead 0.0000286 Aluminum 0.000023 Brass 0.0000188 Copper ...... 0.0000172 Iron and Steel .... o.ooooi 22 Platinum 0.0000088 Glass 0.0000086 Wood, Dak 0.000006 Wood, Fir 0.0000035 Laboratory Exercise JO. 234. Effects and Applications of Expansion. — The force that a body can exert in expanding or contracting with change of temperature is equal to the force required to expand or compress it to the same extent by mechanical means. This force is enor- mous, and, under most circumstances, practically irresistible. If a bar of malleable iron one square inch in cross-section were placed between fixed supports, so as to make expansion impossible, and its temperature then raised 40°, it would exert a pressure of about five tons against the supports. The rails of tracks are laid with a small space between their ends, which provides room for expansion. A long steel bridge changes in length several inches between winter and summer, opportunity for this change being afforded by an expansion joint. The tire of a wagon wheel is made just large enough to go on 178 Heat when hot ; it shrinks upon the wheel in cooling, making a very tight fit. For a similar reason red-hot rivets are used in joining the steel plates of tanks and boilers. A wooden rod is better than one of metal for the pendulum of a clock, since its coefficient of expansion is less. 235. The Expansion of Liquids. — In considering the expan- sion of liquids and gases it is increase of volume, or cubical expan- sion^ with which we are concerned. The coefficient of cubical expansion of a solid or a liquid is its expansion per unit volume for a rise of temperature of one degree. As usually contrived, experiments on the expansion of liquids give their apparent expansion, i.e, the difference between their true expansion and the expansion of the containing vessel. The tnie expansion of a liquid is the sum of its apparent expansion and the cubical expansion of the material of the containing vessel. In general, a liquid expands more rapidly as the temperature approaches its boiling point. The following table gives the true average expansion of a few liquids : — Coefficients of Cubical Expansion Ether 0.0015 Alcohol (5° to 6**) . . . . 0.00105 Alcohol (49° to 50**) . . . 0.00122 Acetic acid 0.00105 Petroleum 0.0009 Olive oil 0.0008 Turpentine 0.0007 Glycerine 0.0005 Water (5° to 6°) . . . . 0.000022 Water (49° to 50°) . . . 0,00046 Water (99° to 100") . . . 0.00076 Mercury 0.00018 It can be shown that the coefficient of cubical expansion of a solid is three times its coefficient of linear expansion ; hence by multiplying the values given in the table under solids by three, a comparison can be made between the expansion of liquids and solids. It will be found that the expansion of liquids, though small, is considerably greater than that of solids. The total expansion of water between 4° and 100° is a little over four per cent. Laboratory Exercise ji. Temperature and Expansion 179 236. Importance of the Irregular Expansion of Water. — The expansion of water is curiously irregular. It contracts as its tem- perature rises from 0° to 4° ; when heated beyond this point it begins to expand, at first very slowly, then more and more rapidly (see table). Hence the density of water is greatest at 4° C. (about 39° F.). This behavior of water is of the greatest importance in the economy of nature. In winter the waters of lakes lose heat at the surface by contact with the cold air and by radiation. As the water at the surface cools, it becomes denser and sinks, displacing the warmer water at the bottom. These convection currents con- tinue until the water is cooled throughout to a temperature of 4° ; beyond this point the water at the surface expands as it cools and remains at the top. Thus the water at the surface freezes while that below remains at 4°, even in the most severe winters, — a temperature at which fishes and other inhabitants of the waters are not destroyed. Laboratory Exercise J2. 237. Expansion of Gases. — The effect of heat upon the vol- ume of gases was first accurately investigated by the French physi- cist, Jacques Charles, who discovered the law that bears his name. Law of Charles : The volume of any gas increases under constant pressure by -^-^ of its volume at zero (Centigrade) for each rise of temperature of one degree. The fraction ^|^, or .003665, is, according to the law, the co- efficient of cubical expansion for all gases at all temperatures, under any constant pressure. I^ter and more accurate experi- ments have shown that this law, like that of Boyle (Art. 47), is only approximately true ; though very nearly so indeed, unless the gas is near the temperature at which it liquefies. It can be shown by experiment or proven from the laws of Boyle and Charles that, when a gas is heated without being per- mitted to expand (volume constant), its pressure increases at the same rate as the volume does when it is heated under constant pressure. i8o Heat It is instructive to contrast the identical behavior of all gases as expressed by the laws of Boyle and Charles with the very marked individual differences exhibited by solids and liquids in their relation to changes of pressure and temperature. The gaseous state is evidently very much simpler than the other two ; which is explained by the fact that the molecules of a gas are separated beyond the range of cohesion, 238. Absolute Temperature and Absolute Zero. — Let ?'„ be the volume of a body of gas at o° C, and z^, its volume at any other temperature /| under the same pressure. The increase in volume is 7'i — rv. and this increase is — ^ of the volume at 0** (law of Charles) ; that is, — ^^^ From which Ti = ?'„( i H — ~ ). (i) \ 273/ Similarly, if r, be the volume of the gas at temperature /j, under the same pressure, then — .,=..(.+-4^). (.) Dividing the members of equation (i) by the corresponding members of equation (2), we have — gi_ 273 273 which reduces to ^ = "^ ^^44 ' (s) Vt 2734-/2 ^^^ The relation expressed by equation (3) has led to the adoption of a temperature scale whose degrees are the same as those of the Centigrade scale but whose zero is at — 273° C. This scale of temperature is called the absolute scale, and its zero the absolute zero. The freezing point is 273° Abs. and the boiling point 373° Temperature and Expansion i8i Abs. Any temperature on the Centigrade scale is changed to the absolute scale by adding 273. If we let T denote temperatures on the absolute scale, then 71 =273 + /!, and 7^2= 273 + 4, and equation (3) becomes — M- « Expressed in words the meaning of this equation is : Under constant pressure the volume of any body of gas is proportional to its absolute temperature. This is but another (and the simplest) way of stating the law of Charles. If this law held for all* tem- peratures, it is evident that at absolute zero the volume of any body of gas would be zero ; but, as before stated, the law fails to express the behavior of gases when near the point of condensation, and all licjuefy and even solidify before reaching absolute zero. When near the point of condensation, the decrease of volume for a given fall of temperature is less than that indicated by the law. By reasoning based on the relation of heat to mechanical energy, it is proved that the absolute zero is what its name indicates ; namely, the temperature at which a body would pos- sess no molecular kinetic energy, or no heat, — the molecules would be at rest. No substance has yet been cooled to absolute zero; but the temperature has been closely approached by the evaporation of hydrogen after it has been liquefied (Art. 268). By this means hydrogen has been cooled to a temperature estimated at — 259°C. or 14° Abs., at which temperature it is frozen. Air freezes at a considerably higher temperature and boils at — 191° C. or 82° Abs. PROBLEMS 1. (rt) The reading of a thermometer gives the temperaturt of the ther- mometer. On what grounds do we assume that the reading of a thermometer in a liquid gives the temperature of the liquid? (^) Why do we not take the reading immediately on inserting a thermometer in a liquid to determine its temperature? 2. The reading of a barometer is 76 cm. on a certain day when its tem- perature {i.e. the temperature of the mercury in the barometer) is 0°. What 1 82 Heat would have been the reading of the barometer if its temperature had been 20^? 3. In accurate work the reading of the barometer must be " corrected for temperature " ; 1^. the true height is taken as the heij^ht at which it would stand if the temperature of the mercury were o*'. A barometer read- ing is 75.6 cm. at a temperature of 22*^ ; find the true or corrected height. 4. The thinner a glass tumbler is, the less likely is it to break when hot water is |)Oured into it. Why? 5. Why cannot an air thermometer be used for measuring the lowest attainable temperatures? 6. What will be the volume, at 75", o( a body of air which, under the same pressure, has a volume of 250 ccm. at 20*^ ? SlUGESTlON. — Use equation (3) or (4) above. 7. A body of gas at 10*' and a pressure of one atmosphere is inclosed in a vessel and heated to 300*^. What is the pressure at that temperature, none of the gas being allowed to escape? 8. A quantity of gas is found to have a volume of 800 ccm. at 20" under atmospheric pressure when the barometer reads 75 cm. What would be the volume of the gas at 0° and a pressure of one atmosphere? Si'G(;estion. — Find the volume at the given temperature and 76 cm. pressure (Boyle's law), and from this the volume at 0° under the latter pressure (law of Charles). V. Calorimetry: Specific Heat The Heat Unit. — Heat being a form of energy, it can be measured in terms of any of the units by which mechanical energy is measured (ft.-lb., etc.) ; they are not used, however, as there are more convenient units for the purpose. Two heat tinits are in common use : one, the calorie^ is the amount of heat required to raise the temperature of one gram of water one degree Centi- grade ; the other is the amount of heat required to raise the tem- perature of 'one pound of water one degree Fahrenheit. The calorie is almost exclusively used in scientific work and is the only heat unit that is used in this book. Example. — How much heat is required to raise the temperature of 70 g. of water from 8° C. to 63"^ C? The rise of temperature is 55°; hence the heat required is 55 calories per gram, and 70 X 55, or 3850 calories, for 70 g. Calorimetry : Specific Heat 183 The amount of heat required to raise the temperature of one gram of water one degree is not exactly the same at all tempera- tures, but the difference is too small to be of importance except in the most accurate work. The numerical relation between the calorie and the units of mechanical energy is considered in Art. 270. 240. Specific Heat. — It is found by experiment that only one ninth as much heat is required to cause a given rise of temperature in any mass of iron as is necessary to cause the same rise of tem- perature in an equal mass of water. This ratio J, or .11, is called the specific heat of iron. The term is also applied to the number of calories required to raise the temperature of one gram of iron one degree y which is evidently .11 calorie. The specific heat of a substance is the ratio of the quantity of heat required to raise the temperature of any mass of the sub- stance one degree to the amount required to raise the temperature of an equal mass of water one degree ; or, it is the number of calories required to raise the temperature of one gram of the sub- stance one degree (Centigrade). ExAMi'LKS. — If the specific heat of a substance is .04, to raise the tem- perature of 50 g. of it from 2^ C. to 6" C, would require 50 x 4 X .04, or 8 calories. The same body in cooling from 50° C. to 30° C. would give out 50 X 20 X .04, or 40 calories. The specific heat of water is one, by definition ; it is very large compared with that of most other substances, especially the metals, and is exceeded only by hydrogen. In the following table the substances are named in the order of their specific heats. Table of Specific Heats Hydrogen 3.409 Water i.ooo Alcohol (0° to 50°) . . . .0.615 Ice 0.504 Steam 0.480 Afr 0.237 Marble 0.216 Aluminum 0.213 Glass 0.198 Iron 0.1 13 Copper 0.095 Brass 0.094 Mercury 0.033 Lead 0.031 184 Heat 241. Measurement of Specific Heat. — The method generally used for determining the specific heat of a substance is known as the method of mixtures. It is illustrated by the following example : A brass calorimeter weighing 100 g. contains 400 g. of water at I8^ Into this is put a roll of sheet iron at 100°, weighing 190 g. After stirring, the temperature of the water is 22°, and this is assumed to be the temperature of the roll of iron and the calo- rimeter. The specific heat of the calorimeter is given as .094. Find the specific heat of the roll of iron. Solution. — I^t j denote the specific heat of iron ; i.e. in this case, it is the number of calories of heat given out by each gram of the roll of iron in cooling one degree. Rise of temp, of calorimeter and water = 22" — 18** = 4° Heat received by the calorimeter = 100 x 4 X .094 = 37.6 cal. Heat received by the water = 400 x 4 = 1600 cal. Fall of temperature of the iron = 100° — 22° = 78° Heat given out by the iron = 190 x 78 X .f = 14820 j cal. Assuming that the transfers of heat take place only among the calorimeter and its contents, it follows that the heat given out by the roll of iron in cool- ing to the temperature of the " mixture " is equal to the heat gained by the calorimeter and water in coming to the same temperature ; that is, 14820 J = 37.6 + 1600, from which s — 1637.6 -4- 14820 = .110. 242. The Heat Equation. — The above example illustrates the method of treating the experimental data in all experiments in calorimetry. The following summary of the method will therefore be of service now and later. (i) Find numerical or algebraic expressions for the separate quantities of heat involved in the equalization of temperatures. (2) With these quantities of heat form the heat equation^ which expresses the equality of heat lost and heat gained. (3) The heat equation contains as an unknown quantity the quantity sought (specific heat, heat of fusion, or heat of vaporiza- tion). To find this quantity, solve the equation by the usual algebraic processes. Calorimetry : Specific Heat 185 243. The Control of Heat in Calorimetric Experiments. — Any transfer of heat between the contents of the calorimeter and the surrounding air or other bodies during an experiment is a source of error, and must be avoided in so far as possible. The calo- rimeter is usually nickel plated and brightly polished to dimin- ish radiation when it is warmer than the surrounding air, and to diminish absorption when it is cooler. The calorimeter should stand on a poor conductor (wood) and should be touched with the hands as little as possible, to avoid conduction. At the beginning of an experiment the water should be taken at such a temperature that it (and the calorimeter) will be colder than the air during a part of the time and warmer during a part, in order that the gain of heat by conduction and radiation at the lower temperature may be as nearly as possible equal to the loss by the same means at the higher temperature. Laboratory Exercise jy. PROBLEMS 1. The specific heat of water is much greater than thai of rocks and soils. How does this in part account for the fact that the change of temperature of the land between day and night and between winter and summer is much greater than that of the ocean ? 2. Are equal quantities of heat required to raise equal volumes of different substances through equal changes of temperature ? (Consult table of densi- ties and table of specific heats.) 3. What effect has the large specific heat of water on the sensation caused by putting the hand in hot or cold water ? In general, how does the specific heat of a substance affect the sensation of heat or cold caused by it when touched (see Art. 217) ? 4. A roll of lead weighing 800 g. is heated to 100° and placed in a brass calorimeter weighing 90 g. and containing 406.3 g. of water at 16.2°. The final temperature is 21°. Find the specific heat of the lead. 5. A kilogram of mercury at 200° and a kilogram of water at 0° are mixed. Find the resulting temperature, no allowance being made for the vessel. 6. A piece of aluminum weighing 60 g. is heated to 63°, and placed in a copper calorimeter weighing 50 g. and containing 100 g. of alcohol at 8". The temperature of the alcohol rises to 17°. Find its specific heat, taking the specific heat of copper and aluminum from the ^ble. 1 86 Heat VI. Fusion and Solidification 244. Melting of Ice and Freezing of Water. — \\lien heat is applied to ice at any temperature below o^, the temperature of the ice rises, but melting does not begin until the temperature has risen to o*. With the further application of heat the ice begins to melt, but its temperature remains at o°. When a vessel of water is surrounded by any substance whose temperature remains below zero, the water loses heat and cools U> ©•. With further loss of heat, the water begins to freeze ; but its temperature remains at o° until it is all frozen. Thus the wultimg point of ice and the freeung point of water are exactly the same. Whether melting or freezing will take place in a >*essel containing both ice and water depends upon whether heat is passing into the vessel or from iL K the water is losing heat, it will freeze ; if the ice is receiving heat, it will melt ; if there is neither gain nor loss of heat, neither melting nor freezing win occur. Lmhoraifrx Exrrcisf jj. 945. lldting Points. — Every solid that can be melted has a constant melting point, which is also the temperature at which it freezes or solidifies. .Among fusible solids, some, like ice, change abruptly from the solid to the liquid state. In such cases the melt- ing point can be very accurately determined. Other solids, as seal- ing wax and glass, gradually soften and pass by continuous change into the liquid state. In such cases the melting point, although constant, is nx>re or less indefinite. Talflt of Melting Points yrfc 4» 657 , 1050 Gla» 1000 to 1400 Iron, wrought . . 1500 to 1600 Flatinom 1775 -ijo C Moc«y -39 Ice o Batter n Beeswax 62 Caae.ssgar 170 Solder, soft 225 Fusion and Solidification 187 246. Change of Yolnme during Fusion and Solidification. — Most substances expand in melting and contract in solidifying; in many cases the change in volume is considerable. This is well illustrated in cooling a dish of melted beeswax or paraffine : the contraction leaves a depression at the center of the cake {Exp.). Metals, with few exceptions, also contract in solidifying. Those that do are not adapted for casting, as they would shrink away from the surfaces of the mold. Cast iron and type metal, which is an alloy of lead, tin, and antimony, are among the exceptions. Water expands in solidif>ing, as is well known, the increase in volume amounting to about one eleventh. As a result of ihb expansion ice floats — a fact of great importance in nature. If water contracted in freezing, ice forming at the surface of lakes and rivers would sink. Freezing would consequently continue at the surface throughout winter or until the lakes and rivers were frozen solid, and all animal life inhabiting them would be de- stroyed. The enormous force exerted by water in freezing is shown in the occasional bursting of water pipes in winter. The magnitude of this force was strikingly shown by some experiments of Major Wil- liams, in Canada. " Having quite filled a thirteen-inch bombshell with water, he firmly closed the touchhole with an iron plug weighing three pounds, and exposed it in this state to the frost. After some time the iron plug was forced out with a loud explosion, and thrown to a distance *^ of 415 feet, and a cylinder of ice 8 inches long issued from the opening. In another case the shell burst before the plug was driven out, and in this case a sheet of ice spread out all round the crack." (Fig. 123.) — Ganot*s EUnunts of Physics. " Much of the destruction of rocks which is taking place on the earth's surface is due to the same quiet but intensely powerful i88 Heat action of freezing water. Rain sinks into the cracks and pores which all rocks are liable to contain, and when it freezes there, the crack is inevitably widened or the stnicture of the rock loosened. Thus room is made for more water, which acts in the same way when it freezes ; and so by degrees immense masses of rock and earth are loosened from the mountainside, nor does the action end until the material is reduced to the finest soil." — Madan's Heat, Substances that expand in solidifying have a crystalline structure in the solid state. The crystalline structure is plainly seen in the ice that first forms when water begins to freeze, in the frost that gathers on window panes, and in snow. In crystalline solids the molecules are arranged in clusters of a definite shape, and hence occupy more space than when they lie loosely side by side in the liquid state ; just as a number of bricks would occupy more space if arranged in patterns than if packed in layers. 247. Change of Melting Point produced by Pressure. — Experi- ments have shown that increase of pressure upon a solid that ex- pands in melting tends to prevent melting by raising the melting point. The pressure evidently opposes melting because it opposes the expansion that accompanies the process. Similarly, pressure upon a liquid that expands in solidifying tends to prevent solidification by towering the melting point, for in this case, also, pressure opposes the expansion that accompanies the change of state. While lowering the melting point opposes solid- ification, it aids melting. Thus ice has been melted at — 1 8° by a pressure esti- mated at several thousand atmospheres. The change in the melting point of ice Fig. X24. (jue to a pressure of one atmosphere would escape detection by means of the thermom- Fusion and Solidification 189 eters used in elementary physics ; yet the effects produced under certain conditions by small changes of pressure are very striking. For example, a loop of fine wire to which weights are attached slowly descends through a block of ice round which it has been passed (Fig. 124) ; yet, after it has passed completely through, the ice is in one solid piece as at the beginning {Exp.). The pressure of the wire very slightly lowers the melting point of the ice immedi- ately beneath it ; and the ice melts, receiving the heat necessary for the purpose from the water filling the space just above the wire. This water freezes in losing heat, since it is relieved from pressure. The process is continuous : the water from the ice melting below the wire, passes round and freezes above it. The three stages of the process are (i) melting under pressure, (2) change of position of the water, (3) regelation (refreezing) under diminished pressure. This explains the hardening of snow into a solid mass in making snowballs, and the freezing of ice to flannel wrapped around it. The flow of glaciers is supposed to be due to the same action under great pressure. 248. Heat of Fusion. — We have seen that ice melts only while receiving heat at 0°, and water freezes only while losing heat at 0°. The quantity of ice melted or of water frozen is proportional to the gain of heat in the one case, and to the loss of heat in the other. This is true of any substance that has a definite melting point. Since these transfers of heat during change of state take place without change of temperature, it is evident that heat is lost in the process of fusion and is recovered during solidification. In what form does this energy exist in the liquid ? A solid in melting must receive energy in the form of heat to overcome (in part) the cohesion of its molecules (Art. 189). After doing this work the energy no longer exists as heat, but as potential energy in the changed molecular condition of the sub- stance, — it is molecular potential energy. The process may be illustrated by pulling apart two balls connected by a rubber band, the balls representing molecules and the tension of the rubber 190 Heat band, cohesion. Work is done in separating the balls ; the result is potential energy, which is recovered when the balls are per- mitted to come together again. The number of calories required to melt one gram of any sub- stance is called its Juat of fusion ;^ this is also the number of calories given out by one gram of the substance in solidifying. Substances differ widely in their heats of fusion. The heat of fusion of water is much larger than that of most other substances. Table of Heats of Fusion Caloribs Ice . > 79.25 Wax 42 Zinc 28.13 Silver 21.07 Calories Tin 14.25 Sulphur 9.37 Lead 5.37 Mercury 2.83 249. Determination of the Heat of Fusion of Ice. — The follow- ing example illustrates the process of finding the heat of fusion of ice by the method of mixtures : A quantity of dry, crushed ice weighing 104 g. is placed in a brass calorimeter weighing 85 g. and containing 220 g. of water at 44°. The temperature after the ice is melted is 5.3°. Solution. — Let /denote the heat of fusion of ice. Fall of temperature of calorimeter and water = 44 — 5.3 = 38.7° Heat given out by the calorimeter = 85 X 38.7 x .094 = 309.2 cal. Heat given out by the water = 220 X 38.7 = 8614. cal. Heat received by the ice in melting = 104 /cal. Heat received by the ice water in warming to 5.3°= 104 X 5-3 = 551.2 cal. 104/+ 551.2 = 309.2 + 8514 ; /= 79.5 calories. Laboratory Exercise j8. 1 According to the caloric theory, heat must always remain heal, since it was regarded as a form of matter ; and the heat that disappears in the process of fusion (and vaporization) was called "latent" (meaning hidden), implying that it still exists as heat, although its presence cannot be detected. The only form of energy that is properly called heat at all was then called " sensible " heat to distinguish it from " latent " heat. The terms have outlived the theory that gave rise to them ; thus the heat of fusion of ice is often called the " latent heat of water " (Art, 210). Fusion and Solidification 191 250. Heat of Solution ; Freezing Mixtures. — Work is done in overcoming cohesion in a solid when it is dissolved as well as when it is melted ; and in many instances there is direct experimental evidence that heat disappears in the process, proving that this work is accomplished by heat.* Thus when ammonium chloride or ammonium nitrate is dissolved in water, there is a fall of temper- ature of several degrees ; for the heat required to dissolve the solid is taken from the nearest available source; namely, the water. Solution differs from fusion in that it can take place within a wide range of temperature ; hence the temperature continues to fall (unless heat is received from the outside) until all the solid is dissolved or until the solution is saturated. A mixture of one or more solids and a liquid, or of two solids, is called 2i freezing mixture if the solution or the liquefaction of the solids causes a fall of temperature below zero. The following are examples of freezing mixtures : — (i) One part by weight of ammonium chloride and one of potassium nitrate or ammonium nitrate, powdered together and dissolved in two parts of water. Fall of temperature about 20°. (2) About 5 parts of strong hydrochloric acid and 8 parts of powdered sodium sulphate. Fall of temperature about 30°. (3) One part of table salt and 2 parts of snow or crushed ice. Fall of temperature to about — 18°. The strong attraction of salt for water causes the ice to melt rapidly. The heat required to melt the ice and to dissolve the salt is taken first from the ice and salt, then, by conduction, from surrounding bodies. This freezing mixture is well known from its use in making ice cream. (4) One part each of crystallized calcium chloride and snow or crushed ice. Fall of temperature to about — 40°. The attrac- tion of calcium chloride for water is stronger than that of table salt, and hence causes the ice to melt more rapidly and at a lower temperature. 1 When chemical action accompanies solution, it may result in a rise of temper- ature, the heat generated by the chemical action being greater than the heat lost in solution. 192 Heat PROBLEMS 1. How much heat is required to convert 750 g. of ice at — 20° into water at 50^ ? 2. How many grams of ice at 0° can be melted by 500 g. of water at 60° ? 3. A kilogram of ice and a kilogram of water, both at o"^, receive heat at the same rale. What will lie the temperature of the water when the ice has all been converted into water at 0° ? 4. A piece of aluminum weighing 250 g. and heated to 100° is placed in a dry cavity in a block of ice, and melts 63.1 g. of the ice. Find the specific heat of the aluminum, taking the heat of fusion of ice as 79.25 calories. 5. What purpose is served by vessels of water placed in a cellar where vegetables are stored or in a greenhouse on a frosty night ? 6. (o) Do freezing and thawing take place more or less rapidly than they would if the heal of fusion of ice were less ? (d) Of what importance is this in the economy of nature ? VII. Vaporization and Condensation 251. Vaporization. — The change of a substance from the solid or liquid to the gaseous state is called vaporization. Vaporization may take place at the free surface of a licjuid, or within its mass at the place where heat is applied. In the first case the phenom- enon is generally called amporation ; in the second case, boil- ing, A liquid that evaporates readily is said to be volatile. The gaseous form of a substance that exists in the liquid or the solid state at ordinary temperatures is generally called a vapor. Evaporation takes place at the surface of most liquids at all temperatures, but more rapidly as the temperature rises. It is due to molecular motion. Some of the molecules of a liquid, in their irregular motion, reach the surface with a sufficient up- ward velocity to carry them into the space above, out of the range of cohesion, where they exist as a gas or vapor. With a rise of temperature the velocity of the molecules is increased, and more of them are able to escape from the liquid in a given time. The process is illustrated on the largest scale in the evaporation of water from Ihe surface of the oceans, lakes, ponds, and streams ; Vaporization and Condensation 193 as a result of which, the air always contains a greater or less amount of water vapor. 252. Disappearance of Heat during Vaporization. — It is well known that evaporation is a cooling process. A room is appre- ciably cooled by the evaporation of water sprinkled on the floor. The skin is cooled by the evaporation of water or perspiration from it. This is especially noticeable in a draft, which causes more rapid evaporation by carrying the vapor away as fast as it is formed. The rapid evaporation of highly volatile liquids, as alco- hol and ether, causes much greater cooling. The cooling effect of evaporation is explained as follows : A liquid in vaporizing increases enormously in volume.* In this ex- pansion work is done against cohesion and also against external pressure, and heat is transformed into molecular potential energy. In evaporation, as in solution, this heat is taken from the nearest available sources — first the liquid itself, then adjacent bodies. 253. Vapor Pressure. — A vapor, like any gas, exerts a certain pressure which is proportional to its density and increases with its temperature ; but the behavior of vapors differs from that of other gases in important re- spects, as shown by the following experiment. A barometer tube is filled with mercury and set up as a simple barometer. Ether is introduced into the tube at the bottom, drop by drop, by means of a dropping tube or a pipette, care being taken to let no air enter (Fig. 125). As the first drop rises to the top of the mercury column, it instantly evaporates, and the pressure that it exerts as a vapor causes a depression of the column. The pressure of the vapor, expressed in centi- meters of mercury, is measured by the amount of the - depression. (Why?) Each drop of ether evaporates as HhMHI it rises in the tube and causes a further depression of the ' ^^^^ ' column. This continues, however, only to a certain fig. 125. 1 A cubic centimeter of v/ater forms 1661 ccm. of steam at 100° and a pressure of one atmosphere. 1 94 Heat point, beyond which the liquid ether accumulates above the mer- cury, and the column remains stationary. The ether vapor is now saturatfd ; i.e. // cannot be made denser at its present temperature. Before this condition is reached the vapor is unsaturated^ and hence exerts a less pressure. The pressure exerted by the saturated ether vapor is found by subtracting the height of the mercury in the tube from the read- ing of a barometer. When the tube is inclined, the space occu- pied by the vapor becomes smaller; but the vertical height of the mercury column remains the same as before, indicating that the vapor pressure is unchanged. This is true even when the tube is inclined so far that the space occupied by the vapor almost disappears. In inclining the tube, the vapor is evidently not compressed and made denser ; for in that case it would exert an increased pressure. The fact is that a portion of the vapor is liquefied, and the density of the remainder is unchanged. This behavior agrees with the former statement that the vapor is satu- rated, and cannot be made denser at its present temperature ; and, since it cannot be made denser, it cannot be made to exert a greater pressure. The pressure of the saturated vapor is therefore the maximum pressure of ether vapor at its present temperature. When the tube is returned to the vertical position and the ether warmed by clasping the tube in the hands, the mercury descends further, showing an increase of vapor pressure with rise of tempera- ture. This is partly due to the heating of the vapor already in the tube, but chiefly to the evaporation of more ether. The saturated vapor is denser at the higher temperature. If there were no more ether in the tube to evaporate, the heat of the hand would cause expansion of the existing vapor, and it would become less dense and unsaturated. Similar results are obtained throughout when alcohol is substi- tuted for ether in the experiment ; but they are all on a greatly reduced scale, for the maximum pressure of alcohol vapor is much less than that of ether at the same temperatures. With water the effects are very slight. At 20° the maximum vapor pressure of Vaporization and Condensation 195 ether is 43.28 cm. (of mercury), that of alcohol 4.45 cm., and that of water 1.74 cm. Laboratory Exercise 34, Parts I arid II. 254. Laws of Vapor Pressure. — The above experiment illus- trates the first three of the following laws of vapor pressure : — I. At a given temperature there is a maximum density and pressure for every vapor, in which condition the vapor is said to be saturated. Compression of a saturated vapor without change of tempera- ture causes a portion of it to condense (liquefy) ; but the density and pressure of the remainder are not changed. II. At the same temperature the maximum pressures of different vapors are unequal. III. The density and pressure of a saturated vapor increase with the temperature. IV. The behavior of unsaturated vapors is approximately like that of gases, as expressed in the laws of Boyle and Charles. 255. Mixture of Gases and Vapors; Dalton's Laws. — The following laws relating to mixtures of gases and vapors are known as Dalton's laws, from their discoverer. I. The quantity of vapor which saturates a given space is the same, at the same temperature^ whether this space contains a gas or is a vacmnn. II. The pressure of the mixture of a gas and a vapor is equal to the sum of the pressures which each would exert if it occupied the same space alone. In a vacuum the evaporation of a volatile liquid is almost instan- taneous. In the presence of air or any other gas, evaporation takes place much more slowly ; but, as is implied in Dalton's first law, it will not cease until any inclosed space above the liquid contains as much of the vapor as it would if the gas were not present. The kinetic theory of gases accounts at once for the second law. The law holds for the mixture of any number of vapors and gases, the most familiar example of which is the atmosphere. 1 96 Heat 256. Water Vapor in the Atmosphere. — The atmosi)here is a mixture of several gases, principally nitrogen and oxygen ; the only other constituents of importance are carbon dioxide and water vapor. All of the constituents of the atmosphere except water vapor are practically constant in amount ; the latter varies from an inappreciable fraction to about 2 per cent of the whole, the average amount being not far from i per cent. The condition of the water vapor in the air with respect to saturation is not in the least affected by the presence of the other gases (Dalton's first law), and depends only upon its own density and temperature (which, of course, is the temperature of the air) ; yet common forms of expression seem to imply that the presence and condition of the vapor are due to some action of the air. Thus when the water vapor in the air is saturated, we say that the air is saturated or that the air has all the moisture it can hold ; although, strictly speaking, it is the space that has all the water vapor that it can hold (at the given temperature) . There is per- haps no objection to the use of such expressions when their true meaning is understood. The air is generally not saturated ; it is evidently not saturated whenever further evaporation can take place. Nonsaturated air may become saturated (i) by further evaporation, (2) by a fall of temperature, (3) by the two processes combined. Saturation results from a sufficient fall of temperature because the density of a saturated vapor is less at lower temperatures (Art. 254, third law). Consequently when the quantity of water vapor in the air is less than that required for saturation at the existing temperature, it is equai to the amount required for saturation at a definite lower temperature (called the dew-point). 257. The Dew-point. — The temperature at which the water vapor present in the air at any time would be saturated is called the de7u-point of the air at that time. When any body of air is cooled to the dew-point, condensation of water vapor begins, and continues as long as the temperature continues to fall. The moisture that gathers on the outside of a Vaporization and Condensation ' 197 pitcher of ice water is a familiar illustration. The moisture comes from the surrounding air, which is cooled by coming in contact with the cold pitcher, and begins to deposit moisture as soon as the dew-point is reached. A fall of temperature several degrees below this point generally occurs, causing a considerable deposit which runs down the sides. (What error is implied in calling this phenomenon "sweating" ?) The dew-point may be determined experimentally by putting water in a vessel on whose surface a thin film of moisture can easily be seen (as a nickle-plated calorimeter), and slowly cool- ing the water by means of ice or a freezing mixture till the first trace of moisture appears on the vessel. The temperature of the water when this occurs is the dew-point. The dew-point varies between wide limits. In winter it is often many degrees below zero. It is, of course, lower than the temperature of the air unless the air is saturated at the time ; and it approaches the temperature of the air as the air approaches saturation. Laboratory Exercise 34^ Part III. 258. Humidity. — The humidity (or relative humidity) of the air at any time is the ratio of the amount of water vapor that it contains at the time to the whole amount that would be required to saturate it at the existing temperature. This ratio is usually expressed as a per cent. Thus the humidity of the air is 75 per cent when it contains three fourths as much water vapor as would be recfuired to saturate it at the time. The humidity of saturated air is 100 per cent by definition. The dryness or dampness of the air depends not only upon the amount of water vapor in it, but also upon the temperature ; in other words, it is determined by the humidity of the air. This is illustrated by the well-known fact that very damp, cold air in a room becomes dry when the room is warmed, although there is no less vapor in the room after the heating than there was before. The air is drier because its temperature is farther above the dew- point; i.e. its humidity has been diminished. For example: At 198 * Heat 10° C. (50° F.) the maximum pressure of water vapor is .92 cm. ; at 20** C. (68° F.) it is 1.73 cm. Hence when saturated air at 10° is heated to 20°, without change in the quantity of vapor it con- tains, its humidity falls from 100 per cent to about 53 per cent. At 10° the air would be disagreeably moist ; at 20° it would feel rather dry. 259. Laws of Evaporation. — The conditions affecting the rate of evaporation of a liquid may be summarized as follows : — I. TA^ rate of evaporation increases with a rise of temperature, II. The rate of evaporation increases with an increase of the free surface of the liquid. III. The rate of evaporation of a liquid decreases as t/te space around it approaches saturation by its own vapor ^ and ceases when that space is saturated, IV. The rate of ei^aporation in the open air increases with a more rapid change of air about the liquid. Currents of air (winds) carry the vapor away from the space about the liquid, and the stronger the currents are, the farther will this space be from satu- ration. V. The rate of evaporation increases as the density of the air or other gas surrounding the liquid is diminished; in a vacuum it is almost instantaneous. Changes of barometric pressure are not sufficient to materially affect the rate of evaporation in the open air. It follows from laws I, III, and IV that the most favorable con- ditions for the rapid evaporation of water in the open air are pres- ent on a dry, hot, windy day. 260. Condensation of Water Vapor in the Atmosphere. — Water vapor is ahuays invisible. The visible forms of moisture in the atmosphere — as fog, mist, clouds, and the so-called " steam " near the spout of a kettle in which water is boiling — consist of minute particles of liquid water, and are the result of the conden- sation that accompanies a fall of temperature after the dew-point is reached. Dew, frost, rain, sleet, hail, and snow are forms in which the moisture of the air is condensed and precipitated. The conditions under which the different forms occur are as follows : — Vaporization and Condensation 199 Dew is condensed water vapor coming from the air immediately surrounding the body on which it appears. It has been found by numerous experiments that surfaces upon which dew is form- ing are always at least 3° or 4° colder than the air or dewless surfaces. (Cooling below the temperature of the air is due to the rapid loss of heat by radiation.) When the air is nearly saturated, it is cooled to the dew-point by coming in contact with such surfaces, and moisture is condensed upon them. Dew forms only at night, and most abundantly during the latter part of it; when, by cooling, the air has become nearly saturated. It is formed only on calm, clear nights ; for on clear nights cooling is most rapid (Art. 228), and it is only on calm nights that any por- tion of the air remains long enough in contact with the cold sur- faces to be cooled to the dew-point. Dew forms most abundantly on the coldest objects, which are in general the best radiators and the poorest conductors. Grass, leaves, and boards are good examples. A board lying on the ground will become wet with dew when a stone pavement remains dry ; for the stone is a good conductor and receives heat from the ground, which replaces that lost by radiation, hence its upper surface is warmer than that of the board. When the dew-point is at or below zero, condensation takes place in the form oi frosty under conditions otherwise the same as are necessary for the formation of dew. The water vapor then crystallizes in the solid state as it condenses, without passing through the intermediate state of a liquid. (Is frost '•* frozen dew"?) At temperatures above zero the moisture of clouds is in the form of fog or mist. As the individual particles grow by further condensation and by uniting with one another, they may become too large to be sustained in the air, and will then fall as rain. A drop continues to grow by uniting with smaller particles that it meets with in falling through the cloud. Sleet is formed by the freezing of the raindrops as they fall through a layer of air whose temperature is below zero. 200 Heat Snow is formed by the condensation of vapor in the atmospheie at temperatures below zero. Snow and frost are formed under the same conditions of temperature and humidity, and both have a beautiful crystalline structure. " I/aii is formed in violent storms, such as tornadoes and thun- der storms, where there are strong, whirling currents of air. Hailstones are balls of ice, built up by condensing vapor as they are whirled up and down in the violent currents, freezing, melting and freezing again as they pass from warm to cold currents. For this reason they are often made of several layers, or shells, of ice." — Tarr's Nov Physical Geography, PROBLEMS 1. For what two reasons oint of a liquid is considerably lower upon a mountain than it is near sea level. On the summit of Mont Blanc, for example, water boils at 84°. 263. Boiling Points. — A liquid is said to boil when bubbles of vapor formed by vaporization within its mass are given off" at its surface. ^Vhen no pressure is mentioned, the boiling point of a liquid is understood to mean the temperature at which it boils under a pressure of one atmosphere. The boiling point of a liquid may also be defined as the temperature at which^the pressure of its saturated vapor is equal to one atmosphere. Tabli of Boiling Points Ether 35° Chloroform 61.2 Alcohol 78.4 Water icx) Turpentine 160° Glycerine 290 Mercury 357 Sulphur 448 Vaporization and Condensation 203 The following table gives the pressure of saturated water vapor (and hence also the pressure under which water boils) at a number of temperatures, the pressure being expressed in centi- meters of mercury in the first column of pressures and in atmos- pheres in the last. Temperature Pressure Temperature Pressure 0° 100 .46 cm. 9.20 cm. 76.00 cm. 120° 140 160 1.96 atmospheres 3.58 atmospheres 6.12 atmospheres Laboratory Exercise j6. 264. Distillation. — A liquid can be separated from impurities, or from nonvolatile substances held in solution, by boiling it in a closed vessel and condensing the vapor as it passes off through a Fig. 127. tube connected with the vessel. The process is called distillationy and the apparatus a still. The process may be illustrated by dis- tilling a solution of copper sulphate in water, using apparatus similar to that shown in Fig. 127. The vapor is condensed by 204 Heat inclosing a portion of the tube through which it passes within a larger tube in which it is surrounded by a continuous supply of cold water. Two or more liquids whose boiling points differ by several de- grees can be separated from one another by distillation. When such a mixture is slowly boiled, the vapor that passes off contains a much higher percentage of the more volatile constituent than the liquid mixture does. Some of the less volatile liquid also passes off, and complete separation can be effecteil only by repeated distillation. This process, which is generally known as fractional distiliation^ is employed on a large scale in separating the constitu- ents of crude petroleum and of coal tar, and in the manufacture of distilled liquors. 265. Cooling by Expansion. — Work is done upon a gas in com- pressing it, and by a gas in expanding against pressure. In tlie first case, mechanical energy is transformed into heat and the gas is warmed (Art. 212) ; in the second case, some of the heat of the gas is transformed into mechanical energy (kinetic or potential) and the gas is cooled, unless it receives an equal supply of heat during the expansion. The cooling of a gas by expansion is often beautifully illustrated when the air is exhausted from the receiver of an air pump. As part of the air is removed, the expansion of the remainder causes a fall of temperature to the dew-point, and some of the water vapor is condensed, forming a fog within the receiver. The fall of tem- perature may be measured by a thermometer placed in the re- ceiver {Exp.^. A further illustration is afforded by directing a jet of air from a tank of compressed air against the bulb of a ther- mometer held a few inches from the opening (Exp.). 266. Heat of Vaporization. — The Aea/ of vaporization of a liquid is the number of calories required to vaporize one gram of it at its boiling point. The heat of vaporization of water is 536 calories, and is greater than that of any other substance. Its value for alcohol is 209 calories, for ether 90 calories, for mercury 62 calories. Vaporization and Condensation 205 Heat is lost during vaporization by transformation in part into ( I ) mechanical potential energy in causing expansion against atmos- pheric pressure (external work), and in part into (2) molecular potential energy in overcoming cohesion during expansion (in- ternal work). When the heat thus transformed is supplied by the liquid itself and by adjacent objects, as is often the case in evaporation, a fall of temperature results (Art. 252); in boiling, the temperature remains constant, the amount of heat received from the fire or flame being equal to the amount transformed (Art. 262, second law). The heat lost during vaporization is all transformed into heat again when condensation takes place. 267. Determination of the Heat of Vaporization of Water. — The determination of the heat of vaporization of water by the method of mixtures is illustrated by the following example : A brass calorimeter weighing 65 g. contains 200 g. of water at 5°. Steam at 100° is passed into the water till the temperature rises to 40°. It is found on again weighing the calorimeter and con- tents that the weight of the steam condensed in it is 12.1 g. Solution. — Let v denote the heat of vaporization of water, — in this case the number of calories given out by i g. of steam in condensing to water at lOO"*. Rise of temp, of calorimeter and water = 40—5 = 35° Heat received by the calorimeter = 65 X 35 X .094 =214 cal. Heat received by the water = 200 X 35 = ycxx) cal. Heat given out by the steam in condensing to water at 100° = 12.1 z/cal. Heat given out by the water from the condensed steam in cool- ing to 40° = 1 2.1 X 60 = 726 cal. 12.1 V -H 726 = 70CX) + 214; z/ = 536.2 cal. I Laboratory Exercise jg. 268. The Condensation of Gases. — All substances that exist only as gases at ordinary temperatures exist also as liquids and even as solids at sufficiently low temperatures. Gases may be condensed (i) by cooling, (2) by pressure, or (3) by the two pro- 2o6 Heat cesses combined. Sulphur dioxide (the gas formed by burning sulphur) is easily liquefied under atmospheric pressure by a freez- ing mixture of ice and salt, its boiling point being — 10.5°. It can also be liquefied at 15° by a pressure of 3 atmospheres. Carbon dioxide can be liquefied at 15® by a pressure of about 52 atmos- pheres, or by cooling to — 80° under a pressure of one atmosphere. Oxygen, nitrogen, air, and hydrogen can be liquefied only at very low temperatures, however great the pressure. The neces- sary reduction of temperature in such cases is effected by the sudden expansion of a ix)rtion of the compressed gas, as in the manufacture of liquid air, or by the evaporation of a gas that is more easily liquefied. Thus in the liquefaction of hydrogen the cooling is effected by the evaporation of liquid air (Art. 238, end). Following is a table of boiling points of certain gases under a pressure of one atmosphere : — Boiling Points of Liquefied Gases C. Abs. Hydrogen -243'' 30° Nitrogen — 194 79 Air — 191 82 Oxygen — 184 89 Carbon dioxide — 78.2 194.8 Ammonia — 38.5 234.5 Sulphur dioxide — 10.5 262.5 269. Cooling by Evaporation : Applications. — The tempera- ture of our bodies is largely regulated by the evaporation of the perspiration. The process is continuous, although we are con- scious of it only when the perspiration is formed more rapidly than it can evaporate, and hence accumulates on the skin. An average of about a quart of water is evaporated from the skin daily ; and the heat that this requires is taken principally from the body. The importance of more abundant perspiration when the body is subjected to high temperatures and during active Vaporization and Condensation 207 exercise is evident. It is not the perspiration, however, but its evaporation that takes heat from the body and thus prevents a dangerous rise of temperature. Hence hot weather is especially oppressive and dangerous when the humidity of the air is high. In the very dry atmosphere of deserts there is comparatively little danger of sunstroke even at a temperature of 100° F., for evaporation is very rapid. The use of ammonia (not ammonia water) and carbon dioxide in the manufacture of artificial ice depends upon the absorption of heat by these substances in vaporizing at low temperatures. Ammonia is used on the largest scale. It is liquefied under pres- sure in long pipes exposed to the open air, where the heat gener- ated by the condensation is permitted to escape. It is thence pumped into coils of pipes immersed in a large tank of strong brine, where it vaporizes under a low pressure, cooling the brine in the tank several degrees below zero and freezing cans of fresh water placed in the brine. The vaporized ammonia is pumped from the coils in the tank into the condensing pipes, where it is again liquefied. PROBLEMS 1. What is the pressure in grams per square centimeter exerted by and upon a bubble of steam forming at a depth of 15 cm., when the barometer reads 76 cm. ? 2. (a) Is rain water distilled water ? (3) Is it perfectly pure ? 3. Mention the important consequences of the great specific heat, heat of fusion, and heat of vaporization of water, including the connection that any of these properties may have with the effect of the ocean on climate. 4. A room 4 m. by 5 m. and 3 m. high is warmed by a steam heater. Assuming no loss, what weight of steam must be condensed in the heater to warm the room from 10° C. to 18° C. ? (Density of the air 1.25 g. per cdm.; specific heat of air = .237.) 5. Water kept in porous earthenware jars in warm weather remains several degrees below the temperature of the air. Explain. 6. What quantity of heat is required to convert 850 g. of ice at — 20° into steam at ICX)° ? 7. How much heat is given out by 500 g. of steam at 100" in condensing and cooling to water at 30° ? 2o8 Heat Fig. 12 VIII. Mutual Translormations of Heat and Other Forms of Energy 270. The Mechanical Equivalent of Heat. — The numerical re- lation between heat ;>n" and back to /^'). The amplitude of vibration is the extent of motion on either side of the position of rest. The rate of vibration is independent of the amplitude ; the vibration is there- fore regular or periodic. This can be shown by counting the number of vibrations with different amplitudes when the motion is sufficiently slow; but it is proved for all sounding bodies by the fact that the pitch does not change as the sound becomes fainter {Exp. with tuning fork). The rate of vibration is meas- ured by the number of vibrations per second. Laboratory Exercise 40. 279. The Vibration of a Tuning Fork. — A tuning fork is so frequently used in sound experiments that it is important to know definitely what its motion is when vibrating. A quick blow upon one prong in the direction of the other sets both prongs in vibration. Their motion is always toward each other and from each other in succession (Fig. 132). This transverse vibration of the prongs is accompanied by a vibration of the stem in the direction of its length {/ongitudina/ wihrsition) , which can be dis- tinctly felt by placing the stem of a sounding fork against Flo. 132. the teeth. 2i6 Sound 280. The Transmission of Sound. — Solid Media. — When the stem of a sounding fork is pressed against the top of a table, the sound becomes much louder {Exp.). The stem in vibrating strikes a rapid succession of blows upon the table, and the impulses thus imparted cause the table to vibrate in unison with the fork — the table becomes a sounding body. With the stem of a sounding fork against one end of a wooden rod (meter stick), the sound instantly becomes loud when the other end of the rod is touched to a table {Exp.). The rod transmits the vibrations to the table, or, as we commonly say, the sound travels through the rod. Any substance through which sound travels is called a medium for the transmission of sound, or a sound medium (plural media). The above experiment succeeds equally well with rods of different material; in fact, any highly elastic (rigid) solid is a good sound medium. The sound of a distant train is plainly heard through the rails, and the tread of a galloping horse can be heard for miles through the earth by putting the ear close to the ground. On the other hand, soft and yielding solids " deaden " sound, for they transmit it poorly. Thus little or no sound will be heard when a rubber stopper or a roll of cotton wool is placed between the sounding fork and the table {Exp.). Liquid Media. — Sound can be transmitted from a fork to a table through a jar of water or other liquid ; but, in order that the liquid may take up the vibrations with suf- ficient intensity, the area of the vibrat- ing surface in contact with it must be rather large. The stem of the fork is therefore firmly inserted in a hole in a small block of wood, and the block touched to the liquid {Exp.). Sounds made under the surface of a large body of water are transmitted through it over long dis- tances. Fig. 133. Gaseous Media. — The air is the usual Origin and Transmission of Sound 2 1 7 medium by which sound vibrations are transmitted to the ear. That sound is not merely transmitted through the air but by it is shown by the following experiment : A loud-sounding body, as an electric bell (Fig. 133) or a metronome, is placed on a soft cushion or suspended from wires under the receiver of an air pump, and the air exhausted. The sound grows continually fainter as the exhaustion proceeds, and becomes inaudible if a good vacuum is secured. The sound is restored when air or any other gas is admitted into the receiver (Exp.) Sound, unlike radiant energy, is not transmitted through a vac- uum ; it is transmitted only by elastic substances — solid^ liquid, and gaseous. 281. Wave Motion. — A sounding body is the center of a peri- odic disturbance consisting of impulses exerted in rapid succession upon any body in contact with it, including the surrounding air ; and these bodies serve as media for the transmission of the dis- turbance. Since this disturbance is invisible, it will be helpful in the study of its nature and the manner of its transmission to con- sider briefly a few cases of visible motion that are in some respects like it. When a stretched rubber tube or a spiral spring, three or four meters long, is struck a sharp blow near one end, a distortion is produced which travels rapidly as a wave to the other end. By tying strips of cloth to the tube at different points, it can be seen that, as the wave passes any point, that point moves quickly out in a direction at right angles to the length of the tube and returns {Exp.). The curved form that we call the wave is, in fact, passed from point to point along the tube by the transverse vibra- tion of successive portions of the tube. A distortion of a different character is started by stretching a portion of the tube near one end either considerably more or less than the remainder and sud- denly releasing that portion. The strips of cloth will now indicate a to-and-fro or longitudinal vibration as the disturbance passes {F.xfi.). The waves that pass over a field of grain when a strong wind is 21 8 Sound blowing are due to the forward bending and springing back of successive stalks of grain, a row of stalks at right angles to the direction of the wind moving in unison. The vibration of each head of grain is mainly longitudinal with respect to the direction in which the waves travel. The motion of the water in transmitting a water wave is mainly a transverse vibration ; as is indicated by the rise and fall of any floating object as the waves pass under it. (A chip in a tub of water serves well for experiment.) A wave is not formed of the same water as it travels ; it is the disturbance that travels, not the water. When a pebble is dropped into a pool of still water, a train of circular waves travels outward from the point where the pebble strikes the surface. The waves are circular because the disturb- ance is transmitted with equal velocity in all directions over the surface ; they are concentric because they all originate at the same point. Each wave consists of a crest and a trough. The length of a wave is the distance from crest to adjacent crest or from trough to trough, measured radially^ i.e. toward or from their common center. The waves rapidly decrease in height as they travel outward because their energy is transferred (radially out- ward) to an ever increasing body of water. 282. Sound Waves. — Suppose a sounding fork to be held at an end of a tube of indefinite length. As the nearer prong moves taivard the tube, it pushes against the air immediately in front of it. As this body of air is driven forward by the advancing prong, it is slightly compressed, and hence expands on the farther side, Fig. 134. causing compression of the air in advance of it (Fig. 134). By the repetition of this process between successive portions of the air, the compression is rapidly transmitted along the tube. As Origin and Transmission of Sound 219 the compression passes any section of the tube, the air particles in that space move forward in a body. Each particle starts for- ward when the front of the condensation strikes it, and stops as soon as the condensation has passed. As the prong of the fork moves from the tube during the second half of a vibration, the body of air on the side toward the tube follows the fork up in its retreat, and expands in doing ? w Fig. 135. so (Fig. 135). This causes air from a greater distance to move toward the fork in restoring the density and pressure in that re- gion. Thus a rarefaction is transmitted along the tube by the backward motion of the air particles. The rarefaction follows the preceding compression (or condensationy as it is generally called), and is itself followed by the next condensation (Fig. 136). Fig. 136. A conden g^M'nq and flr^j'^Cfi"^ mrpfhrfinn together ^Constitute. a s ound _i pave. _A sound wave is transmitted, or propagated, by a vibration of the air particles — forward in the condensation and backward in the rarefiiction, as indicated by the arrows in the figures. This vibration is in a straight line parallel to the direc- tion of propagation of the wave, i.e. it is io?igifiidinal ; its ampli- tude is very small — generally much less than that of the sounding body. A sound wave is represented graphically by a curved line as in the lower part of Fig. 136. The curve above the straight line 220 Sound represents the condensation, the curve below the line the rare- faction. This representation must not be regarded as a picture : a sound wave does not consist of a crest and a trough as a water wave does. 283. Sound Waves in the Open Air. — When a sounding body is surrounded by an open body of air, the waves travel outward from it in all directions. Usually a condensation starts out on one side simultaneously with a rarefaction on another. In the simpler case where the disturbance is the same at the same instant all round the body (as when a firecracker is exploded in the aiO, the waves travel outwar'l n< .-.,„.-.• „/;7V spherical shells^ FIG. 137. represented in section by Fig. 137. The waves are spherical because they are transmitted radially with equal velocity in all directions. A wave front is the surface bounding the front of a conden- sation. Under the conditions just considered it is a spherical surface. A wave length is the distance, measured radially, be- tween adjacent wave fronts or between any corresponding parts of adjacent waves. A sound is (i) a set or train of sound waves, or (2) the sensa- tion produced by such a set of waves through the organs of hear- ing. In physics the word is generally used in the first sense. 284. Energy of Sound Waves; Intensity of Sound. — A part of the energy of a sounding body is transformed into heat by molecular friction within the body itself; but most of it is trans- ferred to the air or other medium in which sound waves are pro- Origin and Transmission of Sound 221 duced. The more rapidly the energy is thus transferred, the greater will be the intensity (or loudness) of the sound and the more quickly will the sound cease. The rate of transference of energy from the sounding body to the medium depends upon (i) the amplitude of vibration of the body, (2) the area of the vibrating surface, and (3) the density and elasticity of the medium. 285. Effect of Amplitude. — The gradual dying away of the sound of a bell, a piano wire, a tuning fork, etc., is due to the diminishing amplitude of vibration as the body approaches a state of rest. With a decrease of amplitude the blows of the vibrating surface against the surrounding air grow less vigorous and the sound waves are correspondingly weaker. 286. Effect of the Area of the Vibrating Surface. — A narrow vibrating surface cuts through the air, producing little effect ; the air slips round it. A broad surface catches the air and carries it bodily forward. This explains why the sound of a tuning fork is very faint when it is held in the hand and loud when it is touched to a table. In the latter case the vibrations are transmitted to the air almost entirely by the vibrating table. The music of a violin or guitar comes practically entirely from the body of the instrument, and the music of a piano from the sounding board on which the wires are strung. 287. Effect of the Density and Elasticity of the Medium. — In the experiment with the sounding body under the receiver of an air pump, it was observed that the sound grows fainter as the exhaustion continues, /. e. as the density of the remaining air is diminished. The reason is obvious : there is less matter in motion in the wave of rarefied air, hence there is less energy — kinetic energy being proportional to the mass of the moving body. A number of experiments have already shown that sound is louder when transmitted through elastic solids than when trans- mitted through the air. A sounding fork held first in the hand then against a table is an excellent illustration. The rigid wood offers much greater resistance to the blows of the fork than the 222 Sound air does, and hence receives a correspondingly greater amount of energy with each vibration.* Observe also that the fork conies to rest much more quickly when held against the table (Exp.), 288. Effect of Distance on the Intensity of Sound. — It is well known that a sound grows fainter with increase of distance from the sounding body. Thfe principle of the conservation of energy affords an explanation and a definite statement of the law of decrease. As a sound wave travels in the open air, its distance from the source is the radius of its surface (the spherical wave front). Now it is proved in geometry that the surfaces of two spheres (or equal fractions of their respective surfaces) are pro- portional to the squares of their radii. Hence, since the length of a wave remains constant, its volume and the amount of matter in it are proportional to the square of the distance it has trav- eled in the open air. This f''°- '3^- is illustrated in Fig. 138, which represents a section of a spherical wave at a distance d^ from the source and again at twice that distance, or //g. If Z'l de- notes the volume of the section at the first distance, v>i its volume at the second distance, then z^g : z'l : • 4 • i, or z/j : Z'l : : //g* : di. Since the energy of a sound wave is transmitted through the medium with the wave, the intensity of the sound (or the amount of energy per unit volume) is inversely proportional to the volume of the wave. Hence, from the above proportion, the intensity is inversely proportional to the square of the distance from the source y when the sound is traveling in the open air. 1 That more work can be done upon the body that offers the greater resistance is plainly evident to one who strikes out at something with his fist and only suc- ceeds in " hitting the air." Origin and Transmission of Sound 223 289. Dissipation of the Energy of Sound. — We have assumed that the total energy of a sound wave remains constant as it travels. This is not strictly true, for the energy is more or less slowly trans- formed into heat by friction in any medium. In the end it is all dissipated in this manner. Hence the intensity of sound decreases somewhat more rapidly than the law stated above indicates. 290. Confined Sound Waves. — Sound travels long distances in elastic media with very little loss of intensity if the waves are pre- vented from increasing in size. This is the principle of the speak- ing tube, which is a long metal tube of small diameter, used for communication between different rooms of a building or between some room and the street door. The tube does not readily take up the vibrations of the air, hence they are almost completely con- fined within it. The intensity of the sound is slowly diminished by friction. The transmission of sound over long distances through the rails of a track and through stretched wires and strings is due to the same cause : the vibrations are largely confined to the solid medium. This fact is utilized in the acoustic or siring telephone. PROBLEMS 1. Are sound waves transmitted by the elasticity of form or of volume of the medium ? 2. (fl) By what force are the waves transmitted along a stretched rubber tube or spring ? (J)) By what force are waves transmitted over the surface of water ? 3. How does the energy of sound differ from heat ? 4. Is the wave front of a water wave a line or a surface ? 5. {a) What angle does the direction of propagation of a water wave make with the wave front ? (Jj) The direction of propagation of a soupd wave ? 6. {a) Would a sounding body continue to vibrate longer in water or in the air ? (^) In the air or in a vacuum ? Why ? 7. How does the intensity of sound at a distance of 5 m. from the source compare with its intensity at 10 m. ? at 15m.? at 20 m. ? 8. At what distance is the intensity of sound one fourth as great as at 100 ro. ?. one half as great ? 224 Sound 291. The Velocity of Sound in Air. — It is a familiar fact that a distant phenomenon that is accompanied by a sound is seen before it is heard. At a distance of a few hundred feet, the blow of an ax is heard after the ax is raised for the next stroke ; a flash of Hghtning is often seen many seconds before the thunder is heard, although they are produced simultaneously ; the whistle of a dis- tant locomotive may not reach the ear until the cloud of " steam " has disappeared. Now the time required for light to travel terres- trial distances is wholly inappreciable (the velocity of light being 1 86,000 mi. per sec.) ; hence the time that elapses between the sensations of sight and hearing in such a case is the time occupied by the sound in traveling from the sounding body to the observer, and, from the measured time and distance, the velocity of sound can be computed. Observations have been repeatedly taken for this purpose by firing a cannon at each of two stations several miles apart, and noting the time between the flash and the report as observed at the other station. By taking observations at each of the stations alternately, the effect of the wind is eliminated. The average of the best determinations is 332 m. or 1090 ft per sec. at 0°, At 20° the velocity is 344 m. or 11 29 ft. per sec. That the velocity of sound is independent of its pitch and intensity is proved by the fact that all the sounds produced simultaneously by an orchestra are heard simultaneously at all distances. Laboratory Exercise 41. 292. Effect of the Elasticity and Density of the Medium on the Velocity of Sound. — Experiment shows that a wave travels more rapidly along a stretched rubber tube when the tension is increased, — a result to be expected, since the propagation of the wave is due to the elastic force (tension) of the cord {Exp.). The elasticity and velocity are not, however, proportional. A wave travels more slowly along a stretched rubber tube that is filled with shot or sand than it does along an empty tube of the same size and under the same tension — a given force moves a greater mass more slowly {Exp.). Origin and Transmission of Sound 225 It can be shown by mathematical reasoning based on the second law of motion that the velocity of a sound wave is proportional to the square root of the elasticity of the medium and inversely proportional to the square root of its density. The velocity of sound in water has been found by experiment to be 1435 "^* P^^ sec. at 8.1°, — a velocity more than four times as great as in air. Thus, in comparison with air, the retarding effect of the greater density of water is more than offset by the accelerating effect of its still greater relative elasticity. The same is true in a still greater degree of soHds, the velocity in glass and steel being about fifteen times as great as in air. The velocity of sound increases with the temperature because, with a rise of temperature, the air expands and its density dimin- ishes, while its elasticity remains unchanged. An increase of pressure increases the elasticity and density proportionally, hence a change of pressure does not affect the velocity. 293. Reflection of Sound : Echoes. — When sound waves strike a large surface, as a cliff or the side of a building, they are reflected. The reflected sound is called an echo when it reaches the ear long enough after the original sound to be distinguished from it. This requires an interval not less than \ sec, during which time sound travels about 68 m. ; hence a distinct echo will not be heard unless the reflecting surface is at a distance not less than about 34 m. from the source of sound. At less distances the direct and the reflected sounds blend together. They are sensibly coincident when the reflecting surface is not more than a few meters from the source of the sound, and the result is an increased loudness. It is for this reason that reflecting surfaces are often erected behind band stands. When the distance is nearly suffi- cient for an echo, the direct and the reflected sounds are mixed confiisedly, causing indistinctness. This is often noticeable in large halls. The change in the shape and the direction of propagation of sound waves caused by reflection from a plane surface is shown in Fig. 139, which represents a section of a train of waves origi- 226 Sound nating at (9 and reflected by a plane surface, AB, The circular arcs represent the wave fronts, and the lines OA, OB, and /)N^ y^ / . ^^ directions of propagation before reflection and AD, BR^ and CF directions after reflec- tion. The waves after reflection have the same shape and direc- tion of propagation as they would have if they originated at 0\ a point on the perpen- dicular from the source of sound to the reflecting surface and at an equal distance behind it. '*'■ *^ After reflection from a con- cave surface, sound waves increase less rapidly in size, and are consequently propagated with comparatively little loss of intensity, almost as if they were confined in an inclosed space. Hence the large reflecting walls at the rear of band stands are concave. When a sounding body is at the proper distance from a concave surface, the reflected waves decrease in size and increase in inten- sity as they travel toward a point. Light is similarly reflected from concave mirrors, such as are used behind wall lamps and the head lights of locomotives and street cars. This efl'ect of concave surfaces will be more fully discussed under the subject of light. Laboratory Exercise 42, PROBLEMS 1. {a) Give two reasons why sound travels farther through the rails of a track than it does through the air. {b) Why does it travel faster through the rails? 2. How would music be affected if sounds of different pitch or intensity traveled with different velocities ? 3. A rifle is fired on one side of a canyon and 3.2 sec. later the echo is heard from the opposite side. The temperature is 20°. What is the width of the canyoQ ? Properties of Musical Sounds 227 4. A flash of lightning is seen 12.5 sec. before the thunder is heard. At what distance did the lightning occur, the temperature being 20° ? 5. The mean distance of the sun from the earth is 93,(XX),C)00 miles. How long after an explosion occurs upon the sun would we hear it if air at 0° were provided as a medium for the transmission ? (Light reaches us from the sun in 499 sec.) II. Properties of Musical Sounds 294. Properties of Musical Sounds. — Musical sounds have three characteristics or properties ; namely, (i) intensity or loud- ness, (2) pitch, and (3) quality or timbre. Loudness. — Intensity has already been considered. It is de- termined by the energy of the sound waves. Loudness refers to the sensation produced upon the ear. It increases with the intensity ; but we cannot say that they are proportional, as loud- ness cannot be measured. Loudness depends in part upon the pitch, a shrill sound being more distinctly heard than one of equal intensity but of low pitch. Pitch. — Sounds of definite pitch are produced only by bodies whose vibrations are regular and periodic. The waves of such a sound are of equal length and are sent out from the sounding body at equal intervals of time. An increase in the number of vibrations produces what is called a higher pitch {Exp.). Quality or timbre is that property by which we distinguish be- tween sounds produced by different bodies, even when they have the same pitch and intensity. We know at once from the quality of the sounds whether a piece of music is being played on a violin, a flute, or a cornet. We recognize familiar voices principally by their quality, although pitch, loudness, and peculiarities of pronun- ciation are also of assistance. The cause of quality will be con- sidered later. 295. Differences between Musical Sounds and Noises. — The pitch, intensity, and quality of musical sounds remain constant for appreciable intervals of time and do not change irregularly. A musical sound is often called a tone or note. All other sounds are 228 Sound called noises. A noise usually consists of a number of sounds pro- duced by the vibration of the sounding body in parts or segments. These vibrations not only differ among themselves, but are also irregular in rate and amplitude ; they are discordant, unsteady, and nonperiodic. A noise has therefore no definite pitch, and its quality is nonmusical. 296. Measurement of Pitch. — The pitch of a note may be expressed either relatively or absolutely. It is expressed rehi- tively by stating its relation to some other note, generally the keynote of the musical composition in which it occurs (Art. 302). The relative pitch of a note is easily recognized by a trained ear. ThQ abso/ufe pitch of a note is measured by the number of vibrations per second of the sounding body. This is called the vibration number ox frequency of the note. Thus the absolute pitch of the C fork which corresponds to " middle C " of the piano or organ is 256 ; />. the prongs of this fork make 256 vibrations per second. In physics the word pitch generally signifies the absolute pitch or vibration number of the note. 'llie vibration number of a sound can be determined experi- mentally either by causing the sounding body to make a perma- nent record of its vibrations (called the graphic method), or by comparing it with a sound of known pitch. The graphic method is illustrated in part in Fig. 140. A projecting point attached to one prong of the fork traces f.,^, a wavy line on a piece of smoked glass as the vibrating tbrk is drawn over the glass, or the glass pulled from under the fork. Each wave of the line is a record of one vibra- tion of the fork. If by some additional device, not shown in the figure, the time occupied by the fork in tracing the line is deter- mined, the number of vibrations per second can be computed. Comparison with sounds of known pitch, such as the notes of tuning forks, will serve all the purposes of elementary physics. Properties of Musical Sounds 229 297. The Relation between Pitch, Wave Length, and Velocity. — Let n denote the vibration number of a sounding. body, / the length of the waves that it produces in a given medium, and v the velocity of sound in that medium. Since a wave starts from the body with each vibration, a train of n waves is sent out in one second, the last of which will be on the point of leaving the body at the end of the second. During the second the first wave of the train travels the distance v ; hence, the n waves extend over that distance. From which v = /n. Assuming the velocity of sound in the medium to be known, we can from this relation compute the wave length of a sound of given pitch or the pitch of a sound of known wave length. Laboratory Exercise 43. 298. Interference of Sound. — When a sounding fork is held close to the ear and is slowly rotated about the stem as a vertical axis, it will be observed that during one complete rotation there are four positions of the fork in which it is not heard. The sound is faintly heard when the fork is turned very slightly in either direction from a position of silence, and swells to a maximum midway between these positions. With the fork held in a posi- tion of silence, sound is restored by covering either prong with a small cylinder of paper or other material, care being taken not to touch the prongs, as this would stop the vibration {Exp.). These curious effects are explained by Figs. 141 and 142, which represent the sound waves about a vibrating fork, as seen with the ends of the fork pointing toward the observer. As the prongs move apart, a conden- sation is set up on the outside of each, and a rare- faction between them ; as they Fig. 141. Fig. 142. 230 Sound move toward each other, opposite conditions are produced. If tlie space about the fork were partitioned off into four compartments, as indicated in the figures, there would be condensations and rare- factions on opposite sides of the partitions at equal distances from the fork, as shown in Fig. 141 ; but, without such partitions to keep the condensations and rarefactions apart, their opposing ten- dencies destroy each other where they meet, causing silence at these places, as shown in Fig. 142. The principle of the composition of motions as studied in mechanics applies to the resultant vibration of any portion of a medium when acted upon simultaneously by two or more trains of waves. The waves from a tuning fork are an example of the simplest case ; namely, that of two trains of waves of exactly equal wave length and amplitude, traveling in the same direction, the waves of one train being half a wave length in advance of those of the other train. In the region where the two trains of waves meet, the condensations of each unite with the rarefactions of the other. The condensations would be transmitted by a for- ward motion of the air, and the rarefactions by an equal backward motion at the same time; hence the air in this region remains at rest and there is neither condensation nor rarefaction. Silence is thus the result of the inUrference of the waves with each other. 299. Beats. — The sounds of two forks of exactly the same pitch unite perfectly into one sound. If the forks are sounded together after slightly lowering the pitch of one of them (by stick- ing a piece of soft wax near the end of one or both prongs), the sound periodically swells and dies away in strongly marked pulsa- tions, called beats {Exp.), Let us suppose that two middle C forks are used (vibration number = 256), and that, by loading with wax, one is reduced to 255. At intervals of one second the forks "keep step" in their vibrations ; and the waves that they then set up approximately coincide — condensations with condensations and rarefactions with rarefactions, as at ^ and C (Fig. 143). These waves unite in resultant waves of increased intensity, as represented at X and Z. Properties of Musical Sounds 231 Half a second after each coincidence, the forks vibrate oppositely, the condensations produced by each approximately coinciding with the rarefactions produced by the other, as at B; and the resultant waves are of diminished intensity. A complete set of intensified and weakened resultant waves is thus sent out from the forks in one second. This constitutes one beat. Beats may therefore be defined as regularly recurring pulsations of sound caused by the successive reenforcement and interference of two sets of sound waves differing slightly in wave length or pitch. The number of beats per second is equal to the difference between the vibration numbers of the two sounds. Hence the beats become more frequent when the pitch of the loaded fork is further lowered by using more wax (Exp.), PROBLEMS 1. Show from the formula v = /n that the wave length of a sound of given pitch is proportional to the velocity of sound in the medium. 2. Find the wave length of middle C in the air at 20*^; in water. 3. Why is the sound of a fork restored in the position of silence when one prong is covered? 4. Why is the pitch of a fork lowered by loading its prongs? 5. What use can be made of beats in tuning two sounding bodies to the same pitch? 300. Musical Intervals. — The in/erva/ between any two notes is measured by the ratio of the vibration number of the higher to that of the lower. Two notes are said to be in unison when they have exactly the same pitch. The interval between two notes in 232 Sound unison is unity (the ratio of equal numbers). If the vibration number of one note is twice that of another (interval = 2), the first is said to be an octave above the second. Other intervals are considered in Art. 302. 301. Harmony and Discord. — If the effect of two or more tones when sounded together is pleasing to the ear, the tones are said to be harmonious or consonant; if the effect is unpleasant, they are said to be discordant or dissonant. The two wires of a sonometer (Fig. 144) produce one contin- uous sound when tuned to exact unison ; but, when the pitch ^^Wy Fh; 144. of one of the wires is gradually raised (either by shortening the length of the vibrating portion with the movable bridge or by increasing the tension), beats are heard. The beats increase in frequency as the interval is increased ; and, as they become too rapid to be recognized individually, they pass from an unsteady, rattling sound into a discord. As the interval is still further increased, the tones presently become less discordant, then har- monious, then again discordant, etc. {Exp), Four intervals can thus be found between the original tone and its octave for which the tones are in harmony ; at all other inter- vals between these limits they are more or less discordant. It can be shown that these four intervals are {, J, f , and | respec- tively. These ratios are frequently called simple ratios because they are expressible in small numbers. The most perfect harmony is that of a tone and its octave, and they are separated by the simplest possible interval (|). 302. The Major Diatonic Scale. — Musical scales are deter- mined by the comparatively few intervals that are pleasing to the Properties of Musical Sounds 233 ear. The major diatonic scale consists of a series of eight notes whose syllable names are do re mi fa sol la si do^ The intervals between the first or keynote and the other notes of the scale are as follows : — I I * I f 4 ¥ ^ These numbers are sometimes called the vibration ratios of the notes. The smallest whole numbers expressing the same ratios are 24 27 30 32 36 40 45 48 The intervals between successive notes of the scale are do re mi fa sol la si do 2 I ¥ if I ¥ S H The intervals f and y^ are called tones ; the interval |f is called a semitone. The eighth note, which is an octave above the first and is called by the same name, is taken as the first of another series of eight notes, each of which is an octave above the note of the same name in the preceding series. The scale may thus be repeated both upward and downwarcl over as many octaves as is desired. The intervals remain the same whatever the absolute pitch of the keynote may be. When middle C is taken as the keynote, the letter names and the vibration numbers of the notes of the scale are as given below : — f , Position on the stafi, 1 1 J -' ^ SI _. /^ €i •■^ 1 7 \ \ ^\ ^ 1 S-- h i» ^» 6> h *".), It was proved by Helmholtz, a noted German physicist, that the quality of any sound is determined by the overtones which accompany its fumlamental tone. Differences in the quality of sounds are due to the presence of different overtones or to differ- ences in their relative intensity. The tuning fork is the only in- strument that gives a simple tone ; but the notes of the diapason pipes of an organ are quite similar, being almost free from over- tones. A musical sound in which a number of. the lower over- tones are present is full and rich. The tones of the piano and the violin are examples. The penetrating character of the tones of brass instruments is due to their particularly strong overtones. 'ITie pitch of a sound is the pitch of its fundamental ; it is not altered by the accompanying overtones. III. Sympathetic and Forced Vibrations: Resonance Laboratory Exercise 43. 310. Sympathetic and Forced Vibrations. actions 1 Certain mechanical which occur with sounding bodies may be illus- trated on a visible scale by means of the apparatus repre- sented in Fig. 15b. Two pairs of pendulums are sus- pended from a light rod, CZ>, the pendulums of each pair being of equal length. The rod is supported by short cords from a fixed support. ^*°' '^- When any one of the pen- dulums is set in vibration, it pulls the rod from which it is sus- pended back and forth. Sympathetic and Forced Vibrations 241 This vibratory motion of the rod imparts a series of impulses to the other pendulums. AUhough the effect of a single impulse is almost inappreciable, a succession of such impulses causes the other pendulum of the same length to vibrate with increasing amplitude ; while the amplitude of the first steadily decreases as it imparts its energy to the other. Since the two pendulums have the same rate of vibration, the impulses imparted to the one that was at rest are rightly timed to produce a cumulative effect. The vibrations of this penduhmi are called sympathetic^ signifying that its natural rate is in agreement with that of the impulses to which it responds. The other pair of pendulums make a few vibrations with in- creasing amplitude, followed by an equal number during which the amplitude decreases till the pendulums are brought to rest. This series of increasing and decreasing vibrations is repeated in- definitely. The explanation of this behavior is that the impulses are not timed in agreement with the rate of these pendulums ; a few successive impulses produce a cumulative effect, but these are followed by an equal number which are opposed to the motion already produced and hence destroy it. Since these pendulums cannot be forced to vibrate in unison with the impulses, they cannot accumulate any considerable store of energy. When the rod is struck or drawn to one side and released (all of the pendulums being at rest), it vibrates much more rapidly than it does when under the control of a vibrating pendulum. Thus, although the rod has a natural rate of vibration, it does not persist in it as the pendulums do, but yields to the impulses of either a long or a short pendulum. The motion of the rod when thus controlled is called a forced vibration. 311. Forced Vibrations of Sounding Bodies. — The sound that comes from a table, an empty box, or a large board when touched by a vibrating fork is due to the forced vibration of the wood. Since the sound thus produced always has the same pitch as the fork, whatever this may be, it is evident that wood, especially in the form of a thin board, is easily forced to vibrate in unison with 242 Sound periodic impulses of any frequency — a behavior like that of the rod from which the pendulums were suspended (Fig. 150). When a violin is played, the sound is produced by the forced vibration of the body of the instrument. The pitch is . deter- mined by the vibration rate of the strings ; the quality, partly by the manner in which the string is bowed and partly by the kind of wood of which the instrument is made and the workmanship. The music of a piano comes from the large sounding board upon which the wires are strung. 312. Sympathetic Vibration of Tuning Forks and Strings. — A tuning fork may be made to vibrate sympathetically as follows : The stems of a sounding and a silent fork of exactly the same pitch are touched to the top of a table a short distance apart. After one or two seconds, the fork that was sounded is stopped with the fingers or removed from the table, and a sound is then heard from the other fork. If the sound is too faint to be heard at a distance, the vibration of the fork can be proved by touching a suspended pith ball to one of its prongs. This vibration is caused principally by impulses imparted through the stem by the vibrating table. Probably from 500 to 1000 such impulses are required to produce the observed effect {Exp.). The silent fork can also be made to vibrate sympathetically by holding it in the fingers close to the vibrating fork, held in the other hand, the forks facing each other but not touching. In this case the impulses are imparted by the sound waves in the air {Exp.). These experiments fail if the forks are not in perfect unison, as will be found by repeating them with one of the forks loaded with wax {Exp.). If the two wires of a sonometer are tuned to exact unison, either will vibrate sympathetically when the other is sounded, the impulses being transmitted principally through the body of the instrument. As the pitch of one of the wires is slowly changed, the response of the silent wire immediately becomes very faint and quickly ceases {Exp,). Sympathetic and Forced Vibrations 243 These experiments show that tuning forks and strings, like the pendulums, persist in their natural rate of vibration, — a behavior very different from that of sounding boards and the bodies of stringed instruments. Laboratory Exercise 44, 313. Resonance of Air Columns. — The reenforcement of the sound of one body by the sympathetic or forced vibration of another is called resonance; but the word most frequently refers to the reenforcement of sound by the sympathetic vibration of partly inclosed bodies of air. We shall use the word only in this narrower sense. Resonance may be secured by means of a tube provided with a close-fitting piston (Fig 151). When the piston is in a certain £ Fig. 151. position, the sound of a fork held at the end of the tube is strongly reenforced by the sympathetic vibration of the column of air extending to the piston. The sound from the tube is very much fainter when the piston is moved even a very short distance in either direction, from the position of maximum reenforcement {Exp^. The column of air will vibrate strongly only at its natural rate, which varies with the length. This is further shown by repeat- ing the experiment with a fork of different pitch. It will be found that the length of the column for maximum resonance is inversely proportional to the vibration number of the note (^Exp.). The vibration of the air column is longitudinal. As the nearer prong of the fork moves toward the end of the tube, the air par- ticles in the tube are driven a short distance toward the farther end, producing a condensation which is greatest at the piston. When the prong moves away from the tube, the air expands by a motion of the particles toward the mouth of the tube. The 244 Sound expansion, like the compression, is greatest at the piston. Thus the change of density of the air is greatest at the piston and di- minishes toward the open end, where the density remains nearly constant. The amplitude of vibration of the air particles is greatest at the open end and diminishes to zero at the piston. The tube controls the vibration of the air for a short distance beyond its end, and it has been found by experiment that the true length of the air column is equal to the length of the tube (to the piston) plus half the diameter of the tube. It can be shown that this length is one fourth of a wave length, i.e. is one fourth the length of the sound wave set up by the vibration of the fork and the air column. Second resonance occurs when the length of the air column is increased to three fourths of a wave length. The mode of vibra- tion of the air is shown in Fig. 152, which represents the condi- Y | |!|lll ll li l lllll l li lll l!llli !| ii:: uimwimii liiiiil m ■ I \ I / ami Fi<; tion of the air at intervals of one fourth of a vibration. AB is the length for first resonance, AD for second resonance. AB, BC, CD, are each one fourth of a wave length. At B and D there is no motion, and the change of density is the greatest. These Sympathetic and Forced Vibrations 245 positions are called nodes. (Compare with the nodes of a string vibrating in segments.) At A and C there is little or no change of density and the amplitude of vibration is greatest. These positions are called atiiinodes. The arrows in the second and fourth parts of the figure indicate the direction of motion of the air particles. At the instant represented in the first and third parts of the figure the air is at rest throughout the tube. BD is a vibrating segment of the air column; its length is half a wave length. AB is half a segment. If the tube were further lengthened by half a wave length, another whole segment would be added to the vibrating air column and third resonance would occur. 314. Resonance caused by Noise. — Any partly inclosed body of air has a natural rate of vibration as a whole, and, when sub- jected to a series of impulses rightly timed, it will vibrate sympa- thetically. A noise always affords such a series of impulses, since it consists of an indefinite number of different rates of vibration. Hence a hollow body, as a tumbler, a glass or metal tube, or a sea shell, continually sounds a faint note, which is distinctly heard when the body is held to the ear. The pitch of this sound re- mains constant when different noises are made in the vicinity, but its loudness varies, in many cases swelling to a loud roar when the foot is scraped on the floor {Exp.). 315. The Whistle. — In wind instruments the sounding body is a column of air confined in a tube. The whistle is a familiar illustration. Its action is explained as follows : A current of air passing through a narrow slit, a (Fig. 153), is directed against the farther edge of a lateral opening, b. Con- tact with this edge causes the current of air to 3 ' r-—^ flutter irregularly, producing a faint rustling noise. The column of air, c, confined in the body of the whistle is thrown into strong sympathetic vibration by those impulses from the current of air which are in unison with its natural rate. The note thus produced is generally so much louder than the noise of the air current that the latter is not heard. By 246 Sound means of a whistle fitted with a piston it can be shown that the pitch of the sound rises as the size of the air chamber is de- creased {Exp. with Ga/ton's whistle or organ pipe with piston). Within wide Hmits of pitch, the inclosed air always finds its own note in the noise of the air current, and reenforces it. 316. Organ Pipes. — An organ pipe is merely a whistle of spe- cial construction. The pitch of its note is determined by the length of the air column (cor- rected for the diameter of the pipe). The quality of the sound is modified by the shape and material of the pipe. Figure 154 represents a rec- tangular wooden pipe and Fig. 155 a cylindrical pipe of metal. Some pipes are provided with a tongue or reed, against which the cur- rent of air from the bellows is directed, causing it to vi- brate. The reed is tuned to the natural rate of the air column in the pipe, which therefore vibrates sympatheti- cally. The note of a reed Organ pipes are made both open and closed at the top ; the latter are called stopped pipes. The following laws may be illustrated by means of a pipe provided with a piston : — I. The vibration number of an air column is inversely propor- tional to its length. II. The pitch of an open pipe is an octave above that of a closed pipe of the same length. 317. Fundamental Tone and Overtones of Organ Pipes. — In sounding its fundamental note the air in a closed pipe vibrates Fig. Fig. 155- pipe has a characteristic quality. or THF UNIVERSI7 Sympathetic and Forced Vibrati\jsc;,, /^^^v^ in a half segment, with an antinode at the mouth and a node at the closed end, as a resonance tube does for first resonance (Art. 313). Thus the length of a stopped pipe is one fourth the wave length of its fundamental tone. The first overtone is produced by vibration in one and one half segments, as for second reso- nance (Art. 313). Its vibration number is three times that of the fundamental, and hence corresponds to the second overtone of a string. The second overtone is produced by vibration in two and one half segments, and corresponds to the fourth overtone of a string. When a pipe is sounded by a gentle current of air, only its funda- mental is heard ; with a greater pressure of air, this gives place to the first overtone ; and, with still greater pressure, the second overtone is sounded {Exp.). The air in an open pipe necessarily vibrates with an antinode at each end. When sounding its fundamental, there is but one node, and this is at the middle ; i.e. the air vibrates in two half segments. The length of an open pipe is therefore half the wave length of its fundamental tone. The first overtone is produced by vibra- tion with one segment between the half segments at the ends, the second overtone with two segments between, the third with three, etc. From the relative length of the segments thus produced it will be seen that the complete series of overtones may be present as with strings. The difference in the overtones present causes a difference in the quality of open and closed pipes. 318. Wind Instruments. — Each pipe of an organ sounds only one note ; hence in a complete set of pipes there is one for each note of the instrument. An organ is provided with several sets of pipes, the notes of each set differing in quality from those of the 248 Sound other sets. Most wind instruments are provided with but one tube, the different notes being produced either by varying the length of the tube or by sounding overtones. In the trombone (Fig. 156), one part of the tube, SL^ sHdes within the other, and the tube is shortened by pushing the shding part farther in. The tube of the cornet (Fig. 157) forms sev- FiG. 157. eral turns or convolutions, which may either be included or cut off from the remainder of the tube by means of pistons, '. At the beginning of the nineteenth century the subject was again taken up by a number of able physicists. By a series of remarkable experiments adtiitional facts were brought to light, which amounted to conclusive evidence against the emission theory and in favor of the wave theory. The latter, with some comparatively recent modifications, is now regarded as fully established. The facts and experiments that led to the final adoption of the wave theory lie almost wholly beyond the scope of elementary physics ; we must, however, make use of the sim- pler elements of the theory in explaining the phenomena with which we have to deal. 329. The Ether. — The ether fills all space throughout the known universe, for it is only by means of light that reaches us from the heavenly bodies that we have any knowledge of them. It cannot be excluded from a vacuum ; in fact, there is no evi- dence that the quantity of it in a receiver is diminished in the slightest degree by whatever means the receiver may be exhausted. The velocity of light through transparent solids, liquids, and gases is enormously greater than it would be if these bodies served as media by means of which, as well as through which, the light is transmitted ; hence it is concluded that light is transmitted through bodies by means of the ether which fills the spaces between their molecules. While the ether must be regarded as a form of matter, it is in all probability millions of times less dense than air under atmos- pheric pressure, and there is no evidence either that it is subject to gravitation or that it is composed of molecules. On the con- trary, from the manner in which it transmits disturbances, it is thought to be perfectly continuous and incompressible. It is supposed to fill the intermolecular spaces in all bodies fi-om the most highly rarefied to the densest. 330. Nature of Radiation. — Some helpful ideas in regard to the origin and transmission of radiant energy (including light) can be gathered from a comparison with the phenomena of sound. A sounding body, as we have learned, is the center of a Nature and Transmission of Light 257 periodic disturbance which is radiated (transmitted radially) from it in all directions through the surrounding medium, in the form of concentric spherical shells, called sound waves. Now the molecules of all bodies, as we have also learned, are sup- posed to be in constant and inconceivably rapid vibration (Art. 186). According to the wave theory, the vibrations of each mole- cule disturb the surrounding ether; and, as in the case of sound, this disturbance is radiated with equal velocity in all directions as a train of concentric spherical waves. Thus each molecule of a body may be compared to a sounding fork, and the entire body to a large group of forks, each of which is sending out a train of waves. As the energy of a sounding body is gradually imparted to the air or other medium, so too the heat of bodies is gradually imparted to the ether as energy of wave motion, and in this form it is called radiant energy. It must not be supposed, however, that sound waves and ether waves are at all alike in character ; we should rather expect the contrary, since the properties of the ether are very different from those of ordinary matter. Ether waves consist of a periodic dis- turbance 0/ some sort; they have a definite length (measured radially, as in the case of sound waves) and travel with a definite, though very great, velocity ; but they do not consist of conden- sations and rarefactions and the vibrations are not longitudinal. 331. Luminous and Nonluminous Radiation. — All known bodies are a constant source of radiant energy, since all possess some degree of heat ; but bodies colder than their surroundings lose less heat than they receive by the absorption of radiation falling upon them, and hence become warmer. With few exceptions, bodies emit only nonluminous. radiation (the so-called "radiant heat") unless they are very hot. A piece of iron, for example, becomes luminous at about 525°, at which temperature it emits a dull red light. As the temperature increases, the light grows stronger and changes in color, at last becoming white. The nonluminous radi- ation also increases in intensity as the temperature rises, as is shown by the greater heating of the hand when held near the body. 258 Light When a body is heated, its molecules vibrate more rapidly and hence set up shorter waves in the ether, — an effect similar to that produced by raising the pitch of a sounding body. As there are sound waves too long and others too short to cause the sensation of sound, so too there are ether waves both too long and too short to cause sight. Ether waves of the proper length to stimulate the optic nerve and cause the sensation of vision are called light. The distinction between light and nonluminous radiation is there- fore primarily a physiological one (Arts. 221 and 222). 332. The Propagation of Light in a Homogeneous Medium. — Any space or substance through which light can travel is called a medium. A medium is said to be homogeneous when its chemical composition and density are the same in all parts of it. Although light is transmitted or, as we commonly say, propagated in any medium by means of the ether in its intermolecular spaces, the substance itself affects the process in different ways, as will be seen later. When a beam of sunlight is admitted into a darkened room, its path, which is rendered visible by the dust particles in the air, is seen to be perfectly straight {Exp.). This is perhaps the best illustration of a very general law ; namely, In aiety homogeneous medium light travels in straight lines. The most familiar conse- quence of this fact is the formation of shadows. The light that passes on either side of an object continues in a straight line ; if it bent round into the space behind ttie object, there would be no shadow. Figure 165 is a section diagram in which each circle represents a wave of light from a small luminous source at/. The light that passes through an opening, (9, in a screen. Nature and Transmission of Light 259 > > > m Fig. 166. AB, is represented by C/D. It has a conical shape and is called a cone or pencil of lights regardless of the shape of the opening through which it passes. When the source of the light is at a relatively great distance, any small area of a wave front is sensibly plane (Fig. 166), and the light that passes through a small opening is cylindrical in shape and is called a beam of light (represented by CEFD in the figure) . A pencil or a beam of light so slender that its cross-section has no appreciable area is commonly called a ray of light. A ray is often regarded merely as a mathematical line indicating a direction in which light travels. In this sense any radius of a train of spherical waves is a ray. Rays, in either sense of the word, are perpendicular to the wave fronts. 333. Why Light travels in Straight Lines. — The thoughtful pupil will perhaps wonder why light does not spread out after going through an opening or past the edge of an object. We know that sound travels round buildings and other obstacles. If light is a wave motion, why does it not do the same? It was the want of an answer to this question that caused Newton and his followers to reject the wave theory. After more than a century, experiments were devised which proved that this difference between the behavior of light and sound is due to the very great difference in their wave lengths. The waves of most sounds are from one to ten feet in length ; light waves (which are also capable of accurate measurement) vary from 33,000 to 64,000 to the inch. It was found that light waves and sound waves behave in a similar manner when they pass through openings or encounter obstacles of the same relative size in comparison with their wave lengths. The propagation of light in straight lines, leaving the space behind opaque objects in shadow, is due to the fact that ordinary bodies and openings are enor- 26o Light mously large comj)ared with the wave length of light. Sound l)ehaves in a similar manner under corresponding conditions, forming what may be termed sound shadows. " Some few years ago a jx)wd^r hulk exploded on the river Mersey. Just opposite the spot there is an opening of some size in the high ground which forms the watershed between the Mersey and the Dee. The noise of the explosion was heard through this opening for many miles, and great damage was done. Places quite close to the hulk, but behind the low hills through which the opening passes, were completely protected, the noise was hardly heard, and no damage to glass and such like happened. The opening was large compared with the wave length of the sound " — Glazebrook's Phys- ical Optics, When light passes through an opening that is not large com- pared wth the wave length (as is generally the case with sound), it spreads out into the region that is ordinarily occupied by the shadow. A simple example of these effects is obtained by look- ing through a handkerchief, held close to the face, at a brightly illuminated pinhole or narrow slit about the width of a pin. (Try it.) The pinhole or slit may be made in a piece of cardboard, and illuminated by holding it in front of a lamp or gas jet. The light spreads out in different directions in passing through the narrow spaces between the threads of cloth, causing the slit to look like a number of parallel slits, and the hole like a square pattern of many holes. Phenomena of this class are studied in advanced physics. It is by means of experiments involving such phenomena that the wave lengths of light are determined. Laboratory Exercise -//. 334. Shadows. — A cone of light is intercepted by an opaque body, as ab (Fig. 167), when the source of the light, Z, is so small that it may be regarded as a point; and the light is wholly excluded from the portion of this 6"'^^^^^B conical space that lies beyond the body. Fig. 167. d When the source of light is of appreciable Nature and Transmission of Light 261 size, the light is wholly excluded from a portion of the space beyond the body, as acdb (Fig. 168) ; and this space is surrounded or enveloped by a space from which the light is partially excluded. The latter space receives light from a part of the source, the light from the remainder being inter- cepted by the object. In physics the word shadow means the space from which light is wholly or partly excluded by an opaque body. The dark area upon any surface where it intercepts a shadow is a cross-section of the shadow, and should be so named. The part of the shadow from which the hght is wholly excluded is called the umbra; the partly illuminated space surrounding the umbra is called the penumbra. The penumbra merges impercep- tibly into fully illuminated space at its outer surface ; the boundary between the penumbra and umbra is more sharply defined. 335. Solar Eclipses. — In Fig. 169, 6" represents the sun, ^ the earth, M^ the moon at new moon, and M^ at full moon. The Fig. 168. ■'V Fig. 169. shadows of the earth and the moon are diminishing cones, termi- nating in a point. (Why?) On account of the varying distances of the sun and the moon from the earth, the moon's shadow {i.e. the umbra) sometimes reaches the earth and is sometimes too short to do so. The cross- section of the moon's shadow is never more than 167 miles wide at the earth's surface. Within the shadow the sun is totally eclipsed ; within the penumbra, which covers a much larger area, the eclipse is partial. It is evident that an eclipse of the sun can occur only at new moon ; but there is not an eclipse at every new moon, for the moon 262 Light generally passes to one side or the other (above or below the plane of the paper in the figure) of the straight line between the sun and the earth. The least number of solar eclipses that can occur in a year is two, and the greatest number is five. 336. Lunar Eclipses. — The diameter of the earth's shadow at the distance of the moon is about two and two thirds times the diameter of the moon. When the moon passes entirely into the shadow, it is totally eclipsed ; when only one side of it passes through the shadow, the eclipse is partial. There is no perceptible dimming of the moon within the penumbra until it almost reaches the shadow. An eclipse of the moon, either total or partial, is of course visible to half the earth simultaneously. Since the moon is a nonluminous body, shining only by reflected sunlight, it would be invisible when totally eclipsed if it were not for the fact that some light is bent out of its course (refracted) into the shadow in passing through the earth's atmosphere. The moon is thus illuminated with a dull, copper-colored light. An eclipse of the moon can occur only at -ftrfHnobn ; but the moon generally escapes the shadow by passing to one side or the other of it. The number of lunar eclipses in a year varies from none to three. 337. Images produced by Small Openings. — When light from any luminous or brightly illuminated object falls upon a screen after passing through a minute opening, such as a pinhole, it forms upon the screen an inverted image of the object. Figure 170 shows how such images are produced. Every point on the surface of the object is a source of light which travels outward in all direc- tions from the surface. A sle Jer cone of this light from each point passes through the pinhol and illuminates a small spot on the screen of the same shape as the opening. Since these spots have the same relative positions as the corresponding points of Nature and Transmission of Light 263 liie object, and are illuminated by light of the same color as those points, they unite into an image which reproduces the form and color of the object. The inversion of the image is due to the crossing of the cones of light at the opening. If the opening is very small, the image is quite sharply defined, but faint. With a larger opening, the image is brighter, but poorly defined (blurred) ; for the light from each point of the object now covers a larger spot pn the screen, and these spots overlap more and more as their size increases.^ 338. Intensity of Illumination. — The intensity of illumination on any surface is the quantity of light received per unit area of the surface. Effect of Distance, — The intensity of the light from any source, or the intensity of the illumination that it produces on any surface, is inversely proportional to the square of the distance from the source. This " law of inverse squares " is the same as that for sound (Art. 288), and for the same reasons. The reasoning, as applied to light, may be briefly stated as follows: (i) Assuming that there is no loss of light by absorption or other cause, the same total quantity of light (radiant energy) passes all cross- sections of a cone of light ; (2) hence the quantity of light per unit area at any distance is inversely proportional to the area of the cross-section of the cone at that distance ; (3) but the area of the cross-section of a cone of any shape is proportional to the square of the distance from its vertex (Fig. 171); (4) hence the law. 1 If the class room can be made perfectly dark, an interesting study of these //'«- hole images, as they are called, can be made by admitting light into the darkened room through a small hole in a window screen or shutter, and catching it up>on a screen of oiled tissue paper or upon the opposite wall of the room. In the latter case the opening must be a centimeter or more in diameter to give suflficent illumi- nation. Under these conditions an image of the landscape in its natural colors will be formed upon the wall or the screen. A pinhole camera can be made from a pastelxjard box a foot or more in length. A large pinhole is made in the center of one end to admit the light, which is caught upon a screen of oiled tissue paper pasted in position across the center of the box. A hole half a centimeter or more in diameter is made in the other end of the box. The image upon the screen is viewed by placing the eye close to this hole. 264 Light Effect of Illuminating Power. — The total quantity of light con- tinuously given out by any source is called its illuminating power. The light given out by a standard candle is taken as the unit and is called a candle power. Thus an incandescent lamp of sixteen candle power gives out sixteen times as much light as a standard candle. The intensities of iHumination produced by two sources of light at equal distances are proportional to the illuminating powers of the sources. Effect of Distance and Illuminating Poiver Combined. — Let P denote the illuminating power of a source of light, and / the in- tensity of illumination which it produces at the distance D; then, since / is proportional to P and inversely proportional to the square of Z>, we may write p ^^ D"' 339. Photometry. — Photometry deals with the comparison and measurement of the illuminating powers of different sources of light. Any apparatus by means of which such measurements are made \%Z2^^^2i photometer. We can form no reliable estimate of the relative brightness of unequally illuminated surfaces, but are able to judge with considerable accuracy whether two adjacent parts of the same surface are equally illuminated ; hence, with all forms of photometers, the distances of the lights compared are adjusted to give equal illumination. Let Px and P^ denote the illuminating powers of two sources of light, and let /, and L denote the intensities of illumination which they produce at the distances D^ and Z>2, respectively ; then, If the distances are such that the intensities of illumination are equal {i.e. if I^ = /a), then ' — ^^2 f.j.— p.p..r)'i.r)2 Nature and Transmission of Light 265 This is the relation used in photometric measurements. Stated in words : The illuminating powers of two sources of light are pro- portional to the squares of the distances at which they produce equal illumination. Laboratory Exercise 48. 340. The Shadow Photometer (Rumf ord's Photometer) . — There are several forms of photometers ; but the shadow photometer, devised by Count Rumford, will serve as a sufficient illustration. Figure 172 shows the adjustment of the apparatus for a comparison 172. of the illuminating powers of a lamp and a candle. The rod, Ry casts two shadows ; c is due to the candle, and / to the lamp. Each source of light illuminates the shadow due to the other ; hence when they are placed so that the shadows are equally dark {i.e. equally illuminated), they give equal illumination at their respective distances from the screen. The room must be dark- ened, or other sources of light will make the shadows too foint for accurate comparison. 341. The Velocity of Light. — The velocity of light in a vacuum and in air is 186,000 miles per second in round numbers, — a velocity sufficient to encircle the earth seven and one half times in one second. Notwithstanding the difficulties involved in the measurement of such rapid motion, this velocity has been re- peatedly determined with consistent results by two experimental methods ; it has also been computed by two independent methods 266 Light from astronomical data. We shall consider only the astronomical method by which the first determination of the velocity of light was made. Jupiter, the largest of the planets, revolves about the sun in an orbit whose diameter is about five times that of the earth, the time occupied in one revolution being nearly twelve years. In Fig. 1 73, S represents the sun, £* and £ two positions of the earth in ©\ its orbit, y* and J two positions of \-v^ Jupiter. Jupiter is accompanied \T^ by a number of satellites (moons), s ]i which revolve round it as the moon I does round the earth. The nearest / of these satellites is shown in the pftfc _ figure. It passes through the _ / shadow of Jupiter in each revolu- Fic. 173. / •' * / tion, and is thus eclipsed at regular intervals of 42 hr. 28 min. and 36 sec. An observer does not see these eclipses when they occur ; for, after the satellite has entered the shadow, it continues visible unAV the light that last Uft it reaches the earth. If the eclipses were observed from any constant distance, they would be seen at regular intervals ; for they would all be seen the same length of time after their actual occurrence. For example, if the earth remained at its least distance from Jupiter, each eclipse would be seen 35 min. after it occurred, that being the time required for light to travel the intervening distance, EJ\ if the earth remained at its greatest distance, EJ, each eclipse would be seen 51 min. and 40 sec. after it occurred, and the observed intervals between the eclipses would be the same as before. But, while the earth, in its annual revolution, is receding from Jupiter, the observed interval between successive eclipses exceeds the true interval by the time required for light to travel the' added distance due to the earth's motion during the interval. While the earth is advancing* toward Jupiter, the conditions are reversed and the observed intervals are less than the true intervals. Hence if the eclipses are computed ahead for one year, begin- Nature and Transmission of Light 267 ning when the earth is at E and assuming a constant interval, the echpses as observed fall constantly more and more behind until the earth is at E\ when they are 16 min. and 40 sec. late. Dur- ing the second half of the year, the intervals are less than the average, and the loss is gradually made up; so that when the earth has arrived at E the eclipses are again on time. These irregularities in the observed intervals were discovered and explained by Roeme r. a Danish astronomer, in 1675. He announced that the whole apparent retardation of the eclipses from E to E' was the time required for light to travel across the earth's orbit, which is known to be a distance of 186,000,000 mi.^ (Compute the velocity of light from the given data.) PROBLEMS 1. {a) What is the necessary condition for a shadow without a penumbra? (^) for an umbra of finite length? (r) for an umbra of indefinite length? (-^^ / \ ^,j^ The ray EFGH is re- """^-^^ / \ ,-'-"'" fracted toward the per- ^^ ^Z--i7fr^'~-\ ^ ^" pendicular MNoxi enter- _^^,-^^^/a^\ '^'^"^^x'^Ell ing the prism and from ' ^^ , ^ ^^^ the perpendicular il/'iV' '" ^^* on leaving it. The deviations d and (f are in the same direction (away from the refracting angle) ; hence the total deviation is their sum and is measured by the angle KPH. This angle is called the afig/e of ikviation. The deviation increases with the refracting angle of the prism and its index of refraction ; it also varies with the angle of inci- dence, being least when the angle of incidence is such that the angle of emergence is equal to it. The deviation varies slightly for light of different colors, producing effects which are considered later. The apparent source of the ray GH is some point on the line HL ; hence an object viewed through a prism is apparently dis- placed in the direction of the refracting edge of the prism. Laboratory Exercise 52, Parts II and III. 367. Partial Reflection and Refraction. — In general, when light meets a smooth surface separating two transparent media, part of it is reflected and part refracted. A number of illustrations are familiar where air is one of the media. For example, the 292 Light greater part of the light falling upon window glass passes through it by refraction, as described in Art. 365 ; but a considerable por- tion of it is regularly reflected from the front surface, forming an image of its source as in a plane mirror. Such images are dis- tinctly visible when the glass is backed with black cloth to pre- vent the transmission of light from the opposite side. Similarly, light falling upon the surface of still water is partly reflected, form- ing images ; but the greater part is refracted into the water. It is by partial reflection and refraction that a number of images of a small, bright object, as a candle flame or a lighted match, are formed by a single mirror when the images are viewed obliquely. (Try it.) Tiiese multiple images are especially prominent in mirrors of thick glass. Let ABDC (Fig. 206) represent a section of a mirror taken at right angles to the reflecting surface AH^ and O a luminous point in front of the mirror. Part of the incident ray OE is reflected from the front surface at E^ forming (or helping to form) the image /i. The greater part of the incident light enters the glass, and is reflected at the rear surface. The greater part of this light is refracted into the air at /% forming the brightest of the images /, ; the remainder is inter- nally reflected at /% is again reflected at the rear surface, and the greater part of it passes into the air at G, forming the image /j. This process is repeated, forming still other images ; but their number is limited, as the light rapidly diminishes in intensity with the successive reflections and refractions. 368. Total Reflection. — When light is incident in the more re- fractive of two media (as when it passes from water into air), the angle of refraction is always greater than the angle of incidence. For a certain angle of incidence, MOE Fig. 207. /^ u / A "*' c/ ^ /^ B "^£:=i^s^ssyi=-^=-£:s- '^KUtTrT^ M i=^"2^' - 1 Fig. 208. Refraction of Light 293 (Fig. 207), the angle of refraction is 90°, and the refracted ray is parallel to the surface of the water. For a greater angle of incidence, as angle MOF, refraction cannot take place, and all of the light is reflected internally according to the laws of reflection. The ray OFG is therefore said to be totally reflected at F. Total reflection in water can be exhibited by reflecting a beam of light upward through water in a rectangular glass vessel (Fig. 208) {Exp.). The angle of incidence in the more refractive medium for which the angle of refraction is 90° is called the critical angle. When the angle of incidence is less than the critical angle, refraction and partial reflection take place ; when it is greater, total reflection occurs. When light is incident in the less refractive medium, refraction and partial reflection take place at all angles of incidence. The critical angle for water and air is 48.5° ; for crown glass and air, about 41° ; for flint glass and air, about 38° ; for diamond, about 24°. Laboratory Exercise ^4. 369. Illustrations and Applications of Total Reflection. — When a glass of water is held above the level of the eye, its surface, viewed from below through the side of the glass, looks like a mirror. When a spoon or a pencil is placed in the glass, the part above the water is invisible, but a very distinct image of the immersed part of it is seen in the surface. This image is formed by total reflection. (Try it.) Glass prisms afford excellent illustrations of total reflection. Light that falls upon the inside of any face of the prism at an angle greater than the critical angle is totally reflected ; and, when the eye is in position ^^''" to receive this light after refraction into the air, the Fig. 209. reflecting surface has the appearance of a mirror and forms a brilliant image of the source of the light (Fig. 209). 294 Light- Prisms having an angle of 90° and two angles of 45° are used in astronomical telescopes and in other optical instruments to change the direction of the light by 90° (Fig. 210). Incident light per- pendicular to the face AB enters the prism without deviation and meets the face BC 2X an angle of 45°. \^^ | / Since this is greater than the critical angle, the light is \J*"- totally reflected at the same angle, and passes out of the ^ face AC without deviation. Such prisms are the most •10. 210. pgj.fgj,^ mirrors known. They give only a single reflec- tion, thus avoiding the faint, overlapping images due to multiple reflection in ordinary mirrors. A totil-reflecting prism at the eye end of a telescoi)e adds to the comfort of the observer, as it enables him to look obliquely tlownward in viewing the heavenly bodies, instead of in the direction in which the telescope points. IV. Atmospheric Refraction 370. Atmospheric Refraction. — Although the refractive power of the air is small, it gives rise to a number of interesting and familiar phenomena. When we look over a bonfire or a hot stove at any object situated beyond it, the object appears to undergo a rapidly changing distortion, similar to that of a pebble in the bottom of a brook. This appearance is due to the colistantly changing refraction of the light as it passes through the currents of air rising from the fire ; for these currents consist of bodies of air of varying temperatures and hence of varying densities, and the refractive power of air increases with the density. A similar effect may often be observed when the line of sight passes near the surface of some object that has become hot in the sunshine. 371., Twinkling of the Stars. — The twinkling of the stars con- sists in a rapid, irregular variation in brightness. With the aid of a telescope, this is seen to be accompanied by a dancing motion. The phenomenon is wholly atmospheric ; the stars themselves are fixed and shine with a steady light. The dancing is a rapid change of apparent position, caused by changing refraction as currents of Atmospheric Refraction 295 air of varying density cross the line of sight. As a beam of light passes through successive layers of air, the refraction at the irregu- lar boundaries separating thorn may cause either a slight con- vergence or divergence of the beam. The first increases the intensity of the light, the second diminishes it ; and the twinkling is largely due to the rapid alternation of these effects. Stars near the horizon, the light from which traverses a greater stretch of atmosphere, twinkle more than those overhead. The twinkling also differs greatly on different nights according to the steadiness of the air. 372. Regular Atmospheric Refraction. — The inconstant or irregular refraction to which the twinkling of the stars is due is small in comparison with the regu- lar refraction, due to the increas- ing density of the atmosphere from its upper limit to the earth's surface. Light traveling obliquely downward through the atmos- phere is bent continuously toward the perpendicular (Fig. 211). The total deviation thus produced varies from zero for heavenly bodies directly overhead to a little more than half a degrfte at the horizon (it is greatly exaggerated in the figure). Since the angular diameter of the sun at the earth is about half a degree, the sun is really just below the horizon when it appears to be just above it. Thus, on account of atmospheric refraction, sunrise occurs from two to four minutes earlier than it otherwise would (depending upon the angle that the sun's path makes with the horizon), and sunset is retarded by the same amount. 373. Mirage. — In sandy deserts the reflection of the sky and of the scattered trees and other objects in the landscape is often seen in the distance, on hot sunny days, as in the surface of a calm lake. This optical illusion is called a mirage. It is due to the heating and expansion of the air in contact with the hot sand ; as a result of which the density of the air increases upward for Fig. 211. 296 Light some distance from the ground. Light traveling obliquely down- ward through this layer of air is gradually bent from the perpen- dicular; and the angle of incidence, if nearly 90° at first, may thus become greater than the critical angle. The light is then totally reflected by the layer of rarer air into which it cannot pass, and is refracted toivard the perpendicular as it returns through the denser air alx)ve. By this total reflection images are formed like those seen in the surface of still water (Fig. 212). The sky and other objects are also seen, at the same time, erect and in their true positions, by light that comes straight to the eye. V. Lenses 374. Lenses. — A lens is a portion of a transparent medium bounded by two curved surfaces or by a plane and a curved surface. Lenses are usually made of glass, and their curved surfaces are usually spherical. There are six forms of spherical lenses, sections of which are represented in Fig. 213. From their optical effects they are classed in two groups of three each, as follows : — Convex or Convergins^ Lenses. — The first three lenses repre- sented in the figure belong to this class. The first of these is Lenses 297 called double convex, the second plano-convex^ and the third con- cavo-convex. All are thicker in the middle than at the edges. They are called converging lenses, because light is more converg- ent or less divergent after passing through them than before Fio. 213. {Exp^. The three forms are equivalent in their effects so far as the purposes of elementary physics are concerned ; and the double- convex lens having surfaces of equal curvature is the only one that will be considered. Concave or Diverging Lenses. — To this class belong the last three lenses represented in the figure. The first of these is double-concave^ the second piano- concave , and the third convexo- concave. They are all thinner in the middle than at the edges ; and are called diverging lenses because they increase the diverg- ence of light passing through them {Exp.). The double-concave lens will be taken as the type of its class. 375. The Double-convex Lens. — The line joining the centers of curvature of the spherical surfaces of a convex lens (C and C, Fig. 214) is called iht principal axis of the lens. 298 Light Let OA be a ray of light from a luminous point on the prin- cipal axis. On entering the lens, the ray is bent toward the perpendicular AC ; on ^merging at B, it is bent from the per- pendicular BC. The deviation of the ray is the same as it would be if the lens were replaced by a prism ADB of the same mate- rial and having faces tangent to the lens at A and B. The angle between the tangent planes at the jwints of entrance and emerg- ence of a ray increases toward the edge of the lens {g^. angle £ is greater than angle D) ; hence the deviation also increases. A ray of light traveling along the principal axis falls perpendicularly upon both surfaces of the lens, and hence passes through it with- out deviation. The increased deviation toward the edge of the lens is almost exactly what is required to bring a// the refracted light to the same point, /. We shall for the present regard the focusing as perfect. Thus the diverging cone of incident light A'OG undergoes re- fraction at the surfaces of the lens and emerges as a converging cone, L///, forming a real '^' ^'^* image of its source at /. The effect of the lens is also shown in Fig. 215, in which the curved lines represent light waves. The points O and / are called conjitgaU foci. Light radiating from either converges to the other. 376. Conjugate Foci on the Principal Axis. — Real Foci. — As the luminous point 6>(Fig. 214) is moved from the lens along the principal axis, the incident cone of light becomes less divergent and the refracted cone more convergent ; the image therefore moves toward the lens along the axis. When the distance of the object is relatively great (not less than one hundred times the radius of curvature of the surfaces of the lens), the incident light is sensibly parallel, and the point to which the refracted light con- Lenses 299 verges is called the principal focus of the lens {F, Fig. 216). There is another principal focus at the same distance on the other side of the lens, correspond- ing to an incident beam coming from the opposite direction. Since light can *u *u • F'G. 216. traverse the same path m both directions, it follows that light radiating from a luminous point at either principal focus is refracted as a beam parallel to the principal axis. The distance of the principal focus from the lens is called the focal length of the lens. The focal length depends upon the refractive power of the glass of which the lens is made, as well as upon the curvature of its faces. It can be shown that, when the faces have equal curvature and the index of refraction of the glass is 1.5, the focal length is equal to the radius of curvature. When the index of refraction exceeds 1.5, the focal length is less than the radius of curvature. As the luminous point is moved toward the principal focus from a greater distance, the incident light becomes more and more diver- gent and the refracted light less convergent : the image, therefore, recedes along the axis. When the object is at the principal focus, the light is refracted as a parallel beam, as stated above, and the image is indefinitely far away. Virtual Foci, — When the object is nearer than the principal focus, the divergence of the incident light is greater than the lens can overcome, and the refracted light is still divergent, ,^^ ^arx>--------- | ^-p-| «^ though less so than the inci- ^ '""'"'-^^^^^^^^^ dent light (Fig. 217). The image (or focus) is therefore * ^^^' virtual and at a greater dis- tance than the object. As the object is moved up to the lens from the principal focus, the image approaches the lens from an indefinite distance on the same side. 300 Light 377. Conjugate Foci on Secondary Axes. — When a ray of light passes obliquely through the center of a double-convex lens, the tangent planes at the points of entrance and emergence of the ray (A and B, Fig. 218) ^ are parallel. The emer- gent ray lU is therefore parallel to the incident rays OA (Art. 365). When the lens is thin and the angle of incidence small, as is gen- erally the case, the lateral displacement of the refracted ray is very slight and may be disregarded. Any ray through the center of the lens, as OABI, is therefore regarded as a straight line, and is so drawn in diagrams. Any straight line through the center of a lens is called a second- ary axis. It follows from the above that the conjugate focus of any point not on the principal axis lies on the secondary axis through that point. Conjugate foci on secondary axes are real or virtual under the same conditions as for foci on the principal axis ; i.e. if the distance of a point is greater than the focal length of the lens, the conjugate focus is real ; if less, it is virtual. Laboratory Exercise 55. 378. Real Images. — When light falls upon a convex lens from an object situated beyond the principal focus, the diverging cone of light from each point of the object converges to the conjugate focus, and there forms the corresponding point of the image, which in this case is real. The image can be caught upon a screen, and can also be viewed directly from any point in the path of the light diverging from it. Thus, in Fig. 214, the image can be seen in mid-air from any point within the cone PIQ. There are three rays from any point not on the principal axis whose directions after passing through a lens are known : (i) The ray through the center of the lens continues in the same straight line. (2) The ray parallel to the principal axis is refracted so as to pass through the principal focus. (3) The ray through the principal focus (on the same side as the object) is refracted parallel Lenses 301 Fig. 219. to the principal axis. These three rays are shown in Fig. 218. In drawing figures, the conjugate focus of any point can be deter- mined by means of any two of these rays, when the focal length is known, without constructing angles of incidence and refraction. Figures 219, 220, and 221 illustrate this method of construction. In Fig. 219, AB may be regarded as the object and ab its image, or vice versa. Since any point of the object and a - ^ — ^ A-<^ b^ its image are on the same straight line through the center of the lens, the image, if real, is always inverted. Triangles AOB and aOl> are similar; hence the lengths (and other similar dimensions) of object and image are proportional to their distances from the lens. The following consequences of these geometrical relations are of great importance in optical instruments : — (i) When the distance of the object is so great that the rays from any point of it are sensibly parallel, the real and inverted image which is obtained of it is at the principal focus and is relatively very small (Fig. 220). (2) When the object is at a distance only slightly greater than the focal length, its image is relatively distant and greatly enlarged or magnified. (Draw figure.) (3) For a given object at a given distance, the size of the real image increases with the focal length of the lens ; since, under these conditions, the greater the focal length, the greater is the distance of the image from the lens {Exp.). (Illustrate with two drawings, taking lenses of unequal focal length.) (4) When the object is at a relatively great distance (Fig. 220), the length of the image is proportional to the focal length of the lens. (Draw figures to illustrate.) Fig. 220. -^^ 302 v,o- X Light '--IM" 379. Virtual Images. — When the distance of the object from the lens is less than the focal length, the light from each point of the object is still divergent after refraction ; and its apparent source is the corresponding point of the image, which in this case is virtual. A virtual image can be seen only by looking through the lens toward the object. What we really see through the lens is not the " magnified object," but its magnified virtual image. Figure 221 illustrates the formation of a virtual image, following „ the usual construction. It will be seen from the figure that ^"^irr ^-^^.A ^^ the virtual image is ahvays *p!^ erect and magnified, and is at a greater distance than the ob- :: ^.s--- ject. A similar figure in which *" ^^' the object is taken nearer the lens will show that, as the object approaches the lens from the principal focus, the image also approaches the lens and grows smaller. (Draw the figure.) From the similar triangles A OB and aOb it is evident that the lengths of object and image are proportional to their distances from the lens, as in the case of real images. The less the focal length of the lens, the larger is the virtual image when formed at a given distance from the lens. (Draw figure to illustrate.) A convex lens, when used for observing the enlarged virtual images of minute objects, is called a magnifying glass or simple microscope. 380. Formulas Relating to Convex Lenses. — Formula for Real Images. — In Fig. 222 the rays AM and BN are ' " ^- — /IT""^^ ^^^^ drawn as if they were re- fracted once midway between the surfaces of the lens in- stead of at each surface. This simplifies the present problem, and involves no appreciable error. Lenses 303 From the similar triangles A OB and a Ob, AB'.ahw CO: Oc. From the similar triangles MFN and aFb, MN'.ab-.'.OF'.Fc, Since AB = MN^ we have from these proportions, CO'.Oc'.'.OF'.Fc, Let CO = D (the distance of the object), Oc = d (the distance of the image), and OF=f (the focal length of the lens). Sub- stituting these values in the last proportion, we have D:d::f:{d-f). From which df^D{d-f), Transposing and combining, /(// + Z>)= Dd, Dividing by /?./5^, . ^^ = 7- JJa J Separating the terms of the fraction and reducing, -1 + 1 = 1. D^ d f ■f By means of this formula any one of the three quantities Z>, d^ and / can be found when the other two are given. Formula for Virtual Images. — From the similar triangles fZil/^ and aFO (Fig. 223), aA\aO:\MA\FO. From the similar triangles OAC ".nd Oac, aA'.aOwcC'.cO. Hence, cC.cOw MA : FO. I^t OC=D{=MA), Oc = d, d.n^.FO=f (the focal length of the lens). Substituting these values in the last proportion, we have (d-D):d:'.D:/, d-D D ->:^-~^. Fig. 223. 304 Light Dividing by D, tf-D I or I I _ I Laboratory Exercise j6 PROBLEMS The following problems will help to familiarize the pupil with a number of facts which will be of assistance in the study of optical instruments. The problems are to be solved by means of the formulas. 1. The distance of the image is how many times the focal length when the distance of the object is (- ject is equal to the focal length when the distance of the image is 10 in. and the focal length of the lens (. in a direction parallel to the slit). These lines are called Fraunho/er's iines^ after the celebrated optician of Munich, who first studied and gave a detailed descrip- tion of them. They represent missing images of the s/it, and indicate that light of certain colors is absent from sunlight. When the width of the slit is only very slightly increased, the overlapping of the images on each side of the dark lines obliterates them. 403. Virtual Spectrum. — If the preceding experiments cannot be performed for want of a dark room or a porte lumiere for directing a beam of sunlight into the room, the observation of a virtual spectrum will serve as a substitute. The experiment consists in looking through a prism at a slit about a millimeter wide in a piece of black cardboard. The cardboard should be held up at arm*s length before a window, with the sky for a background and with the slit horizontal. The prism is held close to the eyes, with its edges parallel to the slit. If the refracting edge of the prism 1 It b only the light from the same portion of the sun's disk that is parallel. The rays in a sunbeam that come from opposite sides of the sun are at an angle of about half a degree {AOB, Fig. 245). The lens, in the position described, brings all the light that passes through any point of the slit to the same point of the image, and hence forms an image of the slit. Dispersion and Color 325 ^ ^;:- Fig. 246. is on the lower side, the cardboard will appear at an angle of about 40° below its true position (Fig. 246) ; and the observer, looking obliquely downward at this angle, will see a virtual spectrum consisting of a series of over- lapping colored images of the slit. Since the violet light is refracted the most, the vio- let image of the slit will be the lowest (see figure). Laboratory Exercise 58, 404. The Nature of Color. — When any part of the light com- posing a spectrum is allowed to pass through a second prism, it is again refracted, but its color remains unchanged (Fig. 247). The colors of the spec- ^ trum are simple or elementary; that is, they cannot be fur- ther decomposed {Exp.). It is found by ex- periment ^ that the wave lengths of the colors of the spectrum increase regularly from the violet to the red ; and that the same elementary tolor always has the same wave length (in the same medium) whether its source is the sun or any other luminous body. It follows that the physical cause of the sensation of color is nothing else than the wave length of the light ; in other words, the sensation produced by an elementary color is determined by its frequency {i.e. the number of waves that pass any point in a second), just as the pitch of a sound is determined by the vibration number of the sounding body or the frequency of the sound waves. As the temperature of a body rises, the vibration of its mole- cules becomes more and more rapid, and shorter waves are set up in the ether. At about 525° C. (Art. 331) some of the molecules 1 It is beyond the scope of elementary physics to discuss the methods by which the wave lengths of light are measured. Fig. 247. 326 Light vibrate with sufficient rapidity to give out red light. As the tem- perature continues to rise, additional colors are given out in order from red to violet, and the color of the body changes from red through orange and yellow to white. " That which we call white light is, in the state in which we receive it from such a body as a white-hot bar of iron, or perhaps in its purest form from the crater of the positive pole of the electric arc, a mixture of long and short waves ; waves of all periods within the range of visibility are either continuously present or, if absent for a time, are absent in such feeble proportions or for such short intervals that they are not appreciably missed by the eye. White light of this kind is comparable to an utterly discord- ant chaos of sound of every audible pitch ; such a noise would produce no distinct impression of pitch ; and so white light is uncolored." — Daniell's Principles of Physics. 405. The Invisible Spectrum. — The luminous ether waves vary in length from .0000767 cm. for the extreme red to .0000397 cm. for the extreme violet. The interval between these extremes, expressed as in music, is somewhat less than one octave. Thus we see that the range of sensibility of the eye is much less than that of the ear (Art. 304). That there are many octaves of non- luminous ether waves extending both above and below the visible portion of the spectrum is proved by their chemical, heating, and electrical effects. 406. Cause of Dispersion. — \Vhenever light is refracted, the elementary colors of which it is composed are refracted unequally, although in many cases the dispersion is not sufficient to be noticeable. This unequal deviation indicates that the index of refraction of a substance varies with the color of the incident light; and, since the index of refraction is the ratio of the velocity of light in a vacuum to its velocity in the substance (Art. 363), it is evident that lights of different colors {or ether waves of different lengths^ travel with unequal velocities in the same substance. This, therefore, is the cause of dispersion. With few exceptions, the deviation increases continuously from Dispersion and Color 327 the red to the violet, as in the preceding experiments, the velocity of the shorter waves being less than that of the longer in most substances. 407. Color of Opaque Bodies. — When a very narrow strip of white paper, pasted on a piece of black cardboard, is viewed through a prism as the slit was in the experiment of Art. 403, the light from it is resolved into a complete spectrum, the colors of which have the same relative intensity as in the spectrum of direct sunlight. Any opaque body which, like the white paper, reflects all the elementary colors of the incident light in equal proportions appears white when white light falls upon it; but when the inci- dent light is colored, the body appears of the same color. Thus when a spectrum is thrown upon a white screen, the part of the surface upon which the red light falls appears red, the part upon which the blue light falls appears blue, etc. ; for each part reflects the color that it receives. When a narrow strip of colored paper is viewed through a prism, the light from it is resolved into an incomplete spectrum ; gener- ally half or more of the spectrum is either wanting or very faint. The spectrum of a blue strip, for example, will probably be found to consist of violet, indigo, blue, and green ; that of a yellow strip, of green, yellow, orange, and some red. A similar analysis of the light from different colored bodies shows that, with few exceptions, the light reflected by them is composite^ i.e. it is composed of a number of elementary colors. Any body that reflects some of the elementary colors of white light in larger proportion than it does others is colored, its color being determined by the combined effect of all the colors that it reflects. A body reflecting no light would be perfectly black. White, black, and the diff"erent shades of gray differ only in brightness ; each reflects the different elemen- tary colors in the same proportions in which it receives them. Color, regarded as a property of opaque bodies, is therefore merely the power of reflecting light of certain wave lengths either exclusively or in larger proportions than others, the light that is not reflected being absorbed. It is further evident that bodies 328 Light have no color of their own. A white body, as stated above, takes the color of the incident light ; a colored body appears of its natu- ral color only when the incident light cqntains all the elementary colors that it is capable of reflecting. This is strikingly illustrated by holding colored papers in different parts of the solar spectrum thrown upon a screen in a darkened room. A piece of green paper, for example, will appear black in the violet, indigo, orange, or red, being incapablfe of reflecting these colors ; in the blue it will probably appear a dark blue, and in the yellow a dirty yellow, due to the reflection of a little of these colors ; in the green it will appear at least very nearly of its natural color {Exp.). This explains why some bodies do not appear of the same color by artificial light as by daylight. Most artificial lights are deficient in violet and blue, and hence are more or less yellowish. In such a light, pale yellow is scarcely distinguishable from white, and blue is often mistaken for green. The greenish appearance of blue is due to the fact that blue pigments reflect violet and green as well as blue light, and green predominates in the light that they reflect when illuminated by light that contains little violet and blue. 408. Color of Transparent Bodies. — A transparent body is colored if it is more transparent to some of the colors of white light than to others, its color being that which results from the J mixture of all the transmitted colors. The remaining colors of the incident light are absorbed on the way through the medium. This action of a colored medium is called selective absorption. If one or more of the elementary colors that a body can transmit are. not present in the incident light, the body will not appear of its natural color ; and if none are present, it will appear opaque, since in this case no light will be transmitted. The light transmitted by a transparent body, as a piece of glass, may be analyzed by observing either its real or virtual spectrum. To obtain the latter, a slit is observed through a prism, as de- scribed in Art. 403, with one end of the slit covered by the trans- parent body. This gives a complete spectrum from the uncovered Dispersion and Color 329 end of the slit, and, beside it, the spectrum of the light transmitted through the body (Lab. Ex.). To obtain the real spectrum, a solar spectrum is projected upon a screen in a darkened room by means of a slit, lens, and prism, as described in Art. 402 ; and the body is held so as to cover either the upper or lower end of the slit. The solar spectrum and the spectrum of the transmitted light will then be projected upon the screen, one above the other, making a comparison of the two very easy. It will be found by either of these methods of observation that the light transmitted by colored bodies is composite and, with few exceptions, gives a considerable portion of the complete spectrum. Blue (cobalt) glass transmits violet, blue, green, and some red ; yellow glass transmits red, orange, yellow, and green ; red (ruby) glass transmits red and a little orange (Exp.). When two transparent bodies of different color are placed before the slit, one in front of the other, the light that passes through both undergoes a double process of selective absorption ; and its spectrum therefore consists only of the color or colors that are common to the light transmitted by the two separately. Thus green is the only one of the colors transmitted by either blue or yellow glass that is also transmitted by the other ; hence the two together appear green. Similarly, the combination of red and blue, red an^ green, or orange and blue glass is very nearly opaque, since no color that they separately transmit in considera* ble quantity is common to both {Exp.). 409. Color of Bodies containing Suspended Particles. — A gas or a liquid which, of itself, is colorless becomes colored when it contains a multitude of minute particles in suspension. An example of this is the sky-blue liquid obtained by adding to water a very small proportion of milk or an alcoholic solution of mastic, or by mixing a few drops of dilute nitrate of silver with a quantity of water in which a little table salt has been dissolved.^ These 1 In this case chloride of silver is formed, which is insoluble in water, but remains suspended in the form of extremely minute solid-^Ef&^e^r=-^K^^same is true of the mastic. jf^^* ^^ Twr 'UNIVERSITY 330 Light liquids appear blue by reflected light ; but are yellow or orange when viewed by transmitted light. This is due to the fact that the suspended particles reflect a considerable part of the violet and blue light, but reflect less and less of the other colors toward the red end of the spectrum. Thus violet and blue predominate in the reflected light, and red, orange, and yellow in the trans- mitted light. The blue color of the sky is similarly explained, " the air being rendered visible against the dark background of black space by sunlight reflected from its fine suspended dust or water particles ; while the light transmitted is always more or less yellowish, and, in the afternoon and evening, when sunlight comes to us through a greater thickness of the more dusty layers, verges toward orange or even red." — r3anieirs PrincipUs of Physics. 410. Mixture of Colors. — The unaided eye is wholly incapable of distinguishing between composite and elementary colored light. The light reflected from a piece of yellow paper or transmitted through yellow glass may produce exactly the same color sensation as the yellow of the spectrum, although it contains all the colors of the spectrum from the red to the green inclusive. Moreover, the sensation of yellow may be caused by light that contains no elementary yellow at all ; in fact, the color sensation caused by any elementary color except violet and red may also be caused by vari- ous combinations of two or more of the other elementary colors in certain proportions.^ In studying mixtures of colored lights, the selected colors of the spectrum are focused by a lens, or reflected by mirrors to the same spot upon a screen, or in some other way are caused to enter the eye in a united beam. Among the results established by such experiments are the following : — I. The mixture of any two elementary colors named in alter- nate spaces in Fig. 248 is like the intermediate one. For example, 1 If the ear were like the eye in this respect, it would be incapable of distinguish- ing the constituents of a complex sound. The notes sounded simultaneously by an orchestra would produce ^e sensation of a single note of average pitch, and harmony and discord would alike be unknown. Dispersion and Color 331 U99Jl'J Fig. 248. Z»^^ the mixture of red and yellow appears to the eye to be identical with elementary orange. The mixture of red and violet light is purple. There is no elementary , . • , r , r Purple purple, as is evident from the fact that this color is not found in the spectrum. 2. Complementary Colors. — The mixture of any pair of opposite col- ors in the figure appears white when the colors are combined in the right proportions. ** Ordinary white light consists of all the colors of the spec- trum combined ; but any one of the elementary colors, from the extreme red to a certain point in yellowish green, can be combined with another elementary color on the other side of green in such proportions as to yield a perfect imitation of ordinary white. The prism would instantly reveal the differences, but to the naked eye all these whites are completely undistinguishable from one another." (Deschanel.) Any two colors which yield white when mixed are called com- plemeniary colors, 3. Primary Colors. — Any color of the spectrum can be pro- duced (so far as the color sensation is concerned) by mixing elementary red, green, and violet lights in proper proportions. Red, green, and violet are therefore called the primary colors. 411. Newton's Disks. — One of the most convenient methods of mixing colors is- by means of colored disks, each of which is slit along a radius, thus permitting any desired amount of overlapping when two or more of the disks are placed together on an axis through their common center (Fig. 249). When the disks are rapidly rotated about the axis, only one color is seen, and this Fig. 249. covers the entire circular area. This results 332 Light from the fact that the sensation of sight continues for a fraction of a second after the light ceases to enter the eye or ceases to fall upon the same part of the retina. The rapid rotation causes the different colors to come from all parts of the surface in such rapid succession that each of them produces a continuous impression ; and the effect is the same as if they came simultaneously from all parts of the surface. , The colors reflected by the disks are, of course, composite; but experiments have shown that a composite color produces the same effect in a mixture as the elementary color that looks like it. Hence the results described in the preceding article can be obtained with the disks. In most cases, however, the total amount of reflected light is so small that the resultant color is very defi- cient in brightness. Complementary colors, for example, generally yield a dark gray instead of white {Exp.). 412. After-images. — If one looks for half a minute or more at a brightly illuminated piece of colored paper on a black back- ground, then at a white surface, an image of the colored paper will appear upon the surface in the complementary color. Thus if the paper is green, the image will appear purple {Exp.). The explanation is that the part of the retina upon which the light from the colored paper falls becomes fatigued for that color, and is less sensitive to it than to the other colors of white light ; hence these other colors produce the stronger impression when white light falls upon that part of the retina, and they together give the complementary color. The image thus produced is called a negative after-image. When the object looked at is very bright, the after-image is u'S\i2\\y positive, that is, of the same color as the object; and this is frequently followed by a negative image. A positive after- image niay be regarded as an extreme instance of the persistance of impressions. After-images of bright objects can often be seen with the eyes tightly closed. Newton is said to have suffered for many years from an after-image of the sun, caused by incautiously looking at it through a telescope. Dispersion and Color -- 333 413. Colors of Mixed Pigments. — We have seen that a mixture of blue and yellow lights (either composite or elementary) is white (Arts. 410 and 411) ; but that when pieces of blue and yellow glass are placed together, they appear green (Art. 408, end). The results are not inconsistent, for they are obtained by wholly differ- ent methods of combination. In the first case the sensation of white is due to the simultaneous action of the two colors upon the retina ; the colors and the sensations that they produce are added. If the colors are complex, as is the case with Newton's disks, they together probably include all the elementary colors. In the sec- ond case, the result is obtained by subtraction^ elementary green being the only color that passes through both pieces of glass in appreciable quantity. The other colors are absorbed, — some by the blue glass, the remainder by the yellow. The mixture of blue and yellow paints or powders is green {Exp.). This is evidently a case of subtraction, like that of the blue and yellow glass. The blue paint (or powder) absorbs the red, orange, and yellow of the incident light, and the yellow paint absorbs the violet, indigo, and blue. Thus green is the only color not strongly absorbed by one or the other, and the mixture is green. It is evident that the results obtained by mixing pigments and by mixing lights of the same color are, in general, very differ- ent. The light reflected by mixed pigments consists of the colors which are not absorbed by either constituent. If the lights reflected by two pigments have no elementary color in common, a mixture of the two will be black or a dark gray. This is the case with vermilion (a bright red) and ultramarine (a deep blue) {Exp.). 414. Chromatic Aberration. — The pupil has very probably observed a fringe of color bordering objects when viewed through a convex lens, and especially when viewed through a pair of lenses, used either as a telescope or a compound microscope. The coloring is due to the unequal refraction of the elementary colors by the lenses. ' ^^°* When white light from any point, O (Fig. 250), falls upon a 334 Light lens, the greater refraction of the violet light brings it to a nearer focus, Vy than that of the red light, r. The foci of the other colors lie between these. When a screen is placed at the focus of the red light, the image is surrounded by a border of violet and blue light ; at the focus of the blue light it is surrounded by red {Exp.), This unequal focusing of the different colors is called chromatic aberration. Since dispersion increases with the deviation, chromatic aberra- tion is much greater for light passing through a lens near its edge than for light passing through its central portion, and is greater the less the focal length of the lens {Exp.). Thus the opaque diaphragm with a small circular opening, which is placed in front of the lens in cameras and other optical instruments, serves the double purpose of diminishing both the spherical and the chro- matic aberration. But the diaphragm only partially overcomes the defect, and besides has the disadvantage of cutting off the greater part of the light. During the seventeenth century the remedy employed in the construction of telescopes was the use of object glasses of great focal length — in some cases exceeding lOo feet. The object glass in such cases was mounted at the top of a high pole, and the eyepiece was on a separate stand below. 415. Achromatic Lenses. — About 150 years after the telescope and the microscope were invented, it was discovered that chro- matic aberration could be almost perfectly corrected by combining a convex lens of crown glass with a concave lens of flint glass (Fig. 251). This depends upon the fact that, while the refracting power of flint glass is only slightly greater than that of crown glass, its dispersive power is nearly twice as great, the spectrum formed by a prism of flint Fig. 251. glass being nearly twice as long as that formed by a prism of crown glass having an equal refracting angle {Exp.). Hence a double lens, consisting of a convex lens of crown glass and a concave lens of flint glass of nearly twice the focal length, produces convergence of the light without dispersion ; for the dis- persion due to the concave lens is equal and opposite to that Dispersion and Color 335 of the convex lens, and it neutralizes only half of the converg- ence caused by the latter (Fig. 252). The objectives of tele- scopes, opera glasses, and microscopes (except the cheapest) are achromatic. 416. The Rainbow. — Rainbows are due to the dispersion of sunHght by raindrops, and by the drops of water in the spray of fountains, waterfalls, etc. Sometimes one fc c Fig. 25a. bow is seen, sometimes two, each consist- ing of the colors of the solar spectrum. They are always arcs of circles, and, when two are seen, they are concentric. The ~ inner or lower one is always much the _ brighter and is called the primary' bow. In it the red is on the outside, the violet on the inside. In the outer, or secondary bowy the colors occur in the reverse order (Fig. 253). The rainbow is always seen in the direction opposite to the sun, — the sun, the observer, and the center of curvature of the bow being in the same straight line, EO. This line is called the axis of the bow. The formation of the rainbow can be experimentally illustrated in a dark- ened room by means of a globe (a round-bottomed flask) filled with water. It will be found that the results obtained , .., when a slender beam of sunlight is ^ «o-«HM ^^^"^ I ', \ caused to fall upon the globe depend upon the angle at which the beam meets its surface. At a certain angle a curved spectrum is formed and may be caught upon a screen ; at another angle the spectrum reappears with the colors in the reverse order. At angles other than these the light is too widely scattered on leaving the globe to produce visible effects. If a beam large enough to cover the globe is used, one, and possibly both, of the spectra will appear as complete circles {Exp.) . 336 Light 42 Fig. 254. The dispersion caused by a single drop of water is like that obtained with the globe in the above experiment, except that the total amount of reflected light is correspondingly less. Each drop forms two complete spectra ; but the eye receives only a slender ray of one color from any one drop, and the bow that is seen is made up of light from a multitude of drops. 417. The Primary Bow. — Figure 254 represents a ray of light entering a drop at the angle required for the primary bow. The unequal refraction of the colors at A 'X causes dispersion, forming a spec- trum, ^ y, at the back of the drop. Here the greater part of the light is refracted out (not shown in the figure) ; the remainder is reflected to /i'y, where the greater part of it is refracted out with further dis- persion. The red and the violet rays make angles of about 42** and 40°, respectively, with the inci- dent ray SA. The reason for the order of the colors in the primary bow will be evident from a comparison of this figure with the preceding one. The eye receives the same color fi-om all drops at the same angular distance from the axis of the bow ; hence the bow is circular. At sunrise or sunset the rainbow, if complete, appears as a semi- circle, its axis, £0(Fig. 253), being horizontal. Since the center of the bow is always at the same angle be- low the horizon that the sun is above it, the higher the sun is, the shorter will be the arc of the bow. When the sun is more than 42° above the horizon, the primary bow is wholly below it, and is therefore invisible. 418. The Secondary Bow. — The ^' ^''' '^* secondary bow is formed by light that has undergone two reflec- Dispersion and Color 337 tions, as shown in Fig. 255. On leaving the drop, the red ray makes an angle of about 51°, and the violet ray an angle of 54°, with the incident ray. A comparison of Figs. 255 and 253 will show why the secondary bow. is above the primary, and why the order of the colors is reversed. The faintness of the secondary bow is due to the additional loss of light at the second reflection. 419. Color by Interference. — When two pieces of plate glass are pressed firmly together in the fingers or in a clamp, curved bands of spectrum colors appear, surrounding the point where contact is closest. The colors are brightest when the plates are looked at from the more strongly illuminated side {Exp.). In Fig. 256, MM' and NN' represent sections of the glass plates, the distance between them being greatly exaggerated. Light incident along the path AB is par- tially reflected at C from the lower sur- face of the upper plate, and also at E from the upper surface of the lower plate. Some of the light reflected at E is transmitted through the upper plate parallel to and nearly coincident with the light reflected from C. But, in twice crossing the space ^^^' ^^^' between the plates^ the waves reflected at E fall behind those reflected at C; and the waves of some one of the elementary colors in these two sets of reflected waves meet in opposite phase, causing interference as in the case of sound waves (Art. 2C)8), and that color is weakened or destroyed. The reflected light is com- plementary to the light cut out by interference, and this differs at different places, depending upon the distance between the plates. Patches and bands of rainbow colors are similarly produced by the interference of light reflected from the two surfaces of a very thin film of any transparent substance, as a soap film or a film of oil floating on water. In the above experiment the layer of air between the glass plates acts as a thin film. Bodies whose colors are due to the interference of the light reflected from them are called iridescent. 338 Light The iridescence of some bodies is caused by interference of the light reflected from minute parallel grooves and ridges (striations) covering their surfaces, as in mother-of-pearl and the plumage of many birds. The colors of an iridescent surface change with the angle of incidence of the light, producing the beautiful effect known as a ** play of colors." The interference of light is the strongest evidence in support of the wave theory. PROBLEMS 1. \Miat is the function of the lens in producing a pure spectrum? 2. Why is it not possible to correct the chromatic aberration of a lens by any change in the form of its surfaces? 3. (. north-seeking pole) and the other end the south poh {Exp,). 422. The Bfagnetic Needle. — A slender magnet suspended at its center by an untwisted fiber or balanced on a pivot (Fig. 258) is called a magnetic needle. After any displacement, a mag- netic needle always returns to *°* ^^ * one definite direction, which is the direction of the magnetic meridian at that place. 423. The Mutual Action of Ifagnets. — Any force exerted be- tween two magnets is most readily detected when one or both are free to turn about an axis under the action of the force. Thus when either pole of a bar magnet is brought up to the like pole of a magnetic needle, the latter turns away from the magnet, show- ing repulsion ; but the unlike pole turns toward the magnet, show- ing attraction (Exp.). When the experiment is performed with two needles, both will turn, showing that the attractions and repul- sions are mutual. The law of equal action and reaction (third law of motion) holds for magnetic forces as for all others. The mutual action of magnets is expressed by the law : Like poles repel and unlike poles attract each other. 424. The Effect of Distance on Bfagnetic Action. — The force exerted by a pole of a magnet increases as the distance from the pole decreases. This is shown by the fact that the nearer an end of a bar magnet is brought to a magnetic needle, the more rapidly will the unlike pole of the needle swing round and vibrate before it ITie exact relation between the force and the distance varies Properties of Magnets 341 considerably under different conditions ; but the force is approxi- mately inversely proportional to the square of the distance except for very short distances. This accounts for the fact that, when the nearer poles of two magnets are unlike, the magnets tend to come together ; for the attraction exerted upon the nearer pole of either exceeds the repulsjon exerted upon its farther pole, giving a resultant force which acts toward the other magnet. Similarly, when the nearer poles are like, the resultant force upon each magnet tends to move it from the other. 425. Magnetic and Nonmagnetic Substances. — Substances that are attracted by a magnet are called magnetic substances ; those that are not attracted are called nonmagnetic. The only substances that are sufficiently magnetic to be attracted by mag- nets of ordinary strength are iron, steel (a form of iron), some compounds of iron, including magnetic iron ore, nickel, and cobalt. All other substances are practically nonmagnetic ; although, under the action of a powerful electro-magnet (Art. 457), all or nearly all exhibit either weak attraction or repulsion. Nickel and cobalt are less magnetic than iron. Iron in its different forms, such as cast iron, wrought iron, and steel, is the only substance whose magnetic properties are of any importance. These properties are usefully applied in the telegraph, the tele- phone, the dynamo, the motor, and many other electrical machines and instruments. 426. Magmetic Action through Bodies. — The action of a mag- net upon any magnetic body is not affected by placing a non- magnetic body between them ; but is affected in a marked degree by interposing another magnetic body. For example, a magnet attracts or repels a magnetic needle through a board, a book, or a plate of glass just as if nothing intervened ; but, when a sheet of iron is placed between them, the needle is only slightly affected by the presence of the magnet, if at all. The sheet of iron, espe- cially if large, serves as a screen to cut off magnetic action from the side opposite the magnet. This is explained in the next article. 342 Magnetism n. Kagnetization Laboratory Exfrcise 64. 427. Bfagnetic Induction ; Penneability. — When either pole of a magnet is held against or very near an end of a soft iron rod, the other end of the rod attracts iron filings in considerable quan- tity, and attracts or repels the poles of a magnetic needle as the nearer pole of the magnet would do. Thus with the north pole against the rod (Fig. 259), the farther end of the rod repels the north pole of the needle. The rod, in fact, senies as a carrier for the magnetic action of the magnet^ and is itself a magnet while doing so, having poles as shown in the figure. Only magnetic substances can thus modify and extend the action of a magnet, and the property thus exhibited is called magnetic permeability. We can now understand how a sheet of iron serves as a magnetic screen. By itself becoming magnetized, it turns aside the mag- netic action to its edges, which afe capable of exerting attractions and repulsions (Exp.). The iron rod in the above experiment is said to be magnetized by induction. Magnetic induction always takes place when a ^_ — ' magnet is brought near a magnetic •*? -v body. The body is then attracted Fig. 259. because its nearer pole is unlike the nearer pole of the magnet (Fig. 259). Thus induction always precedes attraction and is the cause of it. 428. Temporary and Permanent Kagnets. — When soft or wrought iron, hard iron, untempered steel, and tempered steel are subjected to equal inductive action, as by bringing them suc- cessively in contact with the same magnet, a simple test with iron filings will show that the soft iron becomes most strongly mag- netized and the tempered steel the least. On the other hand, the soft iron loses its magnetization, completely or nearly so, as soon as it is removed from the influence of the magnet, while the tem- pered steel retains all or nearly all of the magnetization induced in it. Thus by magnetic induction a piece of soft iron may be Magnetization 343 made a temporary magnet and a piecfe of tempered steel a perma- 7ient one. Hard iron and untempered steel retain a considerable part of induced magnetization ; they are subpermafient. All manufactured magnets are pieces of highly tempered steel that have been magnetized by induction. They may be demag- netized or even magnetized with opposite polarity at any time by sufficiently strong inductive action in the opposite direction. 429. Experimental Evidence on the Nature of Magnetization. — There is much experimental evidence indicating that the magneti- zation of a body is definitely related to its molecular condition. The following are some of the facts that point most strongly to this conclusion : — Properties of a Broken Magnet. — When a magnet is broken into any number of parts, each piece is a complete magnet having the same polarity and approximately the same strength as the original mag- net (Fig. 260). This can be readily shown by breaking a magnetized sewing or knitting needle {Exp,). Such experiments show that every part of a magnet is mag- netized ; in fact, the neutral portion in the middle is generally more strongly magnetized than the ends. The absence of attract- ive power in the middle may be accounted for by regarding the two halves of a magnet ^ ^-^ as complete magnets with their unlike poles joined at the center. These equal unlike poles, situated at the same point, exactly neutralize each other's action upon surrounding bodies. A magnet may be regarded as composed of an in- definite number of little magnets, with all their like poles pointing in the same direction (Fig. 261). !„i;i;i;li;:ii:;^J Fig. 260. ^1 M— » If- —9 n s 7f- ■ 8 n « n 8 n 9 n 8 n 8 n 8 n s n 8 n 8 n 8 n 8 n 8 n S n 8 n 8 n 8 n 8 n 8 n 8 n 3 n H n S n -2 n 8 2- -2 n 8 n 8 7l -J» N Fig. 261. 344 Magnetism Effect of Heat on Magnetization, — The strength of a magnet is always diminished by heating it. This effect is only temporary for moderate degrees of heat ; but a bright red heat causes permanent demagnetization {Ex/>,), This effect of heat suggests that magnetization depends upon or consists in a certain molecular condition which is destroyed by the violent motion of the molecules at a high temperature. Effect of Mechanical Disturbance. — A magnet is weakened by hitting it a number of sharp blows, and a magnetized knitting needle by clamping it in a vise and causing it to vibrate vigorously (Exp.). A magnetized piece of iron wire a foot or so in length is almost completely demagnetized by twisting it once or twice each way. (A small portion at each end may be bent at right angles to the length for convenience in twisting.) {Exp.) In such cases a loss of magnetization results from the disturbance of the molecular condition of the magnet by mechanical forces. On the other hand, such disturbances assist magnetic forces in producing magnetization. Thus a number of blows upon a piece of iron when it is near a magnet will cause it to become more strongly magnetized. 430. Theory of Magnetization. — These facts and others of a similar nature have led to the theory that every molecule of a magnetic substance is a permanent magnet ; and that in an unmag- netized body the poles of these molecular magnets point indis- criminately in all directions (Fig. 262), while in a magnetized body the greater number of the mole- r^^^^M^^M^i^ !?,« ^.^ ...^ , cules lie with their Fia a63. (IG. 263. like poles pointing in the same direction (Fig. 263). According to this theory, the act of magnetizing consists in turning the molecules more or less completely into one particular direction. If all the mole- cules were turned in the same direction, the limit of possible magnetization would be reached. Soft iron is more readily magnetized than steel, because its molecules are more easily turned The Magnetic Field . 345 about, and it loses its magnetization more readily for the same reason. This theory may be illustrated by means of a test tube nearly full of steel filings, each particle of which plays the part of a molecule on a greatly magnified scale. When the mass of filings is magnetized, it exhibits polarity and acts as a magnet until shaken up (Lab. Ex.). What constitutes the magnetism of the molecule is not known. III. The Magnetic Field 431. Magnetic Field and Lines of Force. — A magnetic field is any space within which magnetic forces act. The intensity of these forces is often referred to as the intensity of the tnagnetic field. The field of a magnet is most intense near the poles, and decreases rapidly with increasing distance. It really extends indefinitely in every direction ; but at a comparatively short dis- tance it becomes too weak to produce sensible effects. When a magnetic needle is placed within the field of a magnet, as at O (Fig. 264), its north pole is attracted by the south pole of the magnet and repelled by the north pole. OB represents the attraction and OA the re- pulsion upon the north pole of the needle when at 0\ and OR their resultant (by the parallelo- gram of forces). Hence the needle behaves as if its north pole were acted upon by a single ' pj^^ , ' force in the direction of OR, The component and resultant forces upon the south pole of the needle, when at O^ are respectively equal in magnitude and opposite in direction to those upon the north pole ; hence a short needle placed with its center at O would come to rest with its north pole pointing in the direction OR. If the needle is moved constantly in the direction in which its north pole points, it will trace the curved path OCS, the direction 346 Magnetism of which at any point is the direction of the resultant magnetic force at that point. Such a line in a magnetic field is called a line of force. Since the resultant forces upon a north and a south pole are in opposite directions along a line of force, we avoid ambiguity by defining the direction of a line of force as the direction of the force acting upon a north pole. In accordance with this defini- tion, the lines of force in the field of a magnet are said to extend fix)m its north to its south pole (not from the south to the north pole). In diagrams the direction of a line of force is often indi- cated by an arrowhead placed on the line. Laboratory Exercise dj, 432. Lines of Force in Certain Magnetic Fields. — The direction of the lines of force in different parts of a magnetic field can be determined by merely observing the direction in which the north pole of a magnetic needle points when moved about in the field ; but fine iron filings may be made to serve the same pur- pose for the whole of a plane section of a field at one time. The filings are sprinkled from a pepper box or other sifter upon a sheet of cardboard or stiff paper placed over the magnet. * A light tapping on the cardboard assists the magnetic forces in bringing the filings into definite lines coinciding with lines of force. The lines thus obtained about . \ j //v'""^"^Vv • A'V a bar magnet are shown in • \\\\' . l /v; ^rr:::- ^> '.'■'»!/'/// ^ «=» — >^r- — > — 15>»» — -> f Fig. 265. Beyond a distance ,y;, ' j ; \\.'^ :~~".-s^ y/i]\ v^\ .of a few inches the field is 'V i \ 'v^srrirl'Cr' V i \ X'* too weak to direct the filings ; ^ hence the information that ^'^* ^^' they afford is incomplete. All the lines of force extending from the north pole are really continuous with lines of force coming to the south pole (when no other magnet is in the vicinity). N TTT /// The Magnetic Field 347 When the north pole of one magnet is placed near the south pole of another, the filings are arranged in lines as shown in Fig. 266. The lines of force extend across between the i\^ unlike poles of the two mag- \ \^ ^ . \ > / ' / , / i nets. But when the like poles \ ^. \ \ "'i \ / >^ / / / ' of two magnets are turned i i \ '. . .' . . • . toward each other (Fig. 267), * no lines are found to extend from one to the other ; on the con- trary, the lines in one field turn away from those of the other. 433. Theory of Magnetic Action. — Magnetic action takes place at a distance apparently without the aid of any medium by means of which the force is exerted upon the distant body. In this respect it is like gravitation ; and, like gravitation, it takes place in a vacuum. But as action at a distance without an intervening medium for its transmission is not considered possible (Art. 129), it is assumed that a medium exists by means of which magnetic forces are exerted, and this medium is thought to be no other than the ether that pervades all space. According to this view, the ether surrounding a magnet is under certain stresses (Art. 206) due in some way to the presence of the magnet; and the laws of magnetic action indicate that these stresses consist of a tension along the lines of force and a pressure across them. Thus we have a mental picture of an elastic sub- stance which is in a state of tension between unlike poles, tending to draw them together by contraction along the lines of force, and in a state of compression between like poles, tending to push them apart by expansion at right angles to the lines of force. PROBLEMS I, (a) When a pole of a strong magnet is brought toward the like pole of a magnetic needle, repulsion may be followed by attraction as the magnet is brought closer. Explain. {U) The same may happen when an end of a weakly magnetized piece of iron is brought toward a needle. Explain. 348 Magnetism 2. Why should decision as to the polarity of a magnetized body be based on repulsion of the magnetic needle rather than on attraction ? 3. In what different ways may an unmagnetized magnetic substance be dbtinguished from a magnet ? 4. Explain the effect of the soft iron bar, called the armature or keeper, which is placed across the ends of a horseshoe magnet, when not in use, to preserve the strength of the magnet. 5. In what respects does magnetic action resemble gravitation ? In what respects docs it differ ? IV. Terrestrial Magnetism 434. The Earth's Magnetic Field. — Everywhere upon the earth's surface the magnetic needle, when removed from all mag- netic substances, always comes to rest in a definite direction, clearly indicating that it is controlled by a magnetic field. This is the magnetic field of the earth. It varies largely in intensity and in the direction of its lines of force over different portions of the earth's surface ; but the changes are so gradual that the lines of force are sensibly straight and parallel, and the intensity constant over areas many miles in extent. In general, the lines of force extend in a direction several degrees either to the east or west of north, and are more or less inclined to the horizontal. The magnetic field of the earth indicates that the earth is an irregularly magnetized body. The cause of its magnetization is not known. 435. Action of the Earth's Field on a Compass Needle. — How- 4Aaa*aaaa*4**a»*4 ever much or little the lines offeree of I the earth's field may be inclined, it is I only the horizontal component of the I magnetic force that exerts a directive j action upon magnets that are free to turn only in a horizontal plane. Hence the Fig. 268. directive action upon compass needles is the same as it would be if the lines of force were horizontal, as represented in Fig. 268. The horizontal forces exerted upon the two poles of a compass Terrestrial Magnetism 349 needle by the earth's magnetic field are equal and opposite, since the field is of uniform intensity and the lines of force are straight. Hence when the needle is not parallel to these forces, they act as a couple to swing the needle into Hne with them (A and B, Fig. 268) ; and the needle is brought to rest in this position by friction after a number of vibrations. 436. Magnetic Meridians and Declination. — A line extending over the earth and having at every point the direction of the com- pass needle is called a magnetic meridian. In Fig. 269 the somewhat irregular heavy lines represent magnetic meridians. The magnetic meridian at any place is sometimes called the mag- netic north-and-south line ; and the angle that it makes with the true north-and-south line is called the magnetic declina- tion or simply the decHnation at the place considered. The curved Hues in Fig. 270 are so drawn that each passes through all points having the same declination. Such lines are called isogenic lines, or lines of equal declination. The arrows in the figure show the direction of the declination, whether east or west. Magnetic declination is subject to a number of variations, only one of which exceeds a small fraction of a degree. This variation consists in a continuous change in declination in one direction for about two hundred years, followed by a like change in the oppo- 350 Magnetism Fig, aTa site direction. Recorded observations show that such changes have amounted to over 35° in certain localities. 437. Inclination or Dip; Magnetic Poles of the Earth. — A magnetic needle mounted on a horizontal axis through its center of gravity is called a dipping needle (Fig. 271). If a dipping needle were unmag- netized, it would be in neutral equilibrium in any position in th6 vertical plane in which it is free to turn ; hence its position in the vertical plane is controlled only by magnetic forces, as is the position of the compass needle in a horizontal plane. Consequently, I- 10. 271. when the axis of a dipping needle is placed at right angles to the magnetic meridian, the needle comes to rest in the direction of the lines of force of the earth's field. The angle between the direction of the dipping needle and the horizontal is called the inclination or dip. The irregular lines extending across Fig. 272 are lines of equal dip. The line of no Terrestrial Magnetism 351 dip is called the magnetic equator. North of the magnetic equator the north pole of the needle is depressed, and south of it the south pole. Arctic explorers have found a place where the dip is 90° ; this is the north magnetic pole of the earth (so called from* its geo- FlG. 272. graphical position, not from its polarity). It is nearly 1400 miles from the geographical north pole, and is shown in Fig. 269 as the point in the northern hemisphere to which the magnetic meridians converge. The south magnetic pole has never been reached. Strictly speaking, the magnetic poles of the earth are far below the surface. 438. Intensity of the Earth's Field; Inductive Action. — The earth's magnetic field is much too weak to arrange iron filings in lines or to appreciably modify magnetic action within a few cen- timeters of a strong magnet ; but it is everywhere sufficiently intense to control a magnetic needle and to cause considerable magnetization in iron and steel. This inductive action is best shown by means of a long rod of soft iron (Norway iron). When 352 Magnetism such a rod is held so as to point north and south or, better, in the direction of the dipping needle, it will be found to be magnetized with its north pole pointing north. When the rod is reversed, its polarity is also instantly reversed, if the iron is very soft ; other- wise it may be necessary to strike the rod on the end while it is held in position {Exp.). Any mass of iron or steel that remains in one position for a long time becomes magnetized. This is especially true of the rails of a track when extending in a northerly and southerly direction. Natural magnets are very probably due to the earth's induction. 439. Importance of the Earth^s Magnetism. — The importance of the earth's magnetism is due to its directive action on the com- pass needle. This is utilized on land in determining directions in surveying, and on sea in directing the course of vessels. In the use of the compass for either 6f these purposes the declination at the place must be known. At sea this is given by the declina- tion map or chart (Fig. 270) from the known latitude and longi- tude of the vessel. " Neither the inventor of the compass nor the exact time of its invention is known. Guyot de Provins, a French poet of the twelfth century, first mentions the use of the magnet in navigation, though it is probable that the Chinese long before this had used it. The ancient navigators, who were unacquainted with the compass, had only the sun or pole star as a guide, and were accordingly compelled to keep constantly in sight of land for fear of steering in a wrong direction when the sky was clouded." — Ganot's Physics. The earth's magnetic field also plays an essential part in the use of certain instnmients (galvanometers) in electrical measure- ments, as will be seen later. CHAPTER XII ELECTRICITY 440. " Electricity and magnetism are not in themselves forms of energy ; neither are they forms of matter. They may perhaps be provisionally defined as properties or conditions of matter ; but whether this matter be the ordinary matter, or whether it be, on the other hand, that all-pervading ether by which ordinary matter is everywhere surrounded and permeated, is a question which has been under discussion, and which is now held to be settled in favor of the latter view." — Daniell's Principles of Physics, I. The Voltaic CeU 441. Action of Dilute Sulphuric Acid on Zinc and Copper. — When a strip of zinc is placed in dilute sulphuric acid (one part by volume of acid to fifteen or twenty of water), it is acted upon by the acid and is gradually dissolved or eaten away. This action is accompanied by the rapid formation of small bubbles, which adhere to the zinc until detached by the buoyant force of the liquid. The escape of these bubbles at the surface gives the liquid the appearance of boiling (Lab. Ex.). » These effects are the result of chemical action. Sulphuric acid is a compound substance, the constituents of which are hydrogen, sulphur, and oxygen. The action of the acid upon the zinc con- sists in the substitution of zinc for tlie hydrogen of the acid, by which a compound (zinc sulphate) consisting of zinc, sulphur, and oxygen, is formed and the hydrogen of the acid set free. The bubbles observed in the experiment are bubbles of hydrogen ; the zinc sulphate remains in solution in the liquid. ,The union of the zinc and^he acid liberates chemical potential energy, which, 353 354 Electricity under the conditions of the experiment, is transformed into heat, — much as the energy of coal is transformed into heat by union with oxygen in the process of burning. When copper is placed in dilute sulphuric acid, no bubbles are formed and the copper does not waste away however long it may remain in the liquid. There is no appreciable chemical action. 442. The Simple Voltaic Cell. — When a strip of zinc and a strip of copper are in the same vessel of dilute sulphuric acid, but are not in contact, the appear- ance of each strip is the same as if the other were not pres- ent — bubbles, of hydrogen form upon the zinc, but not upon the copper. But on connecting the strips by means of a wire soldered to each (Fig. 273), bubbles form upon the copper as well as upon the zinc. There is still, however, no chemical action upon the copper, as is evident from the fact that the copper does not waste away however long the strips may remain connected. If the wire connecting the strips be turned so as to extend north and south, a compass needle held close to it, either above or below, will be deflected, indicating the existence of a magnetic field about the wire. This magnetic field indicates that something is happening within and about the wire as the result of its connec- tion with the zinc and copper strips in the acid ; and other effects can be produced which prove conclusively that there is a transfer- ence of energy along the wire (either through the wire or through the ether surrounding it) from one of the metal strips to the other. For example, an electric bell may be rung, a telegraph sounder operated, or a piece of platinum wire heated by making proper connections with the wires attached to the strips. These effects and others are attributed to what is known as an Fig. 273. The Voltaic Cell 355 electric current flowing through the wire from the copper strip to the zinc, and through the liquid from the zinc to the copper, making thus a complete circuit. We speak of electricity as if it were a fluid, and think of it as flowing through wires and other conductors in much the same way as water flows through pipes ; but it is not known that anything is actually transferred round an electric circuit except energy (of the kind known as electrical energy), nor is it certain in which direction the transference of this energy takes place. It is assumed, however, that the direction of the current is as stated above. There is always a magnetic field about a conductor carrying a current of electricity ; this is some- times called an electro-magtietic field y because it is due to electricity instead of magnetism. The magnetic fields of electric currents serve as the readiest means of detecting and measuring them, and also give rise to most of the industrial applications of electricity. The vessel of acid, together with the zinc and copper strips, is called a voltaic cell^ in honor of Alessandro Volta^ an Italian physi- cist, who devised this method of producing an electric current in 1800.^ Two or more cells connected together constitute a voltaic or electric battery^. In popular usage, a single cell is commonly called a battery. The copper strip is called \.\\& positive plate, pole, or electrode of the cell, and the zinc strip the negative. In diagrams the signs -f and — are often used to indicate the positive and negative plates respectively. Laboratory Exercise 66. 443. Cause of the Current ; Potential and Electro-motive Force. — In a voltaic cell such as we have described, the energy of the current is derived from the chemical action of sulphuric acid on zinc. How this chemical action causes an electric current is a theoretical question that can hardly be discussed with profit in an elementary course. It should be remembered, however, that while the cell is in action, one of the constituents of sulphuric acid (hydrogen) goes to 'the copper plate, where it accumulates as 1 The Xerm galvanic is sometimes used instead of voltaic; it is derived from the name of Galvani, an Italian physician, who discovered current electricity in 1786. 356 Electricity bubbles of visible size, and that the other part of the acid, consist- ing of sulphur and oxygen in chemical union, goes to the zinc plate, with which it immediately unites, forming zinc sulphate. More or less hydrogen is also liberated at the surface of the zinc, depending upon its condition; but this is not essential to the action of the cell and results only in wasted energy (Art. 447). It can be shown experimentally that the zinc and the copper plates differ in respect to a condition known as electrical potential ; and the copper is said to be at a higher potential than the zinc* The difference between the potentials of the plates is the direct cause of the current when the plates are connected by a wire.^ A difference of potential can be maintained between two parts of a circuit by other means than chemical action (by a dynamo, for example) ; but, however this may be brought about, the result is always an electric current from the point at higher to the point at lower potential when the points are connected by any conductor. This behavior of electricity may be compared to the conduction of heat between two points from higher to lower temperature, or to the flow of water in a pipe from a higher to a lower level. The agency that moves electflcity from any point to a point at a lower potential is called electro-motive force (often denoted by E. M. F.). " Just as in water pipes a difference of level produces a pressure y and the pressure produces 2iflow as soon as the tap is turned on, so difference of potential produces electro-motive force ^ and electro-motive force sets up a current as soon as the circuit is completed for the electricity to flow through." Electro-motive force and difference of potential are commonly used as equivalent expres- sions ; we shall have no occasion to distinguish between them. It should be noted that electro- motive force is not a force at all, in the proper sense of the word, since it does not act upon matter, but upon electricity. • 1 When the zinc and copper plates are connected by a wire, there is a continu- ous fall of potential round tlie circuit in the direction of the current (through the liquid from the zinc to the copper plate as well as through the wire), except in passing from the zinc to the liquid and from the liquid to the copper, at each of which places there is an abrupt rise of potentiaL The potential of the zinc is the lowest in the entire circuit The Voltaic Cell 157 444. Conductors and Nonconductors ; Resistance. — All sub- stances offer greater or less opposition to the passage of electricity through them, and the property thus exhibited is called electrical resistance. The resistance of a good conductor is small, that of a poor conductor large. Substances through which electricity is nearly or wholly unable to pass are called nonconductors or insulators. The metals are good conductors compared with other substances, but differ largely among themselves, copper being much the best with the exception of silver. Carbon and dilute acids are the next best conductors, though not nearly so good as metals. The resistance of the liquid in a voltaic cell is often much greater than that of the remainder of the circuit. Silk, india rubber, vulcanite, and glass are some of the best insulators. 445. The Electric Circuit. — A current of electricity requires a complete circuit, i.e. a path that is continuous from any point back to that point again without retracing any portion of it. The circuit may be made up of any number of substances, and these m'ay be of any size or shape. It is only necessary that all parts of the circuit be of materials capable of conducting electricity and that they be placed in close contact. The circuit is said to be closed when it is complete, open or broken when there is a gap at any point. The wire of an electric circuit is either insulated by a non- conducting cover or supported upon insulators (usually of glass) to prevent the escape of the electricity from the path intended for it. For currents of low potential, such as are used in ringing electric bells, a cotton covering affords sufficiently good insula- tion ; for higher potentials the covering is of silk or rubber. In connecting wires for a circuit, the insulation must be removed for a short distance at the ends, and the bare wires fastened together. 446. Materials used in Voltaic Cells. — An electric current may be obtained with various dilute acids and solutions of different silts, and the plates may be made of any two metals that are unequally acted upon by the liquid. The greater the difference 358 Electricity in the chemical action upon the plates, the greater will be their difference of potential, and hence also the greater will be the current. The best results are therefore obtained when the nega- tive plate is made of zinc and the positive plate of copper or carbon ; for zinc is most readily acted upon by the acids and solutions used in different cells, and copper and carbon are not acted uf)on at all. 447. Local Action upon the Negative Plate. — We have seen that some hydrogen is liberated at the zinc plate when a simple voltaic cell is in action (Art. 443, first paragraph). This is due to the presence of small particles of iron, carbon, or other impuri- ties in commercial zinc. Any such particle on the surface of the zinc and in contact with the liquid acts as a positive pole and forms a minute voltaic cell with the adjacent zinc and liquid. This causes a local or parasitic current at the spot and a continual wasting of the zinc, whether the circuit is open or closed. When the zinc used is chemically pure, this local action ^ as it is called, does not occur. The zinc is consumed only when the circuit is closed, and hydrogen bubbles apj)ear only upon the copper. The same result is obtained with a plate of commercial zinc when amalgamated^ i.e. when covered with a coating of mercury. The mercury dissolves a portion of the zinc, forming a pasty amalgam which covers the surface and keeps the acid from contact with the impurities. As pure zinc is expensive, it is more economical to use plates of commercial zinc and keep them amalgamated. Amalgamation is necessary, however, only in the case of cells in which acids are used, as in the chromic acid cell (Art. 449). 448. Polarization of the Positive Plate. — The current supplied by one or more cells of the type already described rapidly dimin- ishes from the moment the circuit is closed. This may be shown by measuring the current with a galvanometer (a process to be considered later), or by arranging a battery of one or more cells that is just sufficient to ring an electric bell, operate a telegraph sounder, or run a small motor when the circuit is first closed. The Voltaic Cell 359 The current will very quickly become too weak to produce these effects. The power of the battery may be restored by removing the positive plates and wiping them thoroughly or by letting the battery remain idle for some minutes {Exp.). The weakening of the current is due to the accumulation of hydrogen upon the positive plate. A cell that is in this condition is said to be polarized. After the hydrogen has been wiped off or has had time to escape, the current is as strong as at first. Polarization causes a decrease in the current for two reasons. In the first place, hydrogen is a nonconductor, and hence increases the resistance of the cell by cutting off the current from the por- tion of the surface that it covers. In the second place, the hydro- gen tends to reunite with the other constituents of the acid, just as the zinc does, though less strongly ; and hence it sets up an oppos- ing electro-motive force, which tends to send a current in the opposite direction. Polarization is avoided or diminished in vari- ous ways in different forms of cells, some of the most common of which are described in the following articles.^ 449. Chromic Acid or Bichromate Cell. — The zinc plate of this cell (Fig. 274) is attached to a rod, by means of which it can be raised from the liquid when the cell is not in use. The positive pole consists of two plates of carbon — one on each side of the zinc — which are connected to the same binding screw at the top. The liquid is dilute sulphuric acid, containing in solution chromic acid or bi- chromate of potassium or of sodium, which acts as a depolarizer. These substances contain oxygen which they give up readily to hydrogen, forming water. The accumulation of hydrogen upon the carbon plates is thus diminished, but not entirely ^^* ^^ prevented. Polarization diminishes the current by one third or more in a few minutes. 1 These descriptions may be most profitably studied in connection with the use of the cells in the laboratory or the class room. Any or all of them may be passed over for the present. 360 Electricity The electro-motive force of this cell is large compared with that of most cells. Its resistance is small, for the current has only a ver)' short path in the liquid, and the double carbon pole reduces the resistance further by one half. As a result of the high E. M. F. and low resistance, this cell is capable of supplying an exception- ally strong current, and on this account is much used in experi- mental work. The zinc should be kept thoroughly amalgamated : it must be raised from the liquid when not in use^ for it is attacked by the solution even when the circuit is open. 450. The Leclanch^ Cell. — The zinc of this cell is usually in the form of a rod (Fig. 275) ; the positive plate is a block of carbon. The latter is inclosed in a cylindrical cup of porous earthenware, and is surrounded by small fragments of carbon and man- ganese dioxide, with which the cup is filled. The liquid is a solution of am- monium chloride (sal ammoniac) in water. The zinc is not acted upon when the cir- cuit is open, and does not require amal- gamation. When the circuit is closed, chlorine from the ammonium chloride Fig. 275. unites with the zinc, forming zinc chlo- ride and liberating the other constituents of the ammonium chloride (ammonia and hydrogen). The zinc chloride and the ammonia are held in solution ; the hydrogen passes through the porous cup and unites slowly with oxygen from the manganese dioxide, forming water. This cell polarizes rapidly, and is suitable only for uses requiring brief action with comparatively long intervals of rest, during which it recovers from polarization. It is much used for ringing electric bells, and has the merit of not requiring attention for months at a time. 451. The Gravity Cell. — The positive pole of this cell (Fig. 276) consists of a number of strips of copper fastened together, and is placed at the bottom of the jar. The zinc is near the top, The Voltaic Cell 361 and is made in various forms. In some cases it is supported by a rod, as in the figure ; in others, it is hung from the edge of the jar. The lower portion of the hquid is a strong solution of copper sulphate (blue stone) ; the upper portion is a weak solution of zinc sulphate/ which, being of less spe- cific gravity than the lower solution, rests upon it without mixing except by the slow process of diffusion. While the cell is in use, copper from the copper sulphate is continually de- posited upon the copper plate. By certain actions within the liquids which need not be considered, the other con- stituent of the copper sulphate is set free ' ^ at the zinc, with which it unites, forming zinc sulphate. The solu- tion of copper sulphate is continually renewed from a supply of crystals of copper sulphate placed about the copper plate. When not in use, this cell should be kept on a closed circuit through a considerable resistance (about 20 ohms). The small current then flowing tends to prevent the mixing of the liquids by dif- fusion ; otherwise the copper sulphate, coming in contact with the zinc plate, will deposit copper upon it, and in this con- dition the cell will furnish little or no current. The zinc is not amalgamated. Polarization is entirely avoided in the gravity cell, and the current that it sup- plies through a given circuit is approxi- mately constant. Its E. M. F. is about half that of the chromic acid cell, and its resistance is several times as great ; the largest current obtainable from it is consequently comparatively 1 Water containing a very little sulphuric acid may be used in setting up the cell. Fig, 277. 362 Electricity small. It is especially serviceable in experimental work requir- ing a constant E. M. F., and is much used for purposes requiring a current all or nearly all of the time, as in telegraphy. 452. The Daniell Cell. — This cell is essentially the same as the gravity cell; but its parts are differently arranged and the two solutions are kept separate by a partition of porous earthenware in the form of a cylindrical cup (Fig. 277). The porous cup con- tains the negative pole (a long bar of zinc) and a dilute solution of zinc sulphate. This is placed in a glass jar containing a satu- rated solution of copper sulphate. The positive plate is a sheet of copper surrounding the porous cup. II. The Electro-magnetic Field 453. Historical. — The first discovery of a definite relation between electricity and magnetism was made by Oersted, a Danish physicist, in 1819, — nineteen years after Volta's invention of the electric battery. He found that, when a wire carrying a current is placed in a horizontal position above a compass needle, the needle is deflected from the magnetic meridian. When the direction of the current is reversed or the wire held below the needle, the deflection is in the opposite direction. This is known as " Oersted's experiment." It marks the begin- ning of the science of eUctro-magnetismy — that branch of electrical science which treats of the relations between electricity and mag- netism and which is usefully applied in such inventions as the electric bell, the telegraph, the telephone, the dynamo, and the motor. Laboratory Exercise 6/. 454. Magnetic Field due to a Current in a Straight Conductor. — Iron filings sprinkled on a horizontal piece of cardboard, through which a vertical conductor passes, show circular lines of force about the conductor when a sufficiently strong current is flowing ^ 1 In studying the magnetic field about a conductor carrying a current, a strong current must be used ; otherwise the field would be too weak to bring iron filings into line, and the behavior of a magnetic needle would be largely modified by the The Electro-magnetic Field 363 Fig. 278. (Fig. 278). Since all cross-sections of the field taken at right angles to the conductor are alike, it will be seen that a straight con- ductor carrying a current is surrounded by a cylindrical magnetic field, whose lines of force are circles about the con- ductor as a center and lie in planes at right angles to it. The relation between the direction of the lines of force round the wire {i.e. the direction in which the north pole of a needle points) and the direction of the current is imix)rtant and may easily be remembered from the following right-hand rule: Grasp the wire with the right hand so that the extended thumb points in the direction of the current ; then the fingers point round the wire in the direction of the lines of force. 455. Field Due to a Current in a Circular Coil. — When a con- ductor is curved, the lines of force are crowded together on the concave side and spread apart on the convex side, the planes of the lines of force being perpendicular to the con- ductor at every point (Fig. 279) ; hence the field is relatively strong at the center of a circular coil, where lines of force round all parts of the coil meet. The field at the center of a circular coil is of special interest and importance, as it is utilized in the simplest form o{ galvanometer m measuring electric currents. It may be conveniently studied by sending a strong current through all the turns (usually fifteen) of a galvanometer coil. Iron filings sprinkled on a piece of cardboard, placed within the coil, will show that the lines of force at the center of the coil are straight and are perpen- magnetic field of the earth. A battery of three or four chromic acid cells connected , in parallel (Art. 481) gives a current sufficiently strong for this purpose; but even better results are obtained from a single cell by sending the current round a rec- tangle of insulated wire cohsisting of six or eight turns. The field is strengthened in proportion to the number of parallel wires, but is otherwise the same as if there were only one. Fig. 279. 364 Electricity dicular to the plane of the coil. Their direction relative to the direction of the current is given by the following right-hand rult for coils : Close the right hand and place it within the coil with the fingers pointing in the direction of the current: then the extended thumb points in the direction of the lines of force through the coil, 456. The Helix or Solenoid. ^ A long, cylindrical coil of wire is called a helix or solenoid. The successive turns of the coil may be at Some distance apart or may be in contact ; in the latter case insulated wire must be useci^ For some purposes coils are wound upon woo^^^-* make use of an additional instrument called the relay (Fig. 286). The relay acts on the same principle as the Fig. 286. sounder, but the electro- magnet is horizontal and the armature vertical. The lever that carries the armature is light and delicately balanced, and hence is easily moved to and fro by much smaller forces than are required to operate the lever of a sounder. The coils of the electro- magnet are connected with the line by means of the binding posts A and B. The wires of a local circuit containing the sounder and a battery to operate it are connected to the posts C and D. One of these posts is connected by a wire under the base of the instrument with a metal column, the upper end of which forms an arch above the lever, and the other post is similarly connected with the lever. The local circuit is closed by contact of the lever with the platinum tip of a screw, which it strikes when drawn over by the electro-magnet, and is broken when the magnet ceases to act and the lever is pulled back by a spring against the hard rubber tip of the opposite screw. Thus when the line circuit is closed or opened by means of the key, the local circuit is at the same instant closed or opened by the action of the relay. Since the resistance of the local circuit is small, one or two cells are sufficient to operate the sounder. The sounds made by the lever of the relay are nearly inaudible. 463. The Telegraph System. — A diagram of a complete tele- graph system connecting two cities is shown in Fig. 287. A key and relay are included in the main line at each station (of which Electrical Measurements 369 there may be any number). There is a line battery^ at each of the terminal stations, each consisting of many cells in series (Art. 480), and the two are so connected to the line that they exert an E. M. F. in the same direction through it. Some form of cell that does not polarize must be used, as the gravity cell. The New York Key Sounder^ Philadelphia f2!""K Key, \JX Local Battery Relay Local Battery Earth Y\G. 287. line wire is connected with the earth at the terminal stations by «ieans of metal plates sunk in moist ground. The earth com- pletes the circuit, taking the place of a return wire. The sounder at each station is in a local circuit connected with the relay. When an operator at any station on the line wishes to send a message, he opens the switch of his key. All other switches on the line must be closed. (Why ?) The operator first calls the station to which he wishes to send the message. The sounders at all the stations deliver the message, but the operator at the station called is the only one who pays attention to it. It is possible, by means of different connections and instru- ments of different construction from those here described, to send two or more messages over the same wire at the same time. IV. Electrical Measurements 464. Strength of Electric Currents. — The strength of an electric current can be determined by observing how great an effect of one kind or another it is capable of producing. Heating and chemical 1 In diagrams each cell of a battery is represented by two parallel lines ( 1 1) ; the short heavy line represents the negative plate, and the long, thin line the positive. 370 Electricity effects may be made to serve this purpose ; but the simplest and most convenient method is to use some form of instrument whose action is due to the magnetic field of the current. Such an instru- ment is called a galvanometer. There are various forms of galva- nometers, but all of them depend in their action upon the fact that the strength of an electric current is proportional to the inten- sity of its magnetic field. 465. Ohm's Law. — Utilizing the magnetic action of the electric current on a magnetic needle, (ieorg Ohm, a German physicist, discovered that the strength of the current in an electric circuit is proportional to the electro- motive force and inversely proportional to the resistance of the circuit. This is known as Ohm's law. It is stated in other terms in Art. 474. The relations included in the law may be separately stated as follows : — (i) If the E. M. F. and the resistance of a circuit (including the resistance of the battery) remain constant, the current remain^ constant. (2) If the resistance remains constant and the E. M. F. varies, the current is proportional to the E. M. F. (3) If the E. M. F. remains constant and the resistance varies, the current is inversely proportional to the resistance. For exam- ple, if the resistance is doubled, the current is decreased one half. 466. The Tangent Galvanometer. — The essential parts of a tangent galvanometer (Fig. 288) are a vertical coil of wire having one or more turns, and a compass with a graduated scale, placed at the center of the coil. The compass needle should be very short in comparison with the diameter of the coil, in order that it may be wholly within the sensibly constant portion of the magnetic field of the current at and near the center of the coil, in whatever direction it may Fig. 288. . , . . r y ' turn. A long, nonmagnetic pomter of alumi- num is commonly attached to the needle at right angles to it Electrical Measurements 371 Fig. 289. (Fig. 289) ; and it is the position of the pointer on the scale that is read. It is evident that the pointer and the needle turn through equal angles. At and near the center of the coil the lines of force of the magnetic field of the current are straight and are perpendicular to the plane of the coil (Art. 455). Hence, if the current in the coil were the only source of a magnetic field where the compass needle is placed, the needle would be brought to rest exactly at right angles to the plane of the coil whenever a current of any strength was flowing. The magnetic field of the earth, however, plays a necessary part in the use of the instrument, the behavior of the needle being determined by the relative intensity of the two fields. .In using a tangent galvanometer it must be set with the plane of the coil in the magnetic meridian ; in which position the lines of force of the coil are at right angles to those of the earth's field. In Fig. 290, let O denote the position of the north pole of the compass needle, ON the intensity and direction of the earth's magnetic field, and OD the intensity and direction of the field of the current. The direc- tion of the resultant of these forces is OAj which is therefore the direction of the resultant force upon the north pole of the needle. Since the resultant force upon the south pole is equal and opposite to that upon the north pole, the needle comes to rest in the line OA, and the deflection of the needle caused by the current is the angle NO A, Any increase in the strength of the current through the galva- nometer increases the strength of its field i^OD) proportionally, and hence increases the deflection, but not proportionally. This is evident from the two parts of the figure. The part at the left represents the field of the current equal to that of the earth, and the deflection is consequently 45°. The part at the right shows ^f A % Fig. 290. 372 Electricity V A B O J} i' Fig. 991. the effect of doubling the current (which makes OD twice as great) ; the deflection is increased, but is much less than 90°. In fact, the deflection is never quite 90°, how- ever great the current may be. Let C and C denote two currents through the same number of turns of the same galvanometer, and let OD and 0£, or JVA and NB (Fig. 291), denote the intensities of their fields at the center of the .galvanometer. OJV^, as before, is the intensity of the earth's field. Then angles a and a' are the deflections caused by C and C respectively. Now the strengths of the currents are proportional to the inten- sities of their magnetic fields (Art. 464), i>. C: C::NA:NB, Since the value of a ratio is not altered when its terms are divided by the same quantity, we may write the above proportion C: C: NA , NB ON ' ON (I) The ratio of one leg of a right triangle to the other is called the NA tangent^ of the angle opposite to the first leg. Thus is the tangent of angle a (commonly abbreviated to tan tf), and is 1 The tangent of angle A (Fig. a^a) is DE : AD or PG : AG, DE and FG being any line perpendicular to either side of the given angle. Since triangles ADE and AFG are similar, the ratios DE : AD and EG : AG are equal. It is evident, therefore, that the tangent of an angle is a definite quantity the value of which depends only upon the sire of the angle. Angles are not prop>ortional to their tangents, although small angles are very nearly so. The tangent of any angle from o'' to 90^* may be found from a table of tangents (Appendix, Table V). Electrical Measurements 373 the tangent of angle a! {tan a'). Hence proportion (i) may be written /-> r^t 4. 4. t / \ C : C : : tan a : tan a'. (2) That is, currents sent through the same number of turns of the coil of a tangent galvanometer are proportional to the tangents of the angles of deflection that they produce. This is why the instru- ment is called a tangent galvanometer. Example. — A current C causes a deflection of 50°, and another current C, a deflection of 25*^. It is found from a table of tangents that tan 50° =1.19 and tan 25° = .466. Hence C: C: : 1.19: .466 ; from which C — 2.55 C, While a tangent galvanometer having a scale graduated in de- grees may be thus used to determine the relative strengths of currents, it does not give' their numerical values. The numerical value (in amperes) may, however, be obtained by multiplying the tangent of the angle of deflection by a constant factor, found by experiment. Laboratory Exercise 68. 467. Use of Different Numbers of Turns of the Coil. — When equal currents are sent through different numbers of turns of a tangent galvanometer, the tangents of the angles of deflection are proportional to the number of turns used (Lab. Ex. -68). For example, when a current is passed through fifteen turns, the tan- gent of the angle of deflection is three times as great as when the same current is sent through five turns. This is due to the fact that the magnetic field of the coil is proportional to the number of turns through which the current is sent (see note to Art. 454). In measuring currents the most accurate results are obtained when the number of turns used is the one that makes the deflection nearest to 45°. PROBLEMS 1. How would the current from a given battery be affected by making the resistance of the circuit four times as great ? ten times as great ? 2. Make a diagram showing the deflection of the needle of a tangent 374 Electricity galvanometer due to a certain current, and also the deflection due ta currents two, three, four, and five times as great. What change in the increase of the deflection for successive equal increases of the current is shown by the diagram ? 3. What value docs the deflection approach as the current increases indefmitely ? 4. Why docs the stronger or weaker magnetization of a galvanometer needle not atfect the deflection ? Laboratory Exercise 6g. 468. Laws of Resistance. — The following laws of electrical resistance have been established by experiment : — I. Thf resistance of a conductor of uniform cross-section is pro- portional to its length. II. The resistance of a conductor is inversely proportional to the area of its cross-section. The resistance of a wire is, therefore, inversely proportional to the square of its diameter. For example, the resistance of a wire 3 mm. in diameter is one ninth as great as that of a wire of the same material and length and i mm. in diameter. IIL The resistance of a conductor depends upon the material of which it is made. The following table gives the relative or specific resistances of a number of substances in the form of wires of equal length and cross- section, the resistance of copper being taken as unity. Specific Resistances (referred to copper) Silver, annealed 0.94 Iron, telegraph wire . . . 9.4 Copper, annealed i.oo German silver 13.0 Aluminum 1. 81 Mercury 59.0 Iron, pure 6.03 Carbon (arc light) about . . 2500.0 IV. The resistance of metals and of mqst other substances in- creases as the temperature rises. TJie resistance of carbon^ dilute acidSf and solutions decreases with a rise of temperature. The resistance of nearly all the pure metals increases about 40 per cent with a rise of temperature of 100° C. The resistance of German silver and other alloys is much less affected by change of Electrical Measurements 375 temperature ; hence they are used in making standard resistance coils (Art. 470). The resistance of the carbon filament of an incandescent lamp when hot is only about half what it is when cold. V. The resistance of a conductor is the same at the same tem- perature whatever the strength of the current. 469. The Unit of Resistance. — The common unit of electrical resistance is called the ohm^ in honor of the physicist of that name. It is defined as the resistance of a uniform column of mer- cury 106.3 cm. long and one square millimeter in cross-section, at 0° C. It is very approximately the resistance of 157 ft. of No. 18 copper wire (diameter = 1.024 mm-) or 349 ft. of No. 16 (diameter = 1.29 mm.). 470. Resistance Coils. — Standard coils of known resistance are used in measuring resistances. They are called resistance coils, and a box containing a set of them is called a resist- ance box (Fig. 293). The coils are made of insulated wire, generally of an alloy having a high specific re- sistance j and the ends of each coil are connected to brass blocks, A, By C (Fig. 294), on the top of the box. These blocks are separated a short distance ; but they are connected electrically by means of the coils, and may also be connected by inserting brass plugs, which fit snugly into the spaces between them. The resistance of the row of blocks and plugs is practically zero ; but, wherever a plug is re- moved, the resistance of the coil that bridges the gap is introduced into the circuit in which The amount of this resistance is marked When two or more plugs are removed, ^93- Fig. 294. the box is included, on the top of the box. 3/6 Electricity the total resistance introduced is the sum of the resistances of the coils that connect the gaps. A set of coils generally includes .1, .2, .3, .4, I, 2, 3, 4, 10, 20, 30, and 40 ohms, and may extend to much higher resistances. Any resistance from .1 ohm to III ohms can be introduced into a circuit with such a box. In finding a required resistance, the coils are tried in order from larger to smaller, as weights are tried in weighing. 471. Measurement of Resistance. — The resistance of a con- ductor can be measured in a number of ways ; but the method of substitution is the only one that we shall consider. Suppose the resistance of a coil of wire, R (Fig. 295), j\->. is to be found. A constant cell (Art 451) is connected with a galvanometer, . stated more fully, the power of a current utilized in any part of the circuit is pro- portional to the strength of the current and to the fall of potential in that part of the circuit. The electric unit of power is called the watt; it is defined as the power of a current of one ampere when driven by an E. M. F. of one volt. Hence, the power of a current in watts is equal to the product of the volts and the amperes; that is, Power ^ EC watts. (10) One thousand watts is called a kiloioatt; hence, EC Power = kilowatts. (11) 1000 It can be shown that one horse i)ower (Art. 153) is equal to 746 watts; hence, ^q Power = — horse power. (12) 746 Examples. — i. If a iio-volt incandescent lamp takes a current of .5 ampere, the power required to light it is i lo x .5, or 55 watts. A little more than one horse power (770 watts) would be required to light fourteen such lamps. 2. The power expended in lighting an arc lamp when the difference of potential between the carbons is 45 volts, and the current 8 amperes, is 45 X 8, or 360 watts (a trifle less than half a horse power). PROBLEMS 1. What is the power of a battery that is able to maintain a current of 4 amperes through a resistance of 6 ohms? 2. A current of 5 amperes is passed for one minute through a coil of 4 ohms' resistance in a calorimeter containing 200 g. of water. Neglecting the heat absorbed by the calorimeter, what is the rise of temperature of the water? 3. A i6-candle-power lamp has a resistance of 200 ohms when hot, and is used on iio-volt circuit. WTiat is the cost of running the lamp at the rate of ten cents per kilowatt-hour? (A kilowatt-hour is a power of one kilowatt supplied for one hour.) 4. An arc lamp takes a current of 7 amperes with an E. M. T. of 50 volts. What is the cost of running the lamp at eight cents per kilowatt-hour? Induced Currents 389 VI. Induced Currents 310. 492. Induction of Currents by Magnets. — Electric currents can be generated without chemical action by means of a process called eleciro-7nagnetic induction, or simply induction. Induced currents are generated on a large scale by means of dynamos. The laws of electro-magnetic induc- tion can be studied by means of the apparatus shown in Figs. 310 and 312. A coil of insu- lated wire is connected with a sensitive galvanometer (astatic or d'Arsonval) . While a strong magnet is being rapidly inserted into the hollow of the coil or rapidly withdrawn from it, the galvanometer indicates a mo- mentary current ; but there is no current while the magnet remains at rest within the coil. Inserting the north pole of the mag- net causes a deflection of the needle in one direction ; insert- ing the south pole, a deflection in the opposite direction. When either pole is withdrawn, the direction of the current is opposite to that produced by inserting the same pole. The induced current is called direct if its direction round the coil is such that like poles of the coil and the magnet point in the same direction ; inverse^ if their like poles point in opposite direc- tions. The direction of the current round the coil can be deter- mined from its connection with the galvanometer and the direction in which the needle is deflected. It will be found that the current is inverse when either pole of the magnet is inserted and direct when it is luithdrawn ( Fig. 311). Laboratory Exercise ^4. 493. Source of the Energy of the Induced Current. — It will be seen from Fig. 311 that, whether the magnet is being inserted or 390 Electricity Fia 311. removed, its motion is opposed by the magnetic field of the induced current. Thus on account of the induced current more work must be done in moving the magnet either into or out of the coil than would other- wise be required. This additional work is the source of the energy of the induced current. The transformation of mechan- ical energy into the electrical energy of the induced current is supposed to be effected through the medium of the ether. It takes place on a large scale in the generation of currents by dynamos. 494. Induction of Currents by Currents. — The same effects are produced when a second coil, in which a strong current is flow- ing, is used instead of the magnet in the preceding experiments (Fig. 312). The coil that takes the place of the magnet is called the primaiy coil^ the other the secondary eoil. The primary coil is connected with a battery, and its inductive action, like that of a mag- net, is due to its magnetic field. The inverse induced cur- rent, which is caused by inserting the pri- mary coil into the secondary, is oppo- site in direction to the primary current ; the direct induced current, which is caused by withdrawing the primary coil, is in the same direction as the primary current. If the primary circuit is closed and broken while the primary Fig. 312. Induced Currents 391 coil remains at rest within the secondary, the effects are respec- tively the same as when the primary coil is inserted and with- drawn with the circuit closed. In either case the induced current is due to the change in the magnetic field within the secondary coil. The induced currents are in all cases much stronger when the primary coil contains a soft iron core. This is because the iron greatly increases the strength of the magnetic field. 495. Laws of Electro- magnetic Induction. — The following laws of electro-magnetic induction have been established by experiment. The pupil should consider to what extent the^ are illustrated by the experiments previously discussed and by subsequent experi- ments with induction coils. I. An increase in the strength of the magnetic field within a closed coil induces an inverse current^ and a decrease in the strength of the field induces a direct current. It will be helpful to remember that the direction of an inverse induced current is anti-clockwise round the coil to an observer looking in the direction of the lines of force of the magnetic field that causes the induction, and that the direction of a direct induced current is clockwise, when viewed in the same manner (Fig. 311)- II. The induced E.M.F. (i.e. the E.M.F. of the induced current^ is proportional to the rate of increase or decrease of the magnetic field within the coil, and also to the number of turns in the coil. The effect of the rate of change of the magnetic field is readily shown by inserting and removing the primary coil at different rates of speed with an iron core inserted. The deflection is con- siderable when the motion is rapid, but may be indefinitely decreased by moving the coil more and more slowly {Exp.). III. The ratio of the induced E. M. F. to the E. M. F. of the current in the primary coil is very nearly equal to the ratio of the number of turns in the secondary coil to the number of turns in the primary. 392 Electricity Thus if there are 150 turns in the primary coil and 30,000 in the secondary, the E. M. F. of the induced current is approxi- mately 200 times as great as that of the primary current. This principle is applied in the generation of high potential currents by means of induction coils (Art. 498). An induced current of lower potential than the primary is obtained when the number of turns in the secondary coil is less than that in the primary. This principle is utilized in the transformer (Art. 507). IV. There is no gain of energy in electro-magnetic induction. The energy of the induced current is derived either from mechanical work, 'as in the experiments with the coil and the magnet and in the generation of currents by dynamos, or from a current in another circuit (without transference of electricity between the circuits), as in making and breaking the circuit through the primary coil when at rest in the secondary and in the action of induction coils and transformers. 496. Historical. — Induced currents were discovered in 1831 by Michael Faraday, one of the greatest of English physicists. Knowing that electric currents act- upon magnets, he conducted a series of experiments extending over seven years in the attempt to discover any action of magnets upon currents, and was at last rewarded by the discovery of electro-magnetic induction. Tyndall pronounces this the greatest experimental result ever obtained. Its importance can hardly be overestimated, since the action of the dynamo depends upon induction, and the currents for all industrial applications of electricity on a large scale are generated by dynamos. 497. Self-induction. — Whenever a current commences or ceases in a coil, the current in each turn exerts an inductive action upon all the turns of the coil. This action of a current upon itself is called self-induction^ and the current due to it is often called the extra current. Self-induction is very considerable if the coil has many turns, especially if it contains an iron core. When the cur- rent is turned on in a coil, the growth of its own magnetic field has the same effect as if a magnet were suddenly thrust into the Induced Currents 393 coil. The inverse E. M. F. thus induced opposes the current, preventing an immediate rise to its full value. When the circuit is broken, the effect of self-induction is the same as if a magnet were suddenly withdrawn from the coil. The induced E. M. F. in this case is direct. It is generally many times greater than the original or pri- mary E. M. F., and continues the cur- rent across the air gap where the cir- cuit is broken, caus- ing a spark. This effect of self- induction can be shown as follows : A file is connected to one pole of a chromic acid bat- tery and a piece of wire to the other. As the free end of this wire is drawn over the file, the circuit is rapidly closed and broken, and at each break a minute spark occurs. When the experiment is repeated with the coils of a large electro-magnet included in the circuit (Fig. 313), brilliant sparks are obtained, indicating a high induced E. M. F. at each break {Exp.). 498. The Induction Coil. — The indue fion or Ruhmkorff coil (Fig. 314) is an instrument for generating induced currents of very high potential. A simplified diagram of the essential parts is shown in Fig. 315. These are an iron core, AB \ a primary coil consisting of one or two layers of turns of large insulated wire ; a secondary coil of very fine wire, well insulated and often many miles in length ; an automatic make-and-break device, or current interrupter, CD, which is included in the primary circuit ; and a condenser, E. There is generally also a device, called a confinu- tator, for reversing the current through the primary coil without changing the battery connections ; but this is not essential. Fig. 313. 394 Electricity When a current from a battery is sent through the primary coil, it magnetizes the iron core, and the core attracts the iron block I'iG. 314. C, which IS supported near the end of the core upon a spring. This spring is the movable part of the interrupter, and the pri- mary current passes between it and the point of a screw, D, against which it rests. By the attraction of the magnetized core the spring is drawn away from the point, breaking the circuit. The core instantly becomes demag- netized, and the spring flies back again, closing the circuit. The primary circuit is thus closed and broken many times every second, causing alternately an inverse and a direct induced E. M. F. in the secondary coil. The ends ^'^- 3^5- of the secondary coil are connected with the binding posts R and G^ and may be extended by means of rods or wires attached to the posts until the gap H is made as small as desired. When this gap is not too great, an electric spark passes between the terminals with every interruption of the primary current. The Induced Currents 395 length of the spark that can be obtained increases with the in- duced E. M. F., and varies in different coils from a few milli- meters to 30 cm. or more for very powerful coils. It is estimated that an E. M. F. of 30,000 volts is required to cause a spark across a distance of i cm. in air under atmospheric pressure and at ordinary temperatures ; and that, under the same conditions, an E. M. F. of at least 300 or 400 volts is required to start a spark, however short. The E. M. F. of the induced current increases with the number of turns in the secondary coil and with the rate of change of the magnetic field (Art. 495, Law II). The latter depends upon the rate of increase or decrease of the current in the primary coil, both of which are retarded by self-induction. The stopping of the primary current is, however, much more abrupt than the starting and induces a correspondingly greater E. M. F. In general, it is only at the " break " of the primary circuit that a spark occurs between the terminals of the secondary coil. The purpose of the condenser is to prevent or at least diminish the spark at the inter- rupter, and thus increase the abruptness of the " break." This it does by serving as a temporary reservoir into which the extra cur- rent flows instead of jumping across the gap. (The construction and action of a condenser are discussed in Art. 524.) 499. Effects of the Induced Current. — While the E. M. F. of the induced current is enormously higher than that of the bat- tery current through the primary coil, its strength is exceedingly small. The induced current may be compared to water flowing through a very small pipe under very great pressure, and the pri- mary current to water flowing through a large pipe under very little pressure. Although the energy of the induced current is necessarily less than the total energy of the primary current, the induced current is nevertheless capable of producing effects that are impossible with the primary current. For example, a spark 3 or 4 cm. long is capable of piercing a sheet of cardboard or thin pieces of other nonconductors {Exp.). The induced current is also capable of 396 Electricity producing a shock and other physiological effects. These are the well-known effects of the physician's battery, which is a small induction coil operated by a voltaic cell. The handles which are held by the patient are the terminals of the secondary coil. The current from a powerful induction coil is very painful and may even be dangerous. The induction coil is also used for obtaining discharges in rarefied gases inclosed in glass tubes and bulbs (Art. 526). VII. The Dynamo and the Motor 500. The Principle of the Dynamo. — Suppose a single loop of wire to be mounted on an axis at right angles to the lines of force of a strong magnetic field as shown in Fig 316. When the loop is vertical, the portion of the magnetic field extending through it in the direction of the lines of force is as great as possible. As the loop is turned from li.is position, the cross- section of the field extending through it (always taken at right angles to Fig. 316. jj^g Ijj^gg Qf force) decreases, and be- comes zero when the loop is horizontal. When the magnetic field is thus Removed from within the loop, the inductive action is the same as if it were removed in any other way. With the direction of rotation indicated by the arrow, the induced current is clockwise, looking in the direction of the lines of force. As the rotation is continued in the same direction from the horizontal to the vertical position again, an increasing cross- section of the magnetic field extends through the coil. This induces an anti-clockwise current, looking in the same direction as before ; but, as the opposite face of the loop is now turned toward the observer, the direction of the current round the loop is the same as before. As the loop passes the vertical, the current is reversed in it, and continues thus till it passes through the vertical The Dynamo and the Motor 397 again. (Why?) Thus a continuous rotation of the loop induces an alternating current in it, the reversal of the current taking place twice during each rotation, as the loop passes through the position at right angles to the lines of force. With a constant rate of rotation, the cross-section of the mag- netic field extending through the loop changes most rapidly when the loop is in .the neighborhood of the horizontal position, and least rapidly in the neighborhood of the vertical position ; hence the induced E. M. F. is greatest in the horizontal position and least in the vertical. In fact, it diminishes to zero in the latter position at the instant it reverses in direction. The induced current passes through like changes.^ The current thus generated in the loop can be sent through an external circuit by means of either device shown in Figs. 317 and 318. In the first case each end of the loop is connected Fig. 317. Fig. 318. with a copper ring surrounding the axis. The terminals of the external circuit are connected with copper strips, called brushes^ which press against the rings and make sliding contact with them as they rotate. The current in the external circuit reverses with every reversal in the loop. This is the principle of the alternating- current dynamo. In the second case the ends of the loop are connected with the two halves of a split copper tube. This device is called a commutator. The brushes are adjusted so that the contact of each changes from one segment of the commutator 1 If the lines of force of the field were vertical, it would be necessary to read hori- zontal for vertical, and v/V. they continue only so long as the pres- ence of the inducing charge keeps them separated. But if the ball be touched by the finger while a negatively electrified rod is held near it, the negative induced charge escapes, leaving only a positive charge on the ball. This remains as a permanent induced charge when the finger is removed before the rod is. The pres- ence of a positive charge on the ball is proved if the ball is repelled on bringing up an electrified glass rod. It will be seen that a permanent charge obtained by induction is unlike the inducing charge. Electrostatics 415 520. The Electroscope. — The suspenled pith ball can be used as an electroscope to detect the presence of a charge upon any body and to determine its sign. The pith ball is given a charge of known sign, and the body to be tested is brought near it. If the ball is repelled, the body is electrified, and its charge is like that of the ball. The attraction of the ball is not a certain test of electrification. (Why not?) 521. The Electric Field. — Electrostatic forces, like magnetic forces, are supposed to act through the medium of the ether. The two forces are of a different character, however, and are wholly unrelated; for static electricity and magnetism have no effect upon each other. The terms electric field and lines of electric force correspond respectively to magnetic field and lines of magnetic force. 522. Electrical Machines. — Machines for developing and col- lecting charges of electricity are of two types ; namely, friction machines and induction machines. Friction Machines. — Figure 333 represents one form of friction machine. A positive charge is developed on a large revolving glass disk, A^ by the friction of leather pads, B. The charge is col- lected on each side by a number of points ^ ^^i^^n^jj^^ /\ Iw which project from a brass rod and nearly touch the disk. The rods carry the charge to an insulated brass yig. 333. cylinder, C, from which it can be drawn off as a spark discharge by bringing the finger or any other conductor near it. A spark a centimeter or more in length can be obtained in this manner from a machine in good condition. Friction machines of various forms were invented during the 4i6 Electricity eighteenth century; but they are greatly inferior to the more modern induction machines, by which they have been superseded. Induction Machines, — The elecirophorus (Fig. 334) is the simplest induction machine. It consists of a disk of vulcanite or other resinous material, and a metal disk of slightly smaller diameter, provided with an insu- lating handle. The vulcanite is negatively electrified by striking or rubbing it with catskin or flannel, and the metal disk or cover is then placed upon it. The disks really touch at only a few points ; and, as the vulcanite is a nonconductor, it does not lose any appreciable part of its charge to the cover. The entire charge, however, acts inductively on the cover, producing a positive charge on its lower side and a nega- tive charge on its upper side (Fig. 335, A). The negative charge is repelled by the charge on the vulcanite, and is permitted to escape by touching the cover with the finger. The positive charge remains, being " bound " by the attraction of the charge on the vulcanite (Fig. 335, B). This leaves the disk positively Fig. 334, cs Fig. 335. electrified when it is lifted from the vulcanite by means of llie handle. It can then be discharged by bringing the finger or other conductor near it, as its charge is no longer bound. The cover can be repeatedly charged and discharged in this manner without again rubbing the vulcanite. Electrostatics 417 Different forms of induction machines have been invented which are wholly automatic in their action, and are much more powerful than the electrophorus. One of these — the Toepkr-Holtz machine — is shown in Fig. 336. The movable parts are carried on a large glass disk. Positive and negative charges are induced on different parts of the revolving disk as they pass certain points. These charges are collected by projecting metallic points, as in the friction machine, and accumulate on insulated conductors until the difference between their potentials is sufficient to cause a spark discharge across the gap between the knobs. Sparks from 5 cm. to 10 cm. long can be obtained from machines of moder- ate size. Full descriptions of these machines are to be found in larger works. 41 8 Electricity 523. Potential of SUtic Electricity. — The same diffcience of potential is required to produce a spark of given length whether it is obtained from an electrified body or an induction coil. Hence we know from the lengths of the sparks that the potentirls due to electrification are often from tens of thousands to hundreds of thousands of volts. A potential difference of 100,000 to 300,000 volts can be obtained with a Toepler-Holtz machine of medium size. In fact, the potential to which it is possible to charge the machine or any body, depends only upon the insulation and the dryness of the atmosphere. Beyond this limit the charge escapes as rapidly as it is developed or imparted. Charges at even the highest potentials mentioned are not dangerous unless the quantity of the charge is much larger than is generally the case. An electrical machine is capable of furnishing small quantities of electricity in the form of an intermittent current of very high E. M. F., like the current produced by an induction coil (Art. 499). Most experiments requiring a high-potentiaU current can there- fore be performed either with af machine or a coil. 524. The Leyden Jar. — The Leyden jar (Fig. 337) is a device for accumulating and storing a large charge, either positive or negative. It received its name from the city of Leyden in the Netherlands, where it was invented in 1746. It consists of a glass jar coated inside and out for about two thirds its height with tin foil. A brass rod, terminating in a knob at the top, extends through the stopper, and is connected with the inner coat of the jar by means of a chain attached to its lower end. The jar is charged by connecting the rod or the knob with one of the terminals of an electrical machine. To dis- ' charge it, one end of a short conductor is touched to its outer coat and the other end brought near the knob. When it is sufficiently near, a spark occurs, discharging the jar. The discharging conductor must be provided with an insulating handle to avoid a shock which, with a large jar, would be very painful and possibly dangerous. Electrostatics 419 The action of the jar is illustrated by the following experiments : (i) The jar is placed on the table and charged, by means of an induction machine, for a certain length of time or until the handle of the mafchine has made a certain number of revolutions. The jar is then discharged, and the length and intensity of the spark noted. (2) The jar is charged for the same length of time as before, while standing on an insulator (a large sheet of vulcanite or glass), and again discharged. The spark obtained with this discharge fs much thinner and less brilliant than before, indicating that the quantity of electricity in the charge is much less (^Exp.).. The explanation of this difference is as follows : While the charge is accumulating on the inner coat of the jar in the first experi- ment, it attracts an opposite charge to the outer coat by induction through the glass. In the accumulation of this charge the table serves as a conductor. In the second experiment the insulation of the jar prevents an induced charge on the outer coat. When the outer coat of the jar is not insulated, the charge that is induced on it attracts the charge on the inner coat. This attraction de- creases the potential of the latter charge, and consequently increases the rate at which the charging takes place. It follows that the attraction of the induced charge increases the amount of the charge on the inner coat for a given potential ; or, in other words, the induced charge increases the capacity of the condenser. The extent to which the capacity of a jar is thus increased is perhaps best shown by the action of the jars of an induction machine (Fig. ^2>^)' When the machine is operated, the charges accumulate principally in the jars, the positive charge in one, the negative in the other. The outer coats of the jars become oppo- sitely charged by induction, each receiving its charge from the other through a metal conductor by which they are connected under the base of the instrument. Under these conditions, the machine gives a thick, brilliant spark at intervals of several seconds. When the outer coats of the jars are disconnected by opening a switch (not shown in the figure), the sparks are thin and much less brilliant than before, and, at the same time, 420 Electricity are much more frequent {Exp.), The quantity of electricity that is discharged with each spark is evidently very much less than before, indicating a corresponding decrease in the capacity of the jars. This is due to the fact that the outer coats of the jars do not become charged, the wooden base of the machine being practically an insulator for such rapid action. The Leyden jar is one form of condenseKf the essential parts of a condenser being two conductors very near each other, but separated by an insulator. A sheet of glass, mica, or paraffined paper, with a smaller sheet of tinfoil attached to each side, leav- ing a wide margin of the insulator round the foil, is a simple form of condenser. 525. Distribution of an Electrical Charge ; Effect of Points. — It is shown by experiments not to be described here that an elec- trical charge resides wholly upon the surface of a solid body, and only upon the outer surface of a hollow body unless there is an opposite charge upon another body inside it. This is due to the repulsion of all parts of a charge for every other part. If the charged body is a conductor, this self-repulsion of the charge causes a definite distribution of it, which depends only upon the shape of the conductor (assuming that there are no other charges in the vicinity to cause induction). A charge is distrib- uted uniformly over the surface of a sphere ; upon other bodies the quantity per unit of surface, or the electric density, is greater where the curvature is greater, and is greatest at edges, corners, and especially at points. " At a point, indeed, the density of the collected electricity may be so great as to electrify the neighboring particles of air, which then are repelled, thus producing a continual loss of charge. For this reason points and sharp edges are always avoided on electrical apparatus, except where it is specially desired to set up a discharge. The effect of points in discharging electricity from the surface of a conductor may be readily proved by numerous experiments. If an electrical machine be in good working order, and capable of giving, say, sparks four inches long when the knuckle is presented to the Electrostatics 421 Fig. 338. knob, it will be found that, on fastening a fine-pointed needle to the conductor, it discharges the electricity so effectually at its point that only the shortest sparks can be drawn at the knob, while a fine jet or brush of pale blue light will appear at the point. If a lighted taper be held in front of the point, the flame will be visibly blown aside (Fig. 338) by the streams of electrified air repelled from the point. These air currents can be felt with the hand. They are due to a mutual repulsion between the electrified air particles near the point and the electricity collected on the point itself." — S. P. Thompson's Elementary Lessons in Electricity and Magnetisfn. 526. The Electric Discharge in Rarefied Gases. — The electric discharge is produced in rarefied gases by means of glass tubes or bulbs, provided with electrodes of platinum wire fused into the glass. Such tubes, when exhausted to a pressure of one or two millimeters of mer- cury, are known as Geissler tubes ( Fig. 339). The differ- ence of potential required to pro- duce a discharge s^ \^-^. Fig. 339. in any gas, between electrodes at a given distance apart, decreases as the pressure of the gas is diminished ; and an induction coil giving a spark i cm. long in air will illuminate a Geissler tube 12 or 15 cm. long. An induction machine can also be used for the purpose. "Through such tubes, before exhaustion, the spark passes without any unusual phenomena being produced. As the air is 422 Electricity exhausted, the sparks become less sharply defined, and widen out to occupy the whole tube, becoming pale in tint and nebulous in form. The cathode exhibits a beautiful bluish or violet glow, separated from the conductor by a narrow dark space^ while at the anode a single small bright star of light is all that remains. At a certain degree of exhaustion the light in the tube breaks up into a set of striip, or patches of light of a cup-like form, which vibrate to and fro between darker spaces." (Thompson.) The color of the discharge in Geissler tubes is different with different gases.^ 527. Atmospheric Electricity. — The sparks obtained from electrical machines and Leyden jars suggested to a number of the early experimenters in electricity that lightning was due to elec- trical discharges in the atmosphere. Benjamin Franklin put this theory to an experimental test in 1752. " He sent up a kite dur- ing the passing of a storm, and found the wetted string to conduct electricity to the earth, and to yield abundance of sparks. These he drew from a key tied to the string, a silk ribbon being interposed between his hand and the key for safety. Leyden jars could be charged, and all other electrical effects produced, by the sparks furnished from the clouds. The proof of the identity was com- plete." (Thompson.) It has been repeatedly shown by later experiments that the atmosphere is generally electrified even in fair weather. In fair weather the electrification is almost always positive ; in stormy weather it is sometimes positive and sometimes negative. The potential increases with the altitude ; but differs widely in different localities and with different states of the weather. The rise of potential has been found as great as 600 volts per meter of eleva- tion above the ground. 1 As the exhaustion in a vacuum tube is continued beyond a pressure of one millimeter, the dark space surrounding the cathode increases in width u:;;!). >Jicn the pressure is reduced to about one millionth of an atmosphere, it completely fills the tube. Tubes exhausted to this degree are called Crookes tubes. The eloctric discharge in a Crookes tube produces new forms of radiation, called cathode rays and X-rays. The latter are also known as Roentgen rays, from their discoverer. The pupil is referred to other works for an account of these rays and their applications. Electrostatics 423 Various theories have been advanced to account for the electri- fication of the atmosphere ; but very little is definitely known about it. Evaporation is very probably one of the principal causes. But, aside from this question, if we suppose the particles of water vapor in the atmosphere to be even slightly electrified, the high potential of clouds is easily explained ; for, as the particles unite in the process of condensation, the charge increases much more rapidly than the capacity of the drop. For example, if one million equally charged particles unite, the potential becomes ten thousand times as great ; and there are thousands of milHons of particles in a drop. The great length of lightning sparks or flashes shows that the potential of a thunder-cloud is enormously high. 528. Thunder. — Thunder corresponds to the snapping sound produced by an electric spark. The sudden heating of the air along the path of a lightning flash causes it to expand with explo- sive violence, producing sound waves of great intensity. If the flash is short and straight, the sound is a short clap ; if it is long and zigzag, the sounds produced by its different parts have unequal distances to travel to the observer and are heard in quick succes- sion as a continuous rattle. The rolling sound of distant thunder is due to various reflections of the sound from clouds, from the ground, and often from neighboring hills. 529. Lightning Conductors. — The use of lightning conductors to protect buildings was first suggested by Benjamin Franklin. The usual device consists of one or more iron rods, extending some distance above the highest points of a building and connected by means of large iron or copper conductors with datnp earth or, better, with water. If the conductor ends in dry earth, it is not only useless but even dangerous. (Why?) Each rod is terminated by a gilded copper point. The action of a lightning conductor depends largely upon in- duction. A charged cloud induces an opposite charge on the ground under it and on houses, trees, and other objects within this area. This inductive action is strongest upon the highest objects, and causes lightning rods to become highly electrified. 424 Electricity Under these conditions a rapid and continuous discharge takes place from the sharply pointed tips of the rods (Art. 525). This quiet discharge of opposite electrification toward the cloud is often sufficient to prevent lightning ; but, if a stroke does occur, the rod receives the discharge and the building is preserved. 530. The Aurora Borealis. — "In the northern regions of the earth the aurora horfalis, or northern lights^ is an occasional phe- nomenon ; and within and near the Arctic Circle is of almost nighdy occurrence. Similar lights are seen in the south polar regions of the earth, and are denominated aurora ausiralis. As Fig. 34a seen in European latitudes, the usual form assumed by the aurora is that of a number of ill-defined streaks or streamers of a pale tint (sometimes tinged with red and other colors), either radiat- ing in a fanlike form from the horizon in the direction of the magnetic north, or forming a sort of arch across that region of the sky, of the general form shown in Fig. 340. A certain flicker- ing or streaming motion is often discernible in the streaks. Under very favorable circumstances the aurora extends over the entire Electrostatics 425 sky. The appearance of an aurora is usually accompanied by a magnetic storm, affecting the compass-needles over whole regions of the globe. This fact, and the position of the auroral arches and streamers with respect to the magnetic meridian, directly suggest an electric origin for the light, — a conjecture which is confirmed by the many analogies between auroral phenomena and those of discharge in rarefied air. Yet the presence of an aurora does not, at least in our latitudes, affect the electric condi- tions of the lower regions of the atmosphere. " The most probable theory of the aurora is that originally due to Franklin; namely, that it is due to electric discharges in the upper air, in consequence of the differing electrical conditions between the cold air of the polar regions and the warmer streams of air and vapor raised from the level of the ocean in tropical regions by the heat of the sun." (Thompson.) APPENDIX Table I Metric Units of Lengthy Surface^ and Volume lo millimeters (mm.) lo centimeters (cm.) lo decimeters (dm.) loo sq. millimeters (smm.) lOo sq. centimeters (scm.) loo sq. decimeters (sdm.) looo cu. millimeters (cmm.) looo cu. centimeters (ccm.) xooo cu. decimeters (cdm.) : I centimeter : I decimeter : I meter (m.) : I sq. centimeter : I sq. decimeter : I sq. meter 1 cu. centimeter : I cu. decimeter : I cu. meter (cu. m.) Table n Equivalents Metric to English cm. = .3937 in. m- =39-37 in. km. =.6214 mile scm. =.1550 sq. in. sq. m. = 1.196 sq. yd. = 10.764 sq. ft. I ccm. =.06103 cu. in. I cdm. =1.0567 qt. (liquid) I cu. m.= 1.308 cu. yd. = 35-317 cu. ft English to Metric * I in. = 2.540 cm. I ft. = 30.48 cm. I yd. =.9144 m. I mile = 1.6093 km. I sq. in. =6.452 scm. I sq.ft. =929.0 scm. I sq. yd. = .8361 sq. m. I cu. in. = 16.387 ccm. I cu. ft. =28,315. ccm. I cu. yd. = .7645 cu. m. I qt. = .9463 cdm. (liters) I gal. = 3.785 liters I gram = .0353 oz. I kg. = 2.2046 lb. 426 oz. lb. = 28.35 g. = 453.6 g. Appendix 427 Table III Mensuration Rules ratio of the circumference of a circle to its diameter = 3.1416 Circumference of a circle (radius, r) = 2 Trr Area of a circle = -nr^ Surface of a sphere = 4 irr^ Volume of a sphere = f Trr^ Lateral surface of a right cylinder (altitude h and radius of base r) = 2 irrh Volume of a right cylinder = irr^h Table IV Densities (in grams per ccm.) Aluminum . . Antimony, cast . Beeswax . . . Bismuth, cast . Brass .... Copper . . . Cork . . . . Galena . . . German silver . Glass, crown . . Glass, flint . . Gold . . . . Ice Iron, bar . . . Iron, cast . . . Ivory . . . . Lead . . . . Marble . . . Mercury, at o°C. Platinum . . . Quartz . . . Silver . . . . Steel . . . . Sulphur, native . Tin. ... . Zinc,' cast . . . 2.67 6.72 .96 9.8 8.4 8.8 to .14 to 7.58 8.5 2-5 3 to 19-3 .917 7.8 7.2 to 1.9 11.3 to 2.72 13-596 21.5 2.65 10.4 7.8 2.03 7-3 6.86 8.9 .24 3-5 7.3 11.4 to 10.5 to 7.9 Alcohol (95%) . . .82 Blood 1.06 Carbon disulphide . 1.29 Chloroform . . . 1.5 Copper sulphate solution i . 1 6 Ether 72 Glycerine . . . . 1.27 Hydrochloric acid . 1.22 Mercury, at 0° C. . 13.596 Milk 1.03 Nitric acid ... 1.5 Oil of turpentine . .87 Olive oil 915 Sulphuricacid(i5%) i.io Sulphuric acid . . 1.8 Water (4° C.) . . i.ooo Water, sea . . . 1.026 Gases at 0° C. and 76 cm. Pressure Air 001293 Carbon dioxide . . .001977 Hydrogen . . . .0000896 Nitrogen 001256 Oxygen 001430 428 Appendix Table V Tangents of Angles To find the tangent of an angle not measured by a whole num- ber of degrees, find first the tangent of the integral part of the number, and add to this the product obtained by multiplying the difference between this tangent and the tangent of the next whole number of degrees by the decimal part of the angle. For example, to find the tangent of 38°.7, proceed thus : — tan 38* =.781, tan 39* = .810. .810— .781 = .029. .7 X .029 = .020. tan 38^.7 = .781 -f .020 = .801. Anglk Tangent Angle Tangent Angle Tangent Angle Tangent 0° .0000 23° .424 46^ 1.036 69° 2.61 I .0175 24 .445 47 1.072 70 2.75 2 .0349 25 .466 48 I. Ill 71 2.90 3 .05 24 26 .488 49 1. 150 72 3.08 4 .0699 27 .510 50 1. 192 73 3-27 5 .0875 28 •532 51 1-235 74 3-49 6 .1051 29 •554 52 1.280 75 3-73 7 .1228 30 •577 53 1-327 76 4.01 8 .1405 31 .601 54 1.376 77 4-33 9 .1584 32 .625 55 1.428 78 4.70 ID .1763 33 .649 56 1.483 79 5.14 II .194 34 .675 57 1.540 80 5.67 12 •213 35 .700 58 1.600 81 6.31 13 .231 36 .727 59 1.664 •82 7.12 14 .249 37 .754 60 1-732 S3 8.14 '5 .268 38 .781 61 1.804 84 9-51 16 .287 39 .810 62 1.88 85 11-43 17 .306 40 •839 63 1.96 86 14.30 18 •325 41 .869 64 2.05 87 19.08 19 .344 42 .900 65 2.14 88 28.64 20 .364 43 .933 66 2.25 89 57-29 21 .384 44 .966 67 2.36 90 00 22 .404 45 1,000 68 2.48 Appendix 429 VI — References to Chute's Physical Laboratory Manual The following list of references to the revised edition of Chute's Physical Laboratory Manual, published by D. C. Heath & Co., is provided for the convenience of teachers who may wish to use this manual in connection with the text. The numbers in the first column refer to articles in the text ; those in the last column, to articles in the manual. Text 14,15 15 15 19 22-25 30-32 35 36 47 53 62, 63 67,68 96,97 119-123 130-138 155 159 162-164 166 190 199 231 233 235 237 241 241 245 249 257 263 Topic illustrated Manual Extension 19-21 Capacity 25 Volume by displacement ... 28 Weighing. . 31 Liquid pressure 52 Buoyancy of liquids . . . . 55 Specific gravity of solids . . 56, 57 Specific gravity of liquids . . 58 Boyle's Law 53 The siphon 54 Concurrent forces 39 Parallel forces 40 Uniformly accelerated motion . 42 Curvilinear motion 41 The pendulum 43 The lever 44 The wheel and axle .... 46 Pulleys 45 The inclined plane .... 47 Tenacity 35 Capillarity 51 The fixed points of a thermometer 85 Coefficient of linear expansion . 86 Coefficient of cubical expansion 87 Law of Charles ..... 88 Specific heat of a solid ... 97 Specific heat of a liquid ... 98 Melting points 89 Heat of fusion of ice ... loi Dew-point 91 Boiling points 90 430 Appendix Text 267 3»3. 313 337 339 344 347 351-355 357 362 375-380 382 394 396, 397 402 404 421 421 426 432 454-456 446 466 468 471 471 475 477 478 4781 485 492, 495 Topic illustrated Manual Heat of vaporization of water . 102 Laws of vibrating strings ... 63 Resonance (velocity ol sound) . 59, 60 Vibration rate of a tuning fork . 62 Pinhole images 64, 65 Photometry 66 Reflection of light 67 Images in plane mirrors .... 69 Concave mirrors . . . . . . 70, 72, 73 Convex mirrors 7i> 73 Index of refraction 74. 75 Convex lens 76, 78, 79 Concave lens 77> 78, 79 The simple microscope .... 80 The telescope 80 Spectra 81 Wave length 82 • The poles of a magnet .... 103 Distribution of magnetic action . 106 Magnetic transparency . . . . 104 Magnetic fields 107 Magnetic eflect of a current . . 109 Electro-motive series . . . . 110 The tangent galvanometer . . . 123, 124 Changeof resistance with temperature 1 20 Electrical resistance 118 The resistance of a cell ....122 Fall of potential along a conductor 125 Resistance of conductors in parallel 119 Electro-motive force of cells . . 126 Use of voltmeter and ammeter . 121 Induced currents 128,129 INDEX The Numbers refer to Pages Aberration, chromatic, 333. spherical, 282, 304. Absolute temperature, 180-181. Absorption, of radiation, 168, 171. selective, 171, 327-329. Acceleration, 71-74- due to gravity, 76-78. Accommodation, power of, 309. Achromatic lens, 334. Action and reaction, 8, 9, 89, 340, 413. Adhesion, 149-150. After-images, 332. Air, buoyancy of, 46-48. composition of, 3. density of, 31. water vapor in, 1 96-197. Air pump, 41-42. Amalgamating zinc, 358. Ammeter, 384. Ampere, 377. Analysis, of light, 322, 327. Angle, critical, 293. of deviation, 284, 291. of incidence and reflection, 269. of refraction, 284. refracting, of prisms, 291. sine of, 286. tangent of, 372. visual, 314. Anode, 408. Antinode, 245. Aperture, of mirror, 274, 282. Arc, electric, 385. Archimedes, principle of, 24, 25. Armature, of dynamos and motors, 398. Artesian wells, 20. Astatic galvanometer, 383. Atmosphere, heating of, 172-173. height of, 23- Atmospheric electricity, 422-425. pressure, 31-36. refraction, 294-296. Attraction, electrostatic, 412. magnetic, 340. molecular, 147. of gravitation, 98-103. Audibility, limits of, 214, 234-235. Aurora borealis, 425. Axis, of lens, 297, 300. of mirror, 274. Balance, 12-13. Balloon, 47. Barometer, 34-36. Battery, see Cells. Beam, of light, 259. Beats, 230-231. Bell, electric, 365. Bellows, 43. Bichromate cell, 359. Bicycle, 134. Boiling, 200-202. Boiling point, 175, 202. Boyle's law, 39-40. Buoyancy, center of, 65. of air, 46-48. V of liquids, 24-25. 431 432 Index Caloric theory, i6l. Calorie, 182. Calorimetry, 182-185, 190, 205. Camera, photographer's, 322. pinhole, 263. Capillarity, 153-155- Cathode, 408. Cells, electric, 354, 357-362. electro-motive force of, 376-377. in battery, 380-382. storage, 410. Center, of buoyancy, 65. of curvature, 274. of gravity, 60-61. Centrifugal force, ^6. Centripetal force, 93-96. Charge, electrostatic, 420. Charles, law of, 179, 181. Chemicar changes, i. effects of electric current, 407-411. energy, 120. Chromatic aberration, 333. scale, 234. Circuit, electric, 357. divided or shunt, 378-379. Clouds, I9'i-I99. Coal, energy of, iii, 120, 210. Cohesion, 147-151. * Coil, induction, 393. Color. 325, 327-333. by interference, 337. Commutator, 397. Compass, 340, 348, 352, ^ Compressibility, of gases, 4, 37-40. of liquids and solids, 4, 140. Compression pump, 43, Condensation, of gases, 205-206. of water vapor, 198-200. Condenser, electric, 420. Conduction, electric, 357. of heat, 164-165.. Conservation, of energy, 132, 209. Convection, of heat, 166. Couple, 58. Critical angle, 293. Crookcs tubes, 422. Current, electric, 354-355. 369-373- chemical effects of, 407-411. extra, 392. first ideas of, 354-355- heating effects of, 385-387. induced, 389-396. magnetic eflects of, 362-365. measurement of, 369-373, 384. unit of, 377. Curvature, center of, 274. Curvilinear motion, 93-^. Dahon's laws, 195. Daniell cell, 362. D'Arsonval galvanometer, 383. Declination, magnetic, 349. Density, 13. and pressure of gases, 40. Deviation, angle of, 284, 291. Dew, 199. Dew-|X)int, 196. Diffusion, of gases, 141-144. of liquids, 145-146. of light, 269-270. Dip, magnetic, 350. Dipping needle, 350. Discord, 232. Dispersion, of light, 322-326. Distillation, 203-204. Divisibility, of matter, 137-138. Ductility, 159. Dynamics, Chap. V. definition of, 49. Dynamo, 396-400. Ear, 249-252. Earth, effect of rotation on its shape, lOI. effect of rotation on weight, 102. magnetic field of, 348-352. revolution and rotation of, 100. Echoes, 225. Eclipses, 261-262. Efficiency, of machines, 132. Index 433 Elasticity, 156-158. Electric, arc, 385. battery, 380-382. bell, 365. cells, 354-355» 357-362. circuit, 357. conduction, 357. current, see Current. discharge, in rarefied gases, 421. energy, 354-355. 387. 389, 392. 399, 401, 402, 407. light, 385-386. measurements, 369-384. motors, 400-402. potential, see Potential. power, 387. resistance, see Resistance. spark, 395. telegraph, 366-369. transmission of power, 402. units, 375, 376, 377, 388. Electricity, Chap. XII. atmospheric, 422-425. •current, 353-4". nature of, 353, 413. static, 411-425. Electrification, by contact, 413. by friction, 412. by induction, 413-414. two states of, 413. Electrodes, 408. Electrolysis, 407-410. Electro-magnet, 364. Electro-magnetic field, 362-364. induction, 389-396. Electro-metallurgy, 409. Electro-motive force, 356. measurement of, 379. of cells, 376-377- uftit of, 376. • Electrophorus, 416. Electroplating, 409. Electroscope, 415. Electrostatic attraction and repulsion, 412. capacity, 419. charge, 420. condenser, 420. field, 415. induction, 413. machines, 415-417. potential, 418. Electrotyping, 408. Energy, Chap. VI. conservation of, 132, 209. dissipation of, 1 21, 223. first ideas of, ii i . forms of, chemical, 120. electrical, 354-35 5» 387. 389. 392, 399,401,402,407. kinetic, in, 116. mechanical, 120. molecular kinetic (heat), 118, 146-147. molecular potential ("latent heat"), 189, 204-205. muscular, 119. of light, 255-258. of sound, 220-223. potential, 118, 1 19, 1 20. radiant, 167-172,255-258. solar, 209-211. sources of, 162-163, 210. transference of, by electric current, 354-355» 402. by machines, 123, 126, 128, 130. conditions necessary for, 112. , two modes of, 255. transformation of, by dombustion, 163. by compression and expansion of gases, 162, 204. by dynamos, 399. by electrical resistance, 387. by friction, 119, 161-162. by fusion and solidification, 189. by motors, 401. by radiation and absorption, 168, 170. 434 Index by steam engine, 213. by vaporization and condensation, 193, 204-207. units of, electrical, 387-388. mechanical, 116. thermal, 182. Engine, steam, 2 12-2 1 3. Equilibrant, 54. Equilibrium, of concurrent forces, 52. of floating bodies, 65-66. of parallel forces, 55-56. of two forces, 49-50. stable, unstable, and neutral, 60- 63. Ether, luminiferous, 256-258, 347, 353. Evaporation, 192. cooling by, 206-207. Expansion, by heat, 141, 176-180. cooling by, 204. force of, 177. Extension, 10. Eye, 306-315. defects of, 310. Falling bodies, 74-79. Faraday, 392. Far sight, 310. Field, electro-magnetic, 362-364. electrostatic, 415. magnetic, 345-347- Field magnet, 399. Floating bodies, buoyancy upon, 24- 25. equilibrium of, 65-66. Fluids, characteristics of, 4-5. Focal length, of lens, 299. of mirrors, 276, 282. Foci, of lenses, 297-300. of mirrors, 276, 279. Fog, 198. Foot-pound, 116. Force, 5-9. buoyant, 24, 25, 46-48. centrifugal, 96. centripetal, 93-96. electro-motive, 356. elements of, 50. graphic representation of, 50. lines of, 345-347- moments of, 57-59. units of, 12. Forces, balanced, 7, 8; Chap. IV. composition of, 51-53,56. concurrent, 51-55. molecular, 147-155. parallel, 55-56. parallelogram of, 52. resolution of, 54. unbalanced, 7, 8; Chap. V. Force pump, 45. Franklin, 422, 423, 425. Fraunhofer lines, 324. Freezing, 186. Freezing mixtures, 191. Freezing point, 1 74. Friction, 6. heating effects of, 119, 161-162. of the air, 74, 75, 78. uses of, 90, 133, 134. Frost, 199. Fulcrum, 123. Fundamental tone, 238, 246-247. Fusion, 186-191. change of volume during, 187. heat of, 189-190. Galilean telescope, 320. Galileo, 76, 79, 92, 320. Galvanometers, 370-373, 383-384. Gases, characteristics of, 3. compressibility of, 4, 39, 40. condensation of, 205-206. cooled by expansion, 204. diffusion of, 141-143. distinguished from vapors, 192. effect of pressure on volume and density of, 39, 40. • effect of temperature on volume, of, 141, 179. Index 435 kinetic theory of 144-145. mechanics of, Chap. III. pressure of, 37-40. Geissler tubes, 421. Glaciers, flow of, 189. Gram, mass and weight, 12. Gram-centimeter, 116. Gravitation, 98-103, 150-151. law of, 98. Gravity, 60. acceleration due to, 76-78. cell, 360. center of, 60, 61. specific, 26-30. Hail, 200. Hardness, 160. Harmony, 232. Hearing, 249-252. Heat, Chap. VHI. conduction of, 164-166. convection of, 166. expansion due to, 141, 176-180. kinetic theory of, 146-147, 161-162. mechanical equivalent of, 208. of fusion, 189-190. of vaporization, 193, 204-205. sources of, 162. specific, 183-184. unit of, 182. Helmholtz, 211, 240. Horse power, 121. Humidity, 197. Hydrostatic press, 21. Ice, 174, 186-190. manufacture of, 207. Illumination, intensity of, 263. Images, by lens, 300-304. by plane mirrors, 271-273. by spherical mirrors, 280-283. by small opening, 262-263. real, 279-281, 300, 302. • virtual, 279-283, 302, 303. Incandescent lamp, 385. Inclination or dip, 350. Inclined plane, 54, 79, 1 14, 131-132. Index of refraction, 287. Induced currents, 389-396. Induction, earth's, 351-352. electro-magnetic, 389-396. electrostatic, 413. magnetic, 342-343. self, 392. Induction coil, 393. Inertia, 5, 87, 89, 95, 96. Insulators, electric, 357. Interference, of light, 337. of sound, 229-231. Iridescence, 337, 338. Joule, 162, 208, 386. Joule's equivalent, 208. law, 386. Kilogram-meter, 116. Kinetic energy, III, Il6. Kinetic theory, of gases, 144, 146- 147. of heat, 146-147, 161-162. Kinetics, see Dynamics. Lamp, arc, 385. incandescent, 385. Lantern, optical, 321. Law, Boyle's, 39-40. Dalton's, 195. Joule's, 386. »f Charles, 179, 181. of gravitation, 98. Ohm's, 370, 377. Pascal's, 20. Laws of motion, Newton's, 91. Leclanche cell, 360. Lenses, achromatic, 334. concave, 305. convex, 296-305. % Lever, 123-126. Leyden jar, 418. Lifting pump, 44. 436 Index Light, Chap. X. dispersion of, 322-326. intensity of, 263-265. interference of, 337.* propagation of, 258-260. reflection of, 268-270. refraction of, 283-292. theory of, 255-260. velocity of, 265-267. wave length of, 259, 325-326. Lightning, 422-423. rod, 423. Lines of force, 345-347- Liquids, characteristics of, 3, 5. diffusion of, 145-146. mechanics of, Chap. IL Liter, 11. Local action in voltaic cell, 358. Lodestone, 339. Loudness of sound, 227. Machines, 123-135. efficiency of, 132. electrical, 415-417. mechanical advantage of, 126. Magdeburg hemispheres, 32. Magnetic action, 340-341, 347. declination, 349. effects of a current, 362-365. field, 345-347- inclination or dip, 350. induction, 342-345. lines of force, 345-347. meridian, 349. needle, 340. permeability, 342. poles, 340. substances, 341. Magnetism, Chap. XL terrestrial, 348-352. Magnetization, permanent and porary, 342-343- theory of, 343-345- Magnets, 338, 342. Magnifying glass, 302, 315-316. tem- Major chord, 234. Malleability, 159. Manometers, 38-39. Mass, detinition of, 11. center of, 60-61. measurement of, by weight, 12, by inertia, 87. units of, 12. Matter, divisibility df, 137. properties of. Chap. VI L states of, 3, 147-148. structure of, 137-147. Measurement, 10-13. Mechanical advantage, 126. equivalent of heat, 208. powers, 123. Mechanics, definition of, 49. of gases. Chap. IIL of liquids. Chap. IL of solids. Chaps. IV, V, VI. Melting, 186. [Celling points, 186. ' effect of pressure on, 1 88. Meter, lo. Microphone, 405-406. Microscope, compound, 316. simple, 302, 315-316. Mirage, 295. Mirrors, parabolic, 282. plane, 271-273. spherical, 274-283. Mobility of fluids, 159. • Molecular forces, 14 7-1 51. motion, 141-147. structure of matter, 137-147. Molecule, 138. Moment of force, 57-59. Momentum, 91. Moon, revolution of, 100. Motion, 68. accelerated, 69, 71-74 curvilinear, 93-96. laws of, '83-92. of falling bodies, 74-78. of pendulum, 104. Index 437 of projectiles, 80-83. on an inclined plane, 79. uniform, 68. wiave, 217-220. Motor, electric, 400-402. Musical, instruments, 242, 246-248. intervals, 231-233. scales, 233-234. sounds, 227. Needle, dipping, 350. magnetic, 340. Newton, 92, 98, 255, 259. Newton's disks, 331. laws of motion, 91. Nodes, 237, 244-245. Noise, 227, 245. Octave, 232. Ohm, definition of, 375. Ohm's law, 370, 377. Opera glass, 321. Optical instruments, 315-322. Organ pipes, 246-247. Overtones, 238, 246-247. Parallelogram of forces, 52. Pascal's law, 20. Pendulum, 104-109. Penumbra, 261. Permeability, magnetic, 342. Photometry, 264-265. Physical changes, i. Pinhole. camera, 263. Pitch, of musical sounds, 214, 227- 229, 234. Plasticity, 149, 158. Polarization, in voltaic cell, 358. Poles, magnetic, 340. of voltaic cell, 355, 358-359- Porosity, 138-139. Potential, electric, 356, 377. of induced currents, 395. of static electricity, 418. Potential energy, 118, 119, 120. Pound, weight and mass, 12. Power, 121. electric transmission of, 402. units of, 121, 387. Pressure, atmospheric, 31-36 of gases, 37-40. of liquids, 15-25. of vapors, 193-195. Pressure gauges, 33-35, 38-39- Prism, 291. Projectiles, 80-83. Properties of matter. Chap. VII. Pulleys, 129-130. Pump, air, 41. compression, 43. force, 45. suction, 44. Quality of sound, 227, 238-240. Radiant energy, 167-172, 255-258. absorption of, 168-169, 171, 172. emission of, 168. luminous and non-luminous, 168, 257. reflection of, 170, 268. selective absorption of, 171,327-329. transmission of, 169, 328-329. Radiometer, 170. Rain, 199. Rainl>ow, 335-336- Ray, of light, 259. Reaction and action, 8, 9, 89, 90, 340, 413. Reflection, of light, 268-283. difi'used, 269-270. of sound, 225. regular, 268-269, 291. total, 292-294. Refraction, 283-292. atmospheric, 294-296. index of, 287. laws of, 286. of different colors, 322-326. relation to velocity, 28S-289. 438 Index Relay, 368. Resistance, electrical, 357. laws of, 374. measurement of, 376. of conductors in parallel, 378. specific, 374. unit of, 375. Resistance coils, 375. Resolution, of a force, 54. of a velocity, 70. Resonance, 243-245. Respiration, 46. Resultant force, 54. velocity, 70. Retina, 307. Rumford, Count, l6l, 265. Scales, musical, 233-234. Screw, 133. Selective absorption, 171, 327-329. Self-induction, 392. Shadows, 260. Short sight, 310. Shunt circuit, 378-379. Sine of an angle, 286. Siphon, 45. Size, angular, 314. Sky, the color of, 330. Snow, 200. Soap bubbles, 152. Solenoid, 364. Solidification, 186-189. Solids, characteristics of, 3, 5. mechanics of. Chaps. IV, V, VI. Solution, heat of, 191. Sonometer, 232. Sound, Chap. IX. intensity of, 220-223. interference of, 229-231. loudness of, 227. media, 216. pitch of, 214, 227-229, 234. properties of, 227. quality of, 227, 238-240. reflection of, 225. sources of, 214. velocity of, 224-225. waves, 218-220, 229. Sounder, telegraph, 366. Speaking tubes, 223. Specific gravity, 26-29. heat, 183-184. resistance, 374. Spectrum, 322-326. invisible, 326. Speed, 68. Spherical aberration, 282, 304. Spyglass, 320. Stability, 64. of floating bodies, 66. Stars, distance of, 267. twinkling of, 294. Static electricity, 411-425; see Elec- trostatic. Statics, of solids, Chap. IV. Steam engine, 212-213. Stereoscope, 313. Stress and strain, 158. Strings, vibration of, 235-240. Sun, energy of, 209-211. Surface tension, 151-153. Sympathetic vibrations, 24^^248. Tangent galvanometer, 370-373. Tangent of an angle, 372. Telegraph, 365-369- Telephone, 404-407. acoustic, 223. Telescopes, 317-321. Temperature, 163-164. absolute, 180. measurement of, 173-176. Tenacity, 148. Terrestrial magnetism, 348-352. Theory, definition of, 145. of electricity, 353,413- of gases, 144-145, 146-147. of heat, 146, 1 61-162, of light, 255-260. of magnetic action, 347. Index 439 of magnetization, 343-345. of the structure of matter, 137-141. Thermometers, 173-176. Thunder, 423. Tone, 233. fundamental, 238, 246. Torricelli, 35. Total reflection, 292-294. Transference of energy, see Energy. Transformation of energy, see Energy. Transformer, 403. Tuning fork, pitch of, 228. vibration of, 215. Umbra, 261. Units, of acceleration, 72. of current strength, 377. of electrical power, 387. of electrical resistance, 375. of E. M. F., 376. of extension, lo-ll. of fluid pressure, 39. of force, 12. of heat, 182. of mass, 1 2. of mechanical power, 1 21. of velocity, 68, 69. of work and energy, 116. Vacuum, 35. Vapor, atmospheric, 196-200. pressure of, 193-195. Vaporization, 192, 198. heat of, 193, 204-205. Vapors, 192. Velocity, 68. graphic representation of, 69. of light, 265-267. of sound, 224-225, 229. resolution of, 70. uniform, 68. variable, 69-74. Velocities, composition of, 69. Vibration, forced and sympathetic, 240-242. of air columns, 243-248. of molecules, 146. of pendulum, 104-105. of strings, 235-240. of tuning fork, 215. Viscosity, 159. surface, 153. Vision, binocular, 311-314. Visual angle, 314. Vocal cords, 253. Voice, 252-254. Volt, definition of, 376. Voltaic cell, 354. Voltmeter, 379, 384, Water, expansion of, 178, 179. Watt, 388. Wave motion, 217. Waves, of light, 257, 259-260, 325- 326. of sound, 218-220, 229. of water, 218. Weather, prediction of, 36. Wedge, 133. Weighing, 12. Weight, 7, II, 102. Welding, 149. Wheel and axle, 127-128. Whistle, 245. Wind instruments, 246-248. Windlass, 128. Work and energy, 311-316. units of, 116. Zero, absolute, 1 80-1 81. THIS BOOK IS DUE uN THE LAST DATE STAMPED BELOW AN INITIAL FINE OF 25 CENTS WILL BE ASSESSED FOR FAILURE TO RETURN THIS BOOK ON THE DATE DUE. THE PENALTY WILL INCREASE TO 50 CENTS ON THE FOURTH DAY AND TO $1.00 ON THE SEVENTH DAY OVEROUe. SE P 13 1934 ACT 19 IS74 17 s^ ¥^ 0^ ^ I,n 21-10O,;i-7.'33 VB ^5Ar ^D4u ^ ^ ^ 6/-" ^^« UNIVERSITY OF CALIFORNIA UBRARY