UNIVERSITY OF CALIFORNIA PUBLICATIONS 
 
 IN 
 
 AGRICULTURAL SCIENCE 
 
 Vol. 3, No. 12, pp. 369-498, 33 text-figs., pis. 43-74 June 30, 1919 
 
 ARE SOILS MAPPED UNDER A GIVEN TYPE 
 
 NAME BY THE BUREAU OF SOILS METHOD 
 
 CLOSELY SIMILAR TO ONE ANOTHER? 
 
 BY 
 
 ROBERT LAKIMORE PENDLETON 
 
 CONTENTS 
 
 PAGE 
 
 Foreword 369 
 
 Introduction 370 
 
 Need of a classification of soils 371 
 
 Historical development of the classification of soils 371 
 
 Plan of the present study 376 
 
 Discussion of results '. 377 
 
 Mechanical analysis 380 
 
 Chemical data 395 
 
 Bacteriological data 414 
 
 Greenhouse data 432 
 
 General discussion 467 
 
 Summary 481 
 
 Appendices 483 
 
 A. Methods and technique 483 
 
 B. Soil sample locations 490 
 
 FOREWORD 
 
 It is due the author, as well as to the undersigned, that a few 
 words be said by way of preparing the reader for what follows in this 
 paper. It will be observed, first, that the manuscript was, for an 
 unusually long time, in the printer's hands. Those who appreciate, 
 as few do today, the great rapidity with which the theories and the 
 methods in soil and plant study change, will readily catch the signifi- 
 cance of the foregoing sentence. Much of the work done by Mr. 
 Pendleton and some of the methods used may now properly be con- 
 sidered obsolete, or, conservatively speaking, at least obsolescent. 
 Nevertheless, I deem it of some importance to give the results obtained 
 in more or less detail, because of their historical value, and because Mr. 
 
370 University of California Publications in Agricultural Sciences [Vol. 3 
 
 Pendleton's residence in India since the paper was written by him 
 has rendered satisfactory changes and deletions practically impossible. 
 Under these circumstances, with the burden of preparing the paper 
 for the press and the reading of the proof falling to me, the author 
 cannot well be held responsible for the inaccuracies and the infelicities 
 of expression which have been carried over from the original manu- 
 script without change. Moreover, the investigation was carried out 
 under my direction, and the plan of attack on the problem, together 
 with the methods employed, were suggested by me. Much that, in the 
 light of present knowledge, is superfluous or patently inexact or 
 erroneous in the paper is due to points of view held by me in 1915, 
 but now happily discarded. For all these, I assume the entire 
 responsibility, and absolve Mr. Pendleton in that regard. 
 
 On the other hand, the work having been carried out at my sugges- 
 tion and under my direction, I feel constrained, in justice to myself, 
 to say that the views expressed in this paper, and the conclusions 
 drawn are wholly Mr. Pendleton's and are not in agreement with those 
 held by me. I fail to see the cogency of the arguments set forth for 
 soil classification and mapping at this juncture in soil studies, and 
 cannot admit the pertinence of the analogy between classification of 
 other objects and of soils which the author of this paper employs. 
 My own general conclusion from the results obtained by Mr. Pendle- 
 ton is that they cast grave doubt on the validity of the Bureau of Soils 
 method of soil classification and mapping, and, incidentally on all 
 methods devised for that purpose to date. I cannot see how such 
 methods can serve us in scientific work at all, and, from the practical 
 standpoint, it would surely seem that guides for the purchaser of land 
 could be arranged more cheaply and less elaborately than by the soil 
 mapping methods extant. This statement has particular reference to 
 the subdivision of types very minutely, such as, for example, sandy 
 silty clay, clay loam adobe, etc. Such minute classification and sub- 
 division in view of the present state of our knowledge of soils, is 
 analogous, in my opinion, to carrying figures out to four decimal 
 places when it is known that the accuracy of the method makes it 
 impossible for them to be correct beyond the first decimal place. In 
 support of this seemingly radical conclusion, the reader will find much 
 of interest in the recent studies of this laboratory on variability in 
 soils, which have already appeared in this same series. 
 
 Chas. B. Lipman. 
 
 INTRODUCTION 
 
 For several years the University of California has been cooperating 
 with the United States Bureau of Soils in the mapping of the soils of 
 the agricultural portions of the State of California. The system of 
 mapping used is that developed by the Bureau of Soils. During the 
 year 1914-1915 the writer, representing the University of California, 
 was engaged in some of this soil survey work. In that year, in the 
 field, many questions arose regarding the criteria used, the methods. 
 
1919] Pendleton: A Study of Soil Types 371 
 
 and the results of the scheme of mapping. It was thought that pos- 
 sibly some of the many questions could be answered through a labora- 
 tory study of some typical soils. This paper is a description of cer- 
 tain parts of the Avork done in this connection. 
 
 THE NEED OP A CLASSIFICATION OF SOILS 
 
 Since soils consist of a number of more or less distinct groups they 
 are fitting subjects for classification. In fact, it is my belief that it 
 is as necessary to have a classification for soils as for any other group 
 of natural objects in order that "the various and complex relations 
 may be shown as far as practicable," 1 and that there be a definite 
 basis for systematic and thorough investigations. 2 The advantages of 
 a classification of soils are apparent. But because soils grade gradu- 
 ally into one another, rather than exist as discrete individuals which 
 can be more easily considered and treated from a systematic stand- 
 point, the problem of evolving a satisfactory classification has been 
 particularly difficult. The many and diverse classifications proposed, 
 and the difficulty of applying many of these classifications under con- 
 ditions other than those for which they were evolved, testify to the 
 difficulty of the task in question. 
 
 The mapping of soils without a classification is impossible, and 
 so a brief summary of the development of soil mapping will bear a 
 close relation to the development of soil classification. 
 
 HISTORICAL DEVELOPMENT OF THE CLASSIFICATION 
 
 OF SOILS 
 
 The early history of the making of soil maps is that of geologic 
 maps as well, when soils, from the agricultural standpoint, and the 
 less distinct geological formations as such, were not sharply distin- 
 guished. Blanck 3 has an excellent treatment of the development of 
 soil mapping and of the modern continental European conceptions of 
 the nature and significance of soil maps. According to Blanck the 
 earliest record of a proposal to make a map to show something of the 
 nature of the actual material composing the surface of the earth is 
 that of Lister's proposal, in 1683, to the Royal Society of London. 
 
 i Coffey, G. N., Proc. Amer. Soc. Agron., vol. 1 (1909), p. 175. 
 2 Cameron, F. K., Eighth Internat. Cong. Chem., vol. 26 (1912), sees, via-xib; 
 app. pp. 699-706. 
 
 sFuhling, Landw. Ztg., vol. 60 (1911), pp. 121-45. 
 
372 University of Calif ornia Publications in Agricultural Sciences [Vol. 3 
 
 But it was not until 1743 that Packe executed a map of Kent, showing 
 the occurrence of minerals by symbols. Apparently the next advance 
 was by the Germans, when Fuchsel, 1773, and Gloser, 1775, first used 
 colors to show granite, limestone, etc. This work constituted the first 
 real geologic map in the modern sense. There was not much activity 
 in this line of geologic work until 1870 or later. Such activity as there 
 was showed a lack of emphasis on soils in the agricultural sense of 
 the term. 
 
 The work on the geologic drifts of northern Europe, and studies of 
 the more recent lowland formations and soils of Germany led to soil 
 mapping. The first real soil map, according to Blanck, was prepared 
 by Benningsten-Forder of Halle, in 1864-67 ; while Carnot 4 states 
 that in 1863 M. Scipion Gras used superposable maps of the Depart- 
 ment of Isere, showing (1) geology, (2) agricultural soils, (3) alti- 
 tudes of agricultural regions, and (4) culture. The first true geologic- 
 agronomic map published by the Preussischegeologische Landesan- 
 stalt appeared in 1878. 
 
 The school of soil classification and mapping just mentioned, using 
 the geologic maps and methods as a point of departure have evolved 
 numerous though similar systems of recording the agrogeologic data 
 on the map. The geologic formation is shown by the color, and the 
 soil textures by sjmibols, while one or more of the following groups 
 of data appear and may be shown : topography by contours, subter- 
 ranean water by blue figures, location of borings in red with figures 
 referring to tables, amount of plant food elements or substances by 
 figures or hatchings, varying directions, color, or nature of lines, etc. 
 The nature and amount of the data shown and the manner of repre- 
 senting them vary a great deal. Some soilists, to use a term proposed 
 by Coffey, 5 advocate and use superposable maps to show one or more 
 groups of data, thus avoiding unnecessary confusion on the main map. 
 
 Hazard proposed a scheme of classification which is quite as 
 directly connected with the economic factors controlling the crops 
 grown, and with the assessable valuation of the land, as with the 
 actual or potential fertility of the soil itself. There are several classi- 
 fications of this type, involving the assessable values of the land. 
 
 i Rapport BUT Les cartes agronomiques, Bull. Min. Agr. France, 1893, no. 8, 
 pp. 956 73. 
 
 • r > Jour. Amor. Soc. Agron., vol. 8 (1916), p. 239. 
 
 eLandw. Jahrb., vol. 29 (1900), pp. 805-911. 
 
 Gregoire, A., and Halet, F., Bull. Inst. Chem. et Bact. Gembloux, 1906, no. 75, 
 pp. 1-43. 
 
1919] Pendleton : A Study of Soil Types 373 
 
 This development of the mapping of soils as an outgrowth of areal 
 geology in France and Germany may be contrasted with the develop- 
 ment of soil classification from other viewpoints, such as that of the 
 Russian school. In Russia there is not the predominance of residual 
 and shallow soils which characterize much of western Europe and 
 which in France especially have led to the adoption of the geologic 
 basis of classification. Dokoutchayev and Sibirtzev have been the 
 chief proponents of a classification of soils based upon the ' ' conception 
 of a soil as a natural body having a definite genesis and a distinct 
 nature of its own. ' ' r 
 
 The genetic conditions of the formation of natural soils include 
 the following variable factors which cause variation : 
 
 (1) The petrographic type of the parent rock; (2) the nature and intensity of 
 the processes of disintegration, in connection with the local climatic and topo- 
 graphic conditions; (3) the quantity and quality of that complexity of organisms 
 which participate in the formation of the soil and incorporate their remains in it ; 
 (-4) the nature of the changes to which these remains are subjected in the soil, 
 under the local climatic conditions and physico-chemical properties of the soil 
 medium; (5) the mechanical displacement of the particles of the soil, provided 
 this displacement does not destroy the fundamental properties of the soil, its geo- 
 biological character, and does not remove the soil from the parent rock; and (6) 
 the duration of the processes of soil formation. 
 
 Upon this genetic basis there has been developed a series of soil zones, 
 ranging from the laterite soils in the tropics to the tundras in the 
 Arctic regions. The outstanding and controlling factor in the scheme 
 proposed is the relation of these zones to climate. For this reason the 
 statement usually seen is that climate is the basis of the classification. 8 
 There are nearly as many groups of intra-zonal and azonal soils as 
 of those belonging to the zones proper. The former include alkali, 
 marshy, alluvial, and other soils. 
 
 Hilgard, while actively interested in the' genetic viewpoint of soil 
 classification, was the foremost proponent of a classification upon 
 the basis of the natural vegetation growing upon the soil. 9 This 
 criterion is not always available, though some groups of plants, as the 
 alkali tolerant ones, are almost invariably present where the condi- 
 
 <Exp. Sta. Record, vol. 12 (1900), p. 704. 
 
 See also Sibirtzev, Cong. Geol. Intern., 1897, pp. 73-125; abstract in Exp. Sta. 
 Eec. vol. 12 (1900-01), pp. 704-12, 807-18. 
 
 Tulai'koff, X., The Genetic Classification of Soils, Jour. Agr. Sci., vol. 3 (1908), 
 pp. 80-85. 
 
 s Coffey, U. S. Bur. Soils, Bull. 85 (1912), p. 32; Jour. Amer. Soc. Agron., 
 vol. 8 (1916), p. 241. 
 
 9 Hilgard, E. W., Soils (New York, Macmillan, 1906), pp. 487-549. 
 
374 University of California Publications in Agricultural Sciences [Vol. 3 
 
 tions are unfavorable for the less resistant plants. Later Hilgard 
 and Loughridge 10 claimed that it is impracticable to attempt "a sat- 
 isfactory tabular classification in which each soil shall at once find its 
 pigeonhole prepared for it . . . because the subject matter is as yet 
 so imperfectly known. ' ' However, this does not dispute the justifica- 
 tion for making classifications for specific purposes or of specific 
 regions. With respect to this point there seems to be confusion. The 
 question is not whether soils can be classified at all or not, for every 
 observant farmer classifies the soil with which he is familiar, but 
 whether a satisfactory classification is possible over a large territory, 
 where soils are subject to the varying action of the important soil 
 forming agencies. 
 
 Still another type of soil mapping is that of Hall and Russell, 
 which is given in their admirable Report on the Agriculture and Soils 
 of Kent, Surrey, and Sussex." 11 In this district the soils are largely 
 residual, and form quite distinct groups, depending upon the parent 
 geologic formation. These groups of soils, such as the Clay-with- 
 flints and the Thanet beds, have very definite agricultural properties ; 
 hence the treatment of all phases of agriculture upon each separate 
 group of soils. Hall and Russell 12 present an excellent discussion of 
 the methods of soil classification and the interpretation of the soil 
 analyses used in their study. Russell 13 gives a very similar though 
 briefer treatment. 
 
 There are other more or less specialized classifications that have 
 been applied to local conditions and problems. As an example may 
 be cited Dicenty's work on grape soils. 14 
 
 Various modifications of the above schemes of classifying and map- 
 ping soils are found in general texts on soils. 15 Nowacki 16 proposes a 
 curious system, Genera et Species Terrarum. It is in Latin terminology. 
 The genera are based on the quality of the soil, whether stony, sandy, 
 clayey, peaty, etc., and the species are dependent upon the quantities 
 of organic matter and clay. 
 
 10 The Classification of Soils, Second Intern. Agrogeol. Conf., Stockholm, 1910, 
 p. 281. 
 
 ii London, Bd. Agr. and Fish., 1911. 
 
 12 Jour. Agr. Science, vol. 4 (1911), pp. 182-223. 
 
 is Soil Conditions and Plant Growth (London, Longmans, 1913), pp. 132-48. 
 
 14 Die ampelogeologische Kartierung. First Intern. Agrogeol. Cong., Budapest, 
 1909, pp. 257-71. 
 
 '■"• Ramann, E., Bodenkunde, Berlin, Springer, 1911. 
 Mitscherlich, E. A., Bodenkunde, Berlin, Parez, 1905. 
 i« Praktwche Bodenkunde (Berlin, 1892), pp. 130-80. 
 
1919] Pendleton: A Study of Soil Types 375 
 
 Soil Surveying in the United States. — In a brief way, it has been 
 shown how there arose the different systems of soil classification. 
 Only a few typical systems of classifications, and something of the 
 reasons for the divergences, have been mentioned. 17 Probably the one 
 agency that has carried on the most extensive soil classification and 
 mapping is the Bureau of Soils of the United States Department of 
 Agriculture. It is now proposed to discuss and in a measure criticize 
 the work of the Bureau of Soils, the one organization that has, more 
 than any other, succeeded in applying a detailed system of soil classi- 
 fication over extensive areas. 
 
 The problems that the Bureau had to face during its early exist- 
 ence were special studies of the soils of certain crops, especially of the 
 tobacco districts. 18 Later the soil utilization work of the Bureau of 
 Soils was transferred to other branches of the Department of Agri- 
 culture, leaving as the main task for the Bureau the systematic classi- 
 fication and mapping of the soils of the United States. 
 
 Coffey 19 has so well discussed the present day conceptions of the 
 bases for the classification of soils, that it does not seem necessary to 
 repeat any portion of that excellent statement here. He showed that 
 the Bureau of Soils, in its method of classifying soils, uses a combina- 
 tion of a number of systems. This matter is dealt with more in detail 
 in an article b} r Coffey, 20 and the Report of the Committee on Soil 
 Classification of the American Society of Agronomy. 21 The question 
 often arises as to the validity of making the close distinctions regard- 
 ing color, texture, geologic origin, etc., and is one which should be 
 dealt with in order to render less empirical the nature of most of the 
 criteria which are used at present. See the Report of the Committee 
 on Soil Classification and Mapping. 22 
 
 Because of different views regarding soils and soil fertility from 
 those held by the Bureau of Soils, the Illinois Agricultural Experi- 
 ment Station has undertaken a soil survey and classification, under the 
 direction of Dr. C. G. Hopkins, which is independent of the Bureau 
 
 17 See Coffey's excellent treatment of the soil survey work in this country. 
 The Development of Soil Survey Work in the United States with a Brief Reference 
 to Foreign Countries, Proc. Amer. Soc. Agron., vol. 3 (1911), pp. 115-29. 
 
 is Whitney, Extension and Practical Application of Soil Surveys, Off. Exp. 
 Sta., Bull. 142 (1903), pp. 111-12; The Purpose of a Soil Survey, U. S. Dept. 
 Agr., Yearbook, 1901, pp. 117-32. 
 
 is A Study of the Soils of the United States, U. S. Bur. Soils, Bull. 85 (1912), 
 pp. 24-38. 
 
 20 Jour. Amer. Soc. Agron., vol. 8 (1916), pp. 239-43. 
 2i Ibid., vol. 6 (1914), pp. 284-88. 
 22 Ibid., vol. 8 (1916), pp. 387-90. 
 
376 University of California Publications in Agricultural Sciences [Vol. 3 
 
 of Soils, and differs from its methods in a number of ways. Since the 
 soils of Illinois are of a much narrower range of variation than are 
 those of the whole of the United States, the system of classification 
 for the state need not be so elaborate. The soils are divided accord- 
 ingly as they have been glaciated or not, and if glaciated, in what glaci- 
 ation period. They are further divided according to color, topogra- 
 phy, and texture of soil and subsoil. 23 Correlation of the types of 
 soil mapped in the various areas, one of the greatest sources of criti- 
 cism of the Bureau of Soils survey methods, is more easily handled 
 in the Illinois work, since it is possible for the one in charge of the 
 work to pass personally, while in the field, upon all correlation and 
 the establishment of all new types. It is insisted that the field men 
 map accurately and in sufficient detail. This insures the accuracy of 
 the maps as regards the standards adopted, the information is specific, 
 and the local users of the maps are not misled. 24 In connection with 
 the field classification and mapping, pot and plot cultures are carried 
 on, not so much to test the relative fertility of the untreated soils, but 
 to determine the effects of the application of various sorts and quanti- 
 ties of fertilizers. Hopkins, 25 to show the differences in detail between 
 the U. S. Bureau of Soils mapping and that of the Illinois Experi- 
 ment Station, compares a U. S. Bureau survey of 1902 with a state 
 survey published in 1911. This is not entirely fair, because with the 
 increase of field knowledge of soils gained by them and the realiza- 
 tion of the need of representing the soils in more detail, a survey 
 made by the Bureau in 1911 would almost certainly show much more 
 detail and show it with greater accuracy than the maps made in the 
 early period of the work. This point may be strengthened by the 
 notes given below on the comparison of a portion of an early survey 
 made in southern California by the Bureau of Soils with a recent 
 survey of the same soils made by the Bureau and the University of 
 California working in cooperation. 
 
 PLAN OF THE PRESENT STUDY 
 
 The present study is an attempt to see if certain soil types mapped 
 as the same from different areas in the state of California, and judged 
 to be the same by the criteria used by the Bureau of Soils, are the 
 
 28 Hopkins, Soil Fertility and Permanent Agriculture (Boston, Ginn, 1910) 
 pp. 54-57. 
 
 24 Ibid., ]>. 115. 
 
 28 Jbid., pp. 114-15. 
 
1919] Pendleton: A Study of Soil Types 377 
 
 same or similar when examined from the laboratory standpoint. For 
 example, we may take the Hanford fine sandy loam, which is one of 
 the types that has been used in the present study. According to the 
 criteria of color, mode of formation, origin (as judged by the presence 
 of mica), nature of subsoil, texture, etc., this soil has been found and 
 mapped in a number of areas that have been mapped in this state. 
 But will these various bodies of soil, from widely separated portions 
 of the state, when judged by laboratory and greenhouse studies on 
 samples as nearly representative as possible, appear to be the same or 
 similar ? 
 
 The types selected for such a study as this should fulfil the follow- 
 ing conditions : first, they should have at least a reasonably wide dis- 
 tribution in the state so as to have been mapped in a number of differ- 
 ent soil survey areas ; and second, the several types should be repre- 
 sentative of different classes of soils (clays, loams, sandy loams, etc.), 
 so that contrasts could be obtained between the types. 
 
 In the collection of samples it was aimed to obtain representative 
 samples from each of a number of bodies of soil of the types selected ; 
 not to obtain possible variations from the ideal in any one body. In 
 the laboratory the soils were compared with regard to their physical 
 composition in the surface horizon, to their chemical composition in 
 three horizons, and to their relative bacteriological activities. In the 
 greenhouse the soils (surface horizon only) were placed in large pots 
 and their comparative ability to produce various crops was studied. 
 
 No claim is made that these criteria should be the ones used in 
 determining the systematic classification of soils or in determining 
 the relative fertility of the soils. They were merely used to determine 
 how nearly the soils classed under a given type name agree from the 
 standpoints named. 
 
 DISCUSSION OF RESULTS 
 
 The bacteriological and chemical determinations were run in dupli- 
 cate so that the figures presented are averages. It is considered that 
 this gives fairer figures for comparison, especially since the determina- 
 tions were run on separate samples, and not on aliquots of a single 
 solution from a single sample. 
 
 There is a very important factor which should always be kept in 
 mind especially when considering the bacteriological and greenhouse 
 comparisons. This is the factor of the probable error. Though the 
 
378 University of California "Publications in Agricultural Sciences [Vol. 3 
 
 advisability of judging all results in the light of the probable error 
 is admitted, no attempt has been made to apply this factor to the 
 results reported in this paper. As the result of the effect which such 
 a factor might have upon the results of bacteriological determina- 
 tions carried on only in duplicate, or upon the results of greenhouse 
 work done in triplicate, one hesitates to draw conclusions, especially 
 those based upon minor variations. Hence in this work only the more 
 marked results will be considered of significance. 
 
 When planning the work it was thought that three or four samples 
 of a type would be enough to show whether or not a given type was 
 approximately uniform, or widely variable, and as to whether the 
 types were similar to one another, or quite dissimilar. But it now 
 seems, after comparing the determinations run on the larger number 
 of samples of the Hanford and San Joaquin types, 9 and 8 respec- 
 tively, with the determinations run on the Altamont and Diablo types, 
 of which there were a much smaller number of samples, 3 and 4 
 respectively, that the larger series gives a much better insight into the 
 variations of a given type and affords a much better basis for con- 
 clusions. 
 
 Hence, as regards the laboratory work thus far carried out, the 
 emphasis has been placed upon the Hanford fine sandy loam and the 
 San Joaquin sandy loam. Determinations have not been completed 
 on the Altamont and Diablo series to the extent that they have on the 
 former two. 
 
 It is of no little significance that the Hanford fine sandy loam and 
 the San Joaquin sandy loam are very widely contrasted soils agricul- 
 turally. The Hanford is typical of good recent alluvial soil in this 
 state ; while the San Joaquin is typical of wide expanses of ' ' old valley 
 filling" soils that are considered poor as regards crop producing 
 power and are underlain by compact iron-cemented hardpan. Conse- 
 quently, the results of comparing soils so different from an agricul- 
 tural point of view, and so radically different as regards soil survey 
 criteria (though the textures are quite similar) will be of considerable 
 interest. They are of greater interest than the comparisons between 
 the Diablo and Altamont soils, as the latter are quite similar in agri- 
 cultural value and use, as well as in field appearances. Between the 
 Diablo or Altamont and the Hanford or San Joaquin one cannot 
 judge as closely regarding variations, for the soils are so radically 
 different. On the other hand, one can compare the soils of the heavy 
 and light types to see to what extent the chemical and bacteriological 
 results differ as compared with the physical results. 
 
02.5 0.5 /. Z. 4 9. 16. 32. 64. Grits. 
 
 Size of Particles nam - 
 
 Fig. 1. Graph showing the results of the Hilgard elutriator method of 
 mechanical analysis on the four samples of Diablo clay adobe. 
 
380 
 
 University of California Publications in Agricultural Sciences [Vol. 3 
 
 Mechanical Analysis 
 
 Hilgarcl Elutriator Method. — That there is a wide variation be- 
 tween the samples is apparent (figs. 1-4). In fact, there is about 
 as wide a range of differences among the samples of the Hanford 
 
 % 
 
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 40 
 
 35 
 
 30 
 
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 32 
 
 64 m m. 
 
 Pig. 2. Graph showing the results of the Hilgard elutriator method of 
 mechanical analysis on the three samples of Altamont clay loam. 
 
 fine sandy loam and among those of the San Joaquin sandy loam as 
 between the two types. The most outstanding differences are where 
 they ought to be, to show the differences that the type names presup- 
 pose, i.e., in the "coarse sand" (64 mm.) and the "grits." The sam- 
 ples of the San Joaquin sandy loam average a larger proportion of 
 each of these separates than do the Hanford fine sandy loam soils. 
 
1919] 
 
 Pendleton : A Study of Soil Types 
 
 381 
 
 In the Hanford, no. 14 is notably heavier than the others, as shown 
 by its silt content, which is nearly half again as great as that of the 
 next highest sample. 
 
 The gravel content (sizes above 2 mm.) is interesting in its uni- 
 formity. In the San Joaquin soils the two samples above 1% are 
 
 :lqy Q25 0.5 I 2. 4- 8 16 32 64- Grits 
 
 Size of Particles. mm 
 
 Fig. 3. Graph showing the results of the Hilgard elutriator method of 
 mechanical analysis on the eight samples of San Joaquin sandy loam. 
 
 nos. 11 and 26. The material in the latter soil is composed almost 
 wholly of iron concretions, leaving sample no. 11 as the only soil with 
 more than 1% actual gravel. In the Hanford samples none were 
 found to have more than 1.5% gravel. 
 
 The Hilgard method does not include any precise subdivision of 
 the soils into groups or classes according to texture. Dr. Hilgard was 
 not in favor of making the fine distinctions in texture that other 
 
382 
 
 University of California Publications in Agricultural Sciences [Vol. 3 
 
 investigators have emphasized. But if there were such a scheme, 
 similar to that which the Bureau of Soils uses, 26 it would be an easy 
 matter to compare the results obtained through the use of the elutri- 
 ator, and determine whether or not the soils examined belong to a 
 given class. The simple comparison of the quantities, in different 
 
 40% 
 
 0^5~ 0.5 1.0 2.0 4.0 8.0 16. 32. 64-. Grits. 
 
 Size of Particles. mm. 
 
 Fig. 4. Graph showing the results of the Hilgard elutriator method of 
 
 mechanical analysis on the nine samples of Ilanford fine sandy loam. 
 
 samples, of any given separate or separates is not absolute. For it 
 must be realized that the conception of a soil class includes a certain 
 range in the quantities of particles of the various sizes. This must 
 be so since soils are ordinarily grouped into but ten or twelve class 
 textures, while there exist among soils those with all gradations in 
 the quantities of particles of the various sizes. 
 
 28 Instructions to Field Parties, U. S. Bur. Soils, Bull. 1914, p. 75; ibid., 
 Bull. 85 (11)12;, p. 28. 
 
1919] 
 
 Pendleton: A Study of Soil Types 
 
 383 
 
 And because the ranges in the sizes of the soil particles separated 
 by the Bureau of Soils method cut across those of the Hilgard 
 method, it is impossible to regroup the results so that the Bureau of 
 Soils grouping into textures may be applied. But without any such 
 scheme, desirable as it may be, it has been pointed out that there is 
 clearly apparent a rather wide variation in the analyses of the several 
 samples of a type. All the soils representative of a given type are by 
 no means closely similar to one another. 
 
 Table 1 — Comparison of Textures 
 
 Texture determined by 
 
 Texture as judged in the field 
 
 mechanical analysis 
 
 *1 
 
 Diablo clay adobe 
 
 Clay 
 
 2 
 
 Diablo clay adobe 
 
 Clay 
 
 3 
 
 Altamont clay loam 
 
 *Silty clay 
 
 4 
 
 Altamont clay loam 
 
 Clay loam (sandy) 
 
 5 
 
 Diablo clay adobe 
 
 Clay 
 
 6 
 
 Diablo clay adobe 
 
 Clay 
 
 7 
 
 Altamont clay loam 
 
 Clay loam (heavy) 
 
 10 
 
 San Joaquin sandy loam 
 
 *Fine sandy loam 
 
 11 
 
 San Joaquin sandy loam 
 
 Sandy loam (heavy) 
 
 12 
 
 San Joaquin sandy loam 
 
 *Fine sandy loam 
 
 13 
 
 San Joaquin sandy loam 
 
 *Fine sandy loam (heavy) 
 
 14 
 
 Hanford fine sandy loam 
 
 Fine sandy loam (loam) 
 
 15 
 
 Hanf ord fine sandy loam 
 
 Fine sandy loam 
 
 16 
 
 Hanford fine sandy loam 
 
 * Sandy loam 
 
 17 
 
 San Joaquin sandy loam 
 
 Sandy loam 
 
 18 
 
 San Joaquin sandy loam 
 
 Sandy loam 
 
 19 
 
 Hanford fine sandy loam 
 
 * Sandy loam (heavy) 
 
 20 
 
 Hanford fine sandy loam 
 
 Fine sandy loam 
 
 21 
 
 Hanford fine sandy loam 
 
 Sandy loam 
 
 22 
 
 Hanford fine sandy loam 
 
 Fine sandy loam 
 
 23 
 
 Hanford fine sandy loam 
 
 Fine sandy loam 
 
 24 
 
 Hanford fine sandy loam 
 
 Fine sandy loam 
 
 25 
 
 Hanford fine sandy loam 
 
 Fine sandy loam 
 
 26 
 
 San Joaquin sandy loam 
 
 Sandy loam 
 
 Note. — Textures not judged correctly in the field. 
 
 Mechanical Analysis by the Bureau of Soils Method. — Among the 
 other determinations made by the Division of Soil Technology on the 
 surface horizons of the twenty-four soils used in this investigation 
 was that of making the mechanical analysis. The tables show the 
 percentages of the several separates. In all cases the figures represent 
 averages of duplicate determinations and in some cases the averages 
 of quadruplicate determinations. With this method, as well as with 
 the Hilgard elutriator, there are shown wide variations between the 
 
384 University of California Publications in Agricultural Sciences [Vol. 3 
 
 .005 .005 .05 JO .25 .5 1.0 
 mm. -.05 -JO -£5 -.5 -/.Q -2.0 
 
 miD. mm. mm. mm. mm. mm. 
 
 Pig. 5. Graph showing the results of the Bureau of Soils method of 
 mechanical analysis on the four samples of Diablo clay adobe. 
 
1919] 
 
 Pendleton: A Study of Soil Types 
 
 38: 
 
 samples of a given type. But the graphs of the percentages (figs. 
 5-8), determined by the Bureau of Soils method for the several types 
 are not as closely similar as the graphs of the elutriator results for 
 the same types. That is, using the Bureau of Soils method, the graph 
 of the Hanford fine sandy loam does not resemble th,at of the San 
 Joaquin sandy loam as much as do the graphs of the results made 
 
 Fig. 6. 
 
 .005 .005-.05 .05-. 10 .10-. 25 .25-. 5 .5-1.0 1.-2. 
 
 Graph showing the results of the Bureau of Soils method of 
 
 mechanical analysis on the three samples of Altamont clay loam. 
 
 upon the same soils by the Hilgard elutriator method. This would 
 lead one to believe that the Bureau of Soils method of mechanical 
 analysis is the better suited for separating soils into groups; even 
 though these soils which were classified in the field according to the 
 differences which are the more prominent would be expected to show 
 greater differentiations when examined by the Bureau of Soils labora- 
 tory methods. 
 
386 
 
 University of California Publications in Agricultural Sciences [Vol. 3 
 
 Comparison of Textures. — Table 1 gives the texture as shown on 
 the soil survey map of the locality, as well as the results of the labora- 
 tory check. This texture as given on the map was also judged by me 
 
 .005 .005 .05 .10 25 
 -.05 -./O -Z5 -.5 
 Size of Particles. 
 
 Pig. 7. Graph showing the results of the Bureau of Soils method of 
 mechanical analysis on the eight samples of San Joaquin sandy loam. 
 
 in the field to be more or less true to the type as mapped. I say more 
 or less true, for the field notes, as given in appendix B, show that in 
 several cases I was unable to obtain in the locality what I believed to 
 
1919] 
 
 Pendleton: A Study of Soil Types 
 
 387 
 
 be a sample of the soil thoroughly typical of the class and type in 
 question. Sample no. 3 had a large lime content which I thought 
 might more or less obscure the texture. ''Slightly heavy, and barely 
 enough sand for a sandy loam" is the comment on sample 12, while 
 "a heavy sandy loam, approaching a loam" is found in the notes on 
 sample 13. The second column of the table shows the class sub- 
 divisions into which the soils were placed according to the mechanical 
 analysis. The words in parenthesis show modifying conditions but 
 do not indicate a change in the class. In considering the class groups 
 such as sandy loam, fine sandy loam, etc., it should be remembered 
 that though the groups are rather broad, the limits are arbitrary 
 and quite sharp. So the results of a mechanical analysis may place 
 a soil in the sandy loam class if 25% or more is fine gravel, coarse and 
 medium sand, while if less than 25% be present the soil belongs to the 
 fine sandy loam class, providing at the same time the amounts of silt, 
 clay, and fine sand are within the specified limits. The two soils may 
 be a great deal alike in texture though placed in different classes. 
 The failure of my judgment regarding the texture shows one of the 
 difficulties that the field man is continually facing. And his failure 
 to judge textures correctly is one of the causes of criticism of soil 
 survey work. 
 
 Table 2 — Mechanical Analyses, 
 
 HlLGARD ELUTRIATOR METHOD 
 
 
 
 Diablo Clay Adobe 
 
 
 
 
 
 Separates 
 
 
 
 Samples 
 
 
 r 
 
 Diameter, 
 mm. 
 
 Velocity, 
 
 mm. per 
 
 second 
 
 
 Name 
 
 1-A 
 
 % 
 
 2-A 
 
 % 
 
 5-A 
 
 % 
 
 6-A 
 
 % 
 
 Clay 
 
 .01 
 
 0.25 
 
 44.16 
 
 35.81 
 
 44.97 
 
 64.63 
 
 Fine silt 
 
 .01 -.016 
 
 0.25 
 
 23.91 
 
 34.08 
 
 25.57 
 
 25.13 
 
 Medium silt 
 
 .016-.025 
 
 0.5 
 
 5.97 
 
 7.37 
 
 4.14 
 
 1.03 
 
 
 .025-.036 
 
 1 
 
 8.10 
 
 9.09 
 
 5.28 
 
 1.83 
 
 Coarse silt 
 
 .036-.047 
 
 2 
 
 7.77 
 
 7.47 
 
 5.45 
 
 1.99 
 
 
 .047-.072 
 
 4 
 
 6.05 
 
 4.09 
 
 6.18 
 
 2.13 
 
 Fine sand 
 
 .072-.12 
 
 8 
 
 3.28 
 
 1.33 
 
 5.81 
 
 2.07 
 
 
 .12 -.16 
 
 16 
 
 0.48 
 
 0.43 
 
 1.73 
 
 0.90 
 
 Medium sand 
 
 .16 -.30 
 
 32 
 
 0.08 
 
 0.21 
 
 0.38 
 
 0.21 
 
 Coarse sand 
 
 .30 -.50 
 
 64 
 
 0.18 
 
 0.11 
 
 0.49 
 
 0.11 
 
 Total weight 
 
 of separates, gm. 
 
 
 19.18 
 
 19.62 
 
 19.30 
 
 19.68 
 
 Weight of original sample, gm. 
 
 
 18.83 
 
 18.88 
 
 18.66 
 
 18.16 
 
 Grits, % 
 
 0.5-2.0 mm. 
 
 
 0.26 
 
 0.29 
 
 0.57 
 
 0.10 
 
 Hygroscopic 
 
 moisture, % 
 
 
 6.20 
 
 5.93 
 
 7.18 
 
 10.12 
 
University of California Publications in Agricultural Sciences [Vol. 3 
 
 .005 .005 .05 JU .25 .5 1.0 mm 
 
 -.05 , -.1.0 -Z5 -.5 -1.0 2.0 mm. 
 
 Size of Particles 
 
 Pig. 8. Graph showing the results of the Bureau of Soils method of 
 mechanical analysis on the nine samples of llnnford fine sandy loam. 
 
1919] 
 
 Pendleton: A Study of Soil Types 
 
 389 
 
 Table 3 — Mechanical Analyses, Hilgard Elutriator Method 
 
 Allamont Clay Loam 
 Separates 
 
 ' 
 
 Diameter 
 mm. 
 
 Velocity 
 mm. per 
 second 
 
 
 A 
 
 
 Name 
 
 3 -A 
 
 % 
 
 4-A 
 
 % 
 
 7-A 
 % 
 
 Clay 
 
 .01 
 
 0.25 
 
 28.48 
 
 26.41 
 
 22.65 
 
 Fine silt 
 
 .01 -.016 
 
 0.25 
 
 43.42 
 
 17.73 
 
 41.18 
 
 Medium silt 
 
 .016-.025 
 
 0.5 
 
 2.96 
 
 2.39 
 
 4.67 
 
 
 .025-.036 
 
 1 
 
 4.37 
 
 4.82 
 
 8.51 
 
 Coarse silt 
 
 .036-.047 
 
 2 
 
 4.95 
 
 4.89 
 
 6.01 
 
 
 .047-.072 
 
 4 
 
 5.52 
 
 7.52 
 
 7.90 
 
 Fine sand 
 
 .072-.12 
 
 8 
 
 5.14 
 
 8.83 
 
 5.54 
 
 
 .12 -.16 
 
 16 
 
 3.89 
 
 13.61 
 
 1.98 
 
 Medium sand 
 
 .16 -.30 
 
 32 
 
 0.88 
 
 10.40 
 
 0.95 
 
 Coarse sand 
 
 .30 -.50 
 
 64 
 
 0.21 
 
 3.39 
 
 0.61 
 
 Total weights 
 
 of separates, 
 
 gm. 
 
 18.71 
 
 19.54 
 
 20.96 
 
 Weight of ori 
 
 ginal sample, 
 
 gm. 
 
 18.50 
 
 19.16 
 
 19.21 
 
 Grits, % 
 
 .5-2.0 mm. 
 
 
 3.98 
 
 8.09 
 
 1.63 
 
 Hygroscopic moisture, % 
 
 
 8.08 
 
 4.37 
 
 4.09 
 
 Table 4 — Mechanical Analyses, Hilgard Elutriator Method 
 San Joaquin Sandy Loam 
 
 
 Separates 
 
 
 
 
 
 Sampl 
 
 es 
 
 
 
 
 
 Diameter 
 t mm. 
 
 Velocity, 
 
 mm. 
 
 per 
 
 second 
 
 
 Name 
 
 10-A 
 
 % 
 
 ll-A 
 
 % 
 
 12-A 
 
 % 
 
 13-A 
 
 % 
 
 17-A 
 
 % 
 
 18-A 
 
 % 
 
 21-A 
 
 % 
 
 2 6- A 
 
 % 
 
 Clay 
 
 .01 
 
 0.25 
 
 11.14 
 
 15.46 
 
 8.99 
 
 10.75 
 
 10.53 
 
 8.72 
 
 8.35 
 
 16.64 
 
 Fine silt 
 
 .01 -.016 
 
 0.25 
 
 20.24 
 
 31.88 
 
 26.57 
 
 24.04 
 
 16.20 
 
 18.56 
 
 14.73 
 
 20.78 
 
 Medium 
 
 
 
 
 
 
 
 
 
 
 
 silt 
 
 .016-.025 
 
 0.5 
 
 1.44 
 
 2.73 
 
 2'.31 
 
 4.64 
 
 1.81 
 
 3.06 
 
 3.54 
 
 3.83 
 
 
 .025-.036 
 
 1 
 
 6.54 
 
 9.11 
 
 1.33 
 
 9.86 
 
 5.89 
 
 6.93 
 
 6.98 
 
 9.24 
 
 Coarse silt 
 
 .036-.047 
 
 2 
 
 8.36 
 
 10.23 
 
 1.19 
 
 9.59 
 
 5.82 
 
 6.90 
 
 7.10 
 
 7.09 
 
 
 .047-.072 
 
 4 
 
 9.50 
 
 8.41 
 
 10.14 
 
 10.05 
 
 8.46 
 
 8.45 
 
 7.67 
 
 8.89 
 
 Fine sand 
 
 .072-.12 
 
 8 
 
 10.66 
 
 7.47 
 
 10.72' 
 
 10.92 
 
 12.04 
 
 9.72 
 
 12.86 
 
 5.77 
 
 
 .12 -.16 
 
 16 
 
 10.30 
 
 5.97 
 
 10.88 
 
 16.14 
 
 13.43 
 
 10.56 
 
 13.53 
 
 3.85 
 
 Medium 
 
 
 
 
 
 
 
 
 
 
 
 sand 
 
 .16 -.30 
 
 32 
 
 14.69 
 
 6.91 
 
 11.75 
 
 1.96 
 
 19.21 
 
 16.59 
 
 3 3.05 
 
 0.86 
 
 Coarse san 
 
 d .30 -.50 
 
 64 
 
 7.11 
 
 1.32 
 
 3.54 
 
 2.12 
 
 6.60 
 
 10.50 
 
 12.14 
 
 23.04 
 
 Total weight of separates, gm. 
 
 20.02' 
 
 20.44 
 
 19.99 
 
 20.10 
 
 20.38 
 
 20.06 
 
 20.33 
 
 20.14 
 
 Weight of 
 
 original sample, gm. 
 
 19.80 
 
 19.51 
 
 19.72 
 
 19.76 
 
 19.85 
 
 19.86 
 
 19.85 
 
 19.69 
 
 Grits, % 
 
 0.5-2.0 mm. 
 
 16.70 
 
 23.54 
 
 8.84 
 
 8.10 
 
 23.12 
 
 32.00 
 
 28.50 
 
 36.00 
 
 Hygroscop 
 
 >ic moisture 
 
 , % 
 
 0.98 
 
 2.48 
 
 1.38 
 
 1.22 
 
 0.75 
 
 0.70 
 
 0.75 
 
 1.57 
 
 Note. — All weighings made on the water free basis. 
 
390 
 
 University of California Publications in Agricultural Sciences [Vol. 3 
 
 Table 5 — Mechanical Analyses, Hilgard Elutriator Method 
 
 Han ford Fine Sandy Loam 
 
 Separates 
 
 Name 
 Clay 
 
 Fine silt 
 Medium 
 
 silt 
 
 Coarse silt 
 
 Fine sand 
 
 Medium sand 
 Coarse sand 
 
 Velocity, 
 mm. 
 Diameter per 
 mm. second 
 
 0.25 
 
 0.25 
 
 0.5 
 
 1 
 
 2 
 
 4 
 
 8 
 16 
 32 
 64 
 
 .01 
 .01 -.016 
 .016-.025 
 .025-.036 
 .036-.047 
 .047-.072 
 .072-12 
 .12 -.16 
 .16- .30 
 .30- .50 
 
 Total weight of separates, gm. 
 Weight of original sample, gm. 
 Grits, % 0.5-2.0 
 
 Hygroscopic moisture, % 
 
 14- A 
 
 % 
 
 12.89 
 
 37.25 
 
 4.19 
 
 8.63 
 
 7.95 
 
 6.23 
 
 5.26 
 
 7.15 
 
 8.81 
 
 1.43 
 
 20.19 
 
 19.46 
 
 4.12' 
 
 2.73 
 
 Samples 
 
 15-A 
 
 % 
 
 8.16 
 
 19.39 
 
 3.05 
 
 5.04 
 
 6.57 
 
 10.23 
 
 12.31 
 
 13.93 
 
 15.29 
 
 6.02' 
 
 20.23 
 
 19.90 
 
 13.23 
 
 0.49 
 
 16-A 
 
 % 
 
 11.97 
 
 24.61 
 
 3.22 
 
 5.06 
 
 5.99 
 
 7.27 
 
 8.57 
 
 9.76 
 
 16.05 
 
 7.51 
 
 20.53 
 
 19.69 
 
 25.47 
 
 1.54 
 
 19-A 
 
 % 
 
 11.09 
 
 5.95 
 
 1.67 
 
 5.27 
 
 7.14 
 
 12.76 
 
 17.79 
 
 12.00 
 
 24.20 
 
 2.13 
 
 20.08 
 
 19.82 
 
 7.85 
 
 0.89 
 
 20-A 
 
 % 
 
 10.55 
 
 22.09 
 
 6.40 
 
 8.40 
 
 7.68 
 
 9.93 
 
 10.48 
 
 12.29 
 
 10.03 
 
 2.70 
 
 20.27 
 
 19.73 
 
 6.71 
 
 1.34 
 
 22-A 23-A 
 
 7.97 
 
 14.15 
 
 3.15 
 
 5.29 
 
 6.47 
 
 11.30 
 
 17.15 
 
 17.39 
 
 14.87 
 
 2.27 
 
 20.06 
 
 19.81 
 
 3.07 
 
 0.94 
 
 8.68 
 
 22.57 
 
 5.90 
 
 6.89 
 
 10.53 
 
 13.03 
 
 12.71 
 
 7.94 
 
 9.88 
 
 1.85 
 
 20.30 
 
 19.78 
 
 7.24 
 
 1.10 
 
 2 4- A 
 
 % 
 
 6.47 
 
 11.11 
 
 1.20 
 
 5.08 
 
 7.48 
 
 13.91 
 
 19.27 
 
 21.56 
 
 12.36 
 
 1.50 
 
 20.26 
 
 19.83 
 
 6.85 
 
 0.84 
 
 25-A 
 
 % 
 
 6.65 
 
 14.54 
 
 1.59 
 
 6.36 
 
 7.91 
 12.64 
 18.11 
 
 9.55 
 19.15 
 
 3.50 
 19.18 
 19.78 
 
 3.83 
 
 1.10 
 
 Table 6 — Mechanical Analyses, Bureau of Soils Method 
 Diablo Clay Adobe 
 
 Separates 
 
 
 Sampb 
 
 3S 
 
 
 Name 
 
 Diameter 
 mm. 
 
 l-A 
 
 2-A 
 
 % 
 
 5-A 
 
 % 
 
 6-A 
 
 % 
 
 Clay 
 
 .005 
 
 44.81 
 
 44.44 
 
 45.67 
 
 56.01 
 
 Silt 
 
 .005- .05 
 
 32.00 
 
 42.51 
 
 23.01 
 
 14.28 
 
 Very fine sand 
 
 .05 - .10 
 
 19.61 
 
 11.35 
 
 21.58 
 
 25.58 
 
 Fine sand 
 
 .10 - .25 
 
 1.36 
 
 1.33 
 
 4.81 
 
 2.10 
 
 Medium sand 
 
 .25 - .5 
 
 0.26 
 
 0.69 
 
 0.95 
 
 2.05 
 
 Coarse sand 
 
 .5 -1.0 
 
 0.58 
 
 0.20 
 
 1.56 
 
 0.00 
 
 Fine gravel 
 
 1.0 -2.0 
 
 0.03 
 
 0.02 
 
 0.04 
 
 0.00 
 
 Note. — Determinations made by the Division of Soil Technology. 
 
 Table 7 — Mechanical Analyses, Bureau of Soils Method 
 
 Altamont Clay Loam 
 
 Separates 
 
 
 
 Samples 
 
 
 Name 
 
 Diameter 
 mm. 
 
 3-A 
 
 % 
 
 4-A 
 
 % 
 
 7-A 
 % 
 
 Clav 
 
 .005 
 
 33.19 
 
 26.50 
 
 31.84 
 
 Silt 
 
 .005- .05 
 
 31.76 
 
 17.35 
 
 37.40 
 
 Very fine sand 
 
 .05 - .10 
 
 22.81 
 
 39.15 
 
 24.70 
 
 Fine sand 
 
 .10 - .25 
 
 8.97 
 
 6.08 
 
 3.27 
 
 Medium sand 
 
 .25 - .5 
 
 1.99 
 
 7.78 
 
 0.92 
 
 Coarse sand 
 
 .5 -1.0 " 
 
 1.74 
 
 3.06 
 
 0.55 
 
 Fine gravel 
 
 1.0 -2.0 
 
 1.01 
 
 1.22 
 
 0.22 
 
 NOTE. — Determinations made by the Division of Soil Technology. 
 
1919] 
 
 Pendleton: A Study of Soil Types 
 
 391 
 
 
 Table 8 — Mechanical Analyses, Bureau of 
 
 Soils Method 
 
 
 
 
 
 San Joaquin Sandy 
 
 Loam 
 
 
 
 
 
 Separal 
 
 es 
 
 
 
 
 Samples 
 
 A 
 
 
 
 
 Name 
 
 ^ 
 Diameter 
 mm. 
 
 10-A 
 
 % 
 
 ll-A 
 
 % 
 
 12-A 
 
 % 
 
 13-A 
 
 % 
 
 17-A 
 
 % 
 
 18-A 
 
 % 
 
 21-A 
 
 % 
 
 2 6- A 
 
 % 
 
 Clay 
 
 .005 
 
 10.78 
 
 15.77 
 
 16.16 
 
 16.94 
 
 11.77 
 
 10.49 
 
 8.28 
 
 17.38 
 
 Silt 
 
 .005- .05 
 
 21.60 
 
 35.97 
 
 25.04 
 
 22.70 
 
 15.97 
 
 2'6.74 
 
 17.70 
 
 18.17 
 
 Very fine sand 
 
 .05 - .10 
 
 28.07 
 
 18.53 
 
 27.42 
 
 47.01 
 
 20.42 
 
 12.02' 
 
 15.92 
 
 13.84 
 
 Fine sand 
 
 .10 - .25 
 
 19.96 
 
 2.66 
 
 17.07 
 
 3.99 
 
 22.57 
 
 16.61 
 
 21.27 
 
 10.26 
 
 Medium sand 
 
 .25 - .5 
 
 9.20 
 
 6.96 
 
 5.80 
 
 4.69 
 
 10.75 
 
 13.85 
 
 13.57 
 
 14.72 
 
 Coarse sand 
 
 .5 -1.0 
 
 9.08 
 
 8.51 
 
 6.52 
 
 2.96 
 
 13.81 
 
 16.52 
 
 21.41 
 
 24.26 
 
 Fine gravel 
 
 1.0 -2.0 
 
 1.34 
 
 12.52' 
 
 2.15 
 
 1.81 
 
 3.13 
 
 4.07 
 
 2.07 
 
 2.02 
 
 Note. — Determinations made by the Di 
 
 vision of 
 
 Soil Technology. 
 
 
 
 
 
 Table 9 — Mechanical Analyses, Bureau of Soils Method 
 Ranford Fine Sandy Loam 
 
 Separates 
 
 A 
 
 
 
 
 
 Samples 
 
 A 
 
 
 
 
 
 f *\ 
 
 Diameter 
 Name mm. 
 
 14-A 
 
 % 
 
 15-A 
 
 % 
 
 16- A 
 
 % 
 
 19- A 
 
 % 
 
 20-A 
 
 % 
 
 22-A 
 
 % 
 
 23-A 
 
 % 
 
 2 4- A 
 
 % 
 
 25-A 
 
 % 
 
 Clay .005 
 
 14.10 
 
 12.08 
 
 16.84 
 
 15.28 
 
 15.95 
 
 7.79 
 
 10.61 
 
 9.83 
 
 7.60 
 
 Silt .005- .05 
 
 39.25 
 
 22.42 
 
 16.16 
 
 15.03 
 
 32.90 
 
 22.70 
 
 24.38 
 
 11.42 
 
 12.90 
 
 Very fine sand .05 - .10 
 
 22.66 
 
 37.12 
 
 16.46 
 
 32.87 
 
 22.58 
 
 36.15 
 
 38.73 
 
 42.05 
 
 67.37 
 
 Fine sand .10 - .25 
 
 17.54 
 
 6.51 
 
 17.32 
 
 8.13 
 
 18.20 
 
 27.78 
 
 16.51 
 
 28.73 
 
 5.88 
 
 Medium sand .25 - .5 
 
 4.71 
 
 11.40 
 
 11.70 
 
 15.42 
 
 4.97 
 
 4.21 
 
 4.66 
 
 4.27 
 
 3.47 
 
 Coarse sand .5 -1.0 
 
 1.99 
 
 8.49 
 
 15.54 
 
 9.27 
 
 3.07 
 
 1.47 
 
 3.28 
 
 3.01 
 
 1.27- 
 
 Fine gravel 1.0 -2.0 
 
 0.13 
 
 1.91 
 
 5.27 
 
 3.63 
 
 0.20 
 
 0.20 
 
 1.48 
 
 1.02 
 
 1.02 
 
 Note. — Determinations made 
 
 by the Division i 
 
 af Soil Technology. 
 
 
 
 
 
 Moisture Equivalent. — The moisture equivalents of the surface 
 horizon samples were determined by the Division of Soil Technology 
 (table 10, and figs. 9, 10). The different types gave quite distinct 
 averages, though there was considerable variation within the type. 
 The Diablo clay adobe varied from 37% to 57%, with an average of 
 47%. The Altamont clay loam varied from 22% to 37%, with 28% 
 as an average. The San Joaquin sandy loam varied from 7% to 
 15%, with the average of 11%. The Hanford fine sandy loam varied 
 from 11% to 25%, with 15% as the average. These figures show 
 that as a whole the moisture equivalents of the several types are 
 distinct, though there is the usual overlapping in some cases. The 
 samples of a given type are in many instances closely similar, though 
 not always or even usually so. 
 
392 University of California Publications in Agricultural Sciences [Vol. 3 
 
 60 
 
 55 
 
 50 
 
 45 
 
 10 
 
 30 
 
 25 
 
 20 
 
 15 
 
 10 
 
 
 
 1 
 
 
 
 / 
 
 
 
 1 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 \ 
 
 
 
 \ 
 
 \ 
 
 \ 
 \ 
 \ 
 
 / 
 / 
 
 / 
 / 
 
 
 
 
 
 
 
 
 Moisture 
 Equivalent 
 
 Hygro. 
 
 Coef. 
 
 35 
 
 ;;<> 
 
 20 
 
 10 
 
 \ 
 
 
 \ 
 
 
 \ 
 
 
 \ 
 
 
 \ 
 
 \ 
 
 
 \ 
 
 \ 
 
 \ 
 
 \ 
 
 
 \ 
 \ 
 
 ^- 
 
 
 
 Moisture 
 Equivalent 
 
 Hygro. 
 Coef. 
 
 12 5 6 Soils 3 4 7 Soils 
 
 Fig. 9. Graph showing the results of the determination of the moisture 
 equivalent and of the hygroscopic coefficient on the four samples of Diablo 
 clay adobe and the three samples of Altamont clay loam. 
 
1919] 
 
 Pendleton: A Study of Soil Types 
 
 393 
 
 Table 10 — Moisture Equivalent 
 
 Diablo Clay 
 
 A 
 
 Adobe 
 
 Altamont Clay Loam 
 
 San 
 No. 
 
 Joaquin 
 Loam 
 
 A 
 
 Sandy 
 
 Hanford Fine 
 Loam 
 
 A 
 
 Sandy 
 
 r 
 No. 
 
 % 
 
 Average 
 
 No. 
 
 % 
 
 Average 
 
 % 
 
 % 
 
 Average 
 
 % 
 
 No. 
 
 % 
 
 Average 
 
 1-A 
 
 49.70 
 
 
 3-A 
 
 38.10 
 
 
 10-A 
 
 10.30 
 
 
 14-A 
 
 25.80 
 
 
 
 48.90 
 
 49.30 
 
 
 37.80 
 
 37.95 
 
 
 10.10 
 
 10.20 
 
 
 25.20 
 
 25.50 
 
 2-A 
 
 37.40 
 
 
 4-A 
 
 23.41 
 
 
 11-A 
 
 15.52 
 
 
 15-A 
 
 11.50 
 
 
 
 36.80 
 
 37.10 
 
 
 22.35 
 
 22.88 
 
 
 15.54 
 
 15.53 
 
 
 11.20 
 
 11.35 
 
 5-A 
 
 46.55 
 
 
 ■ 7-A 
 
 23.90 
 
 
 12-A 
 
 13,72 
 
 
 16-A 
 
 15.60 
 
 
 
 48.10 
 
 47.32 
 
 
 23.90 
 
 23.90 
 
 
 13.62 
 
 13.67 
 
 
 15.60 
 
 15.60 
 
 6-A 
 
 58.80 
 
 
 Average 
 
 28.94 
 
 13-A 
 
 14.50 
 
 
 19-A 
 
 13.30 
 
 
 
 56.80 
 
 57.80 
 
 
 
 
 
 14.60 
 
 14.55 
 
 
 14.30 
 
 13.80 
 
 Average 
 
 i 47.88 
 
 
 
 
 17-A 
 
 8.90 
 
 
 20- A 
 
 18.41 
 
 
 
 
 
 
 
 
 
 8.98 
 
 8.94 
 
 
 18.38 
 
 18.39 
 
 
 
 
 
 
 
 18-A 
 2 1-A 
 26-A 
 
 7.92 
 7.87 
 7.16 
 7.09 
 11.30 
 11.81 
 
 7.89 
 
 7.12 
 
 11.55 
 
 22-A 
 2 3-A 
 24-A 
 
 12.73 
 12.22 
 11.08 
 10.90 
 16.30 
 16.17 
 
 12.47 
 10.99 
 16.23 
 
 
 
 
 
 
 
 Average 
 
 ! 11.18 
 
 25-A 
 
 11.17 
 
 
 
 
 
 
 
 
 
 
 
 
 12.72 
 
 11.94 
 
 
 
 
 
 
 
 
 
 
 Average 
 
 15.14 
 
 Note. — Determinations made by the Division of Soil Technology. 
 
 Table 11 — Hygroscopic Coefficient 
 
 Diablo Clay 
 
 A 
 
 Adobe 
 
 Altamont Clav 
 
 A 
 
 Loam 
 
 San Joaquin 
 Loam 
 
 A 
 
 Sandy 
 
 Hanford Fine 
 Loam 
 
 A 
 
 Sandy 
 
 No. 
 
 % 
 
 Average 
 % 
 
 No. 
 
 Average 
 
 % % 
 
 No. 
 
 % 
 
 Average 
 
 % 
 
 No. 
 
 % 
 
 Average 
 
 % 
 
 1-A 
 
 15.88 
 
 
 3-A 
 
 17.48 
 
 
 14-A 
 
 5.35 
 
 
 10-A 
 
 2.46 
 
 
 
 15.08 
 
 15.48 
 
 
 18.45 
 
 17.93 
 
 
 4.70 
 
 5.03 
 
 
 2.51 
 
 2.49 
 
 2-A 
 
 9.90 
 
 
 4-A 
 
 9,60 
 
 
 15-A 
 
 1.31 
 
 
 11-A 
 
 3.44 
 
 
 
 9.48 
 
 9.69 
 
 
 7.00 
 
 8.30 
 
 
 1.39 
 
 1.35 
 
 
 3.45 
 
 3.44 
 
 5-A 
 
 14.18 
 
 
 7-A 
 
 7.92 
 
 
 16-A 
 
 3.90 
 
 
 12-A 
 
 3.58 
 
 
 
 13.90 
 
 14.04 
 
 
 5.92 
 
 6.92 
 
 
 3.60 
 
 3.75 
 
 
 3.45 
 
 3.52 
 
 6-A 
 
 15.20 
 
 
 Average 
 
 11.05 
 
 19-A 
 
 1.66 
 
 
 13-A 
 
 2.50 
 
 
 
 15.70 
 
 15.45 
 
 
 
 
 
 1.80 
 
 1.73 
 
 
 2.60 
 
 2.55 
 
 Average 
 
 s 13.66 
 
 
 
 
 20- A 
 
 2.90 
 
 
 17-A 
 
 1.84 
 
 
 
 
 
 
 
 
 
 3.02 
 
 2.96 
 
 
 1.62 
 
 1.73 
 
 
 
 
 
 
 
 22-A 
 
 2.48 
 2.89 
 
 2.69 
 
 18-A 
 
 2.10 
 2.00 
 
 2.05 
 
 
 
 
 
 
 
 23-A 
 
 2.38 
 2.53 
 
 2.46 
 
 21-A 
 
 1.98 
 1.92 
 
 1.95 
 
 
 
 
 
 
 
 24-A 
 
 2.39 
 
 
 26-A 
 
 3.57 
 
 
 
 
 
 
 
 
 24-A 
 
 2.39 
 
 
 
 3.52 
 
 3.55 
 
 
 
 
 
 
 
 
 2.37 
 
 2.38 
 
 Average 
 
 2.66 
 
 
 
 
 
 
 
 25-A 
 
 1.78 
 1.84 
 
 1.81 
 
 
 
 
 Note. — Determinations made by the Division of Soil Technology. 
 
394 University of California Publications in Agricultural Sciences [Vol. 3 
 
 15 
 
 10 
 
 
 Moisture 
 Equiv. 
 
 Hygro. 
 Coef. 
 
 10 
 
 11 
 
 12 
 
 13 
 
 18 
 
 21 
 
 2G Soils 
 
 20 
 
 ir> 
 
 10 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 X 
 
 \ 
 
 ^ 
 
 \ 
 
 -"" 
 
 
 
 
 
 
 
 
 
 Moisture 
 Equiv. 
 
 10 
 
 20 
 
 22 
 
 23 
 
 24 
 
 Hygro. 
 Coef. 
 
 23 Soils 
 
 Fig. 10. Graph showing the results of the determination of the moisture 
 equivalent and of the hygroscopic coefficient on the eight samples of San 
 Joaquin sandy loam and the nine samples of Ilanford fine sandy loam. 
 
 Hygroscopic Coefficient. — The determination of this coefficient, 
 also by the Division of Soil Technology, shows no very distinct values 
 for the several types under consideration (table 11, figs. 9,10). The 
 Diablo clay adobe samples vary from 9.6% to 15.4%, with the average 
 of 13.69? • The Altamont clay loam samples vary from 6.9% to 
 17.9%, averaging 11%. The San Joaquin sandy loam varies from 
 
1919] 
 
 Pendleton: A Study of Soil Types 
 
 39; 
 
 1.7% to 3.5%, with the average of 2.66%, while the Hanford fine 
 sandy loam varies from 1.3% to 5%, with the average of 2.68%. 
 There is no question that here the range of values within every type 
 is greater than that from type to type. Even excluding those sam- 
 ples shown by the mechanical analysis to be not true to name there 
 is a wide range within each type — a range too wide to allow one 
 to answer the question of this paper in the affirmative. 
 
 % 
 
 V.6 
 0.2 
 0.1 
 00 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 P 2 5 
 
 N 
 
 6 Soils 
 
 Fig. 11. Graph showing the percentages of nitrogen and of phosphorus in 
 the four samples of Diablo clay adobe. 
 
 The Chemical Data 
 
 Total Nitrogen 
 
 Diablo clay adobe. — There is more variation in nitrogen content 
 between the different representatives of the type than one would 
 expect from a visual examination of the soils (table 12 and fig. 11). 
 No. 2 would be expected to contain less nitrogen than no. 5 because of 
 the lighter color, but such is not the case. In the A horizon, no. 5 
 shows the lowest notal nitrogen content with 0.084%, no. 2 is higher 
 with 0.092%, no. 1 with 0.104%, and no. 6 is the highest with 0.117%. 
 The decrease in the nitrogen content with the increase in depth is 
 normal. In the C horizon, no. 1 has the lowest total nitrogen content 
 with 0.057%, and no. 6 the highest, with 0.078 %. 
 
 Altamont clay loam. — The agreement between the A samples is 
 fairly close (table 13, and fig. 12). No. 4 has 0.103%, no. 7, 0.104%, 
 and no. 3 has 0.123%. This gives an average for the surface soil of 
 0.110%, as compared with 0.099% in the Diablo clay adobe. It is to 
 be noted that the nitrogen content of the subsoil is relatively less 
 than that in the Diablo subsoils, 0.071% and 0.056% in the Altamont 
 B and C horizons, respectively, as against 0.076% and 0.065% in the 
 
396 
 
 University of California Publications in Agricultural Sciences [Vol. 3 
 
 B and C horizons of the Diablo. The average amount of nitrogen is 
 higher in the A horizon of the Altamont than in the Diablo, contrary 
 to what one would expect from the color of the soils, since the Alta- 
 mont is typically a brown soil and the Diablo a dark gray to black soil. 
 San Joaquin sandy loam. — The nitrogen content of these soils is 
 uniformly low (table 14 and fig. 13), from 0.03% to 0.05%, and is but a 
 third to a half of what Hilgard believed adequate for crop production. 
 
 0.6 
 0.2 
 0.1 
 00 
 
 
 
 
 
 
 
 
 
 
 
 
 
 P 2 5 
 
 7 Soils 
 
 Fig. 12. Graph showing the percentages of nitrogen and of phosphorus in 
 the three samples of Altamont clay loam. 
 
 ^ P 2 Q 5 
 
 0.0 
 
 26 Soils 
 
 Fig. 13. Graph showing the percentages of nitrogen and of phosphorus in 
 the eight samples of San Joaquin sandy loam. 
 
 The nitrogen content is seen to vary more or less directly with the 
 amount of the finer sediments present in the soil — nos. 11 and 12 
 being heavy members of the type, with 0.05% and 0.047% respec- 
 tively, and nos. 17 and 18 light members of the type with 0.029% and 
 0.027% respectively. It may be noted that the nitrogen content of 
 the various horizons are not as far apart as in the other types. The 
 averages for the three horizons are: A — 0.037%, B — 0.027%, and 
 C — 0.026%. It must be borne in mind that the San Joaquin sandy 
 Loam horizons are not full 12-inch samples, and that the total depth 
 of the sampling is less. 
 
1919] 
 
 Pendleton: A Study of Soil Types 
 
 397 
 
 Han ford fine sandy loam. — Here again in the A horizon the nitro- 
 gen content is fairly uniform (table 15, and fig. 14), with from 0.045% 
 to 0.072%, if the extra typical no. 14, with 0.119%, be left out of 
 consideration. One would suppose these soils to be higher in their 
 
 or 
 0.9 
 
 0.8 
 
 0.7 
 
 0.6 
 
 0.5 
 
 0.4 
 
 0.3 
 
 0.2 
 
 0.1 
 
 0.0 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 x 
 
 
 
 
 
 
 / 
 
 
 
 
 
 
 
 
 
 
 \ 
 
 
 
 
 
 
 
 
 
 
 
 
 
 — — -~ 
 
 — -^.^ 
 
 
 
 P205 
 
 16 
 
 19 
 
 20 
 
 22 
 
 23 
 
 24 
 
 25 Soils 
 
 Fig. 14. Graph showing the percentages of nitrogen and of phosphorus in 
 the nine samples of Hanford fine sandy loam. 
 
 nitrogen content, as compared with the San Joaquin series, than the 
 results show. The B and C horizons of the Hanford samples contain 
 0.038% and 0.028% nitrogen, respectively, showing that with the 
 increase of deriih there is a more rapid decrease of nitrogen than in 
 the San Joaquin samples, with the nitrogen content of the C horizon 
 of the Hanford only 0.002% above that of the C horizon of the San 
 
398 
 
 University of California Publications in Agricultural Sciences [Vol. 3 
 
 Joaquin. The greenhouse pot cultures showed the effect of the much 
 higher nitrogen content in no. 14 in giving better color and growth 
 to the plants and especially to the grains. The increase of the nitrogen 
 in the surface of no. 23, as compared with the B and C horizons, 
 might be ascribed to the fertilizers applied to the orange grove where 
 this sample was collected; yet no. 24 is a truck soil which has been 
 fertilized to a considerable extent with barnyard manure. The nitro- 
 gen content of this type, as judged by the previous standards, is 
 quite inadequate. 
 
 Compare the nitrogen content of the A horizons of the four types : 
 The Diablo has an average of 0.099%, with a range or from 0.084% 
 to 0.117% ; the Altamont has an average of 0.110%, with a range of 
 from 0.103% to 0.123%; ; the San Joaquin has an average of 0.037%?, 
 with a range of from 0.027% to 0.050% ; and the Hanford has an 
 average of 0.062%, with a range of from 0.045% to 0.119%. Thus 
 the total nitrogen content of the several types is reasonably constant 
 within the type and rather distinct for the types. 
 
 
 
 Table 12- 
 
 -Total Nitrogen 
 
 
 
 
 
 Diablo Clay Adobe 
 
 
 
 
 
 
 Horizon 
 
 A 
 
 
 
 le 
 
 A 
 
 % 
 
 Average 
 
 % 
 
 B Average 
 
 % % 
 
 C 
 
 % 
 
 Average 
 
 % 
 
 
 0.109 
 
 0.105 
 
 0.076 0.069 
 
 0.056 
 
 0.057 
 
 
 0.101 
 
 
 0.063 
 
 0.059 
 
 
 
 0.100 
 
 
 0.072 
 
 0.062 
 
 
 
 0.084 
 
 0.092 
 
 0.064 0.068 
 
 0.058 
 
 0.060 
 
 
 0.085 
 
 
 0.065 
 
 No sample 
 
 
 0.084 
 
 0.084 
 
 0.065 0.065 
 
 
 
 
 0.114 
 
 
 0.097 
 
 0.075 
 
 
 
 0.122 
 
 0.118 
 
 0.107 0.102 
 
 0.083 
 
 0.079 
 
 iver 
 
 age 
 
 0.100 
 
 0.076 
 
 
 0.065 
 
 Sample 
 3 
 
 A 
 
 % 
 
 0.123 
 0.124 
 0.103 
 0.103 
 0.106 
 0.104 
 
 Table 13 — Total Nitrogen 
 Altamont Clay Loam 
 
 Horizon 
 
 Average 
 
 Average 
 
 % 
 
 0.123 
 
 0.103 
 
 0.105 
 0.110 
 
 B 
 
 % 
 
 0.089 
 0.087 
 0.054 
 0.053 
 0.070 
 0.077 
 
 Average 
 
 % 
 
 0.088 
 
 0.053 
 
 0.073 
 0.071 
 
 C 
 
 % 
 
 0.069 
 0.067 
 0.041 
 0.041 
 0.061 
 0.059 
 
 Average 
 
 % 
 
 0.068 
 0.041 
 0.041 
 
 0.060 
 0.056 
 
1919] 
 
 Pendleton: A Study of Soil Types 
 
 399 
 
 Table 14 — Total Nitrogen 
 San Joaquin Sandy Loam 
 Horizon 
 
 Sample 
 
 A 
 
 % 
 
 Average 
 
 % 
 
 B 
 
 % 
 
 Average 
 
 % 
 
 C 
 
 % 
 
 Average 
 
 % 
 
 10 
 
 0.037 
 
 
 0.026 
 
 
 0.022 
 
 
 
 0.038 
 
 0.037 
 
 0.029 
 
 0.027 
 
 0.020 
 
 0.021 
 
 11 
 
 0.051 
 
 
 0.042 
 
 
 0.038 
 
 
 
 0.051 
 
 0.051 
 
 0.046 
 
 0.044 
 
 0.040 
 
 0.039 
 
 12 
 
 0.049 
 
 
 0.032 
 
 
 0.042 
 
 
 
 0.045 
 
 0.047 
 
 0.034 
 
 0.033 
 
 0.040 
 
 0.041 
 
 13 
 
 0.040 
 
 
 0.038 
 
 
 0.033 
 
 
 
 0.040 
 
 0.040 
 
 0.043 
 
 0.040 
 
 0.033 
 
 0.033 
 
 17 
 
 0.028 
 
 
 0.019 
 
 
 No sample 
 
 
 0.030 
 
 0.029 
 
 0.018 
 
 0.018 
 
 
 
 18 
 
 0.028 
 
 
 0.016 
 
 
 0.018 
 
 
 
 
 0.028 
 
 0.017 
 
 0.016 
 
 0.021 
 
 0.019 
 
 21 
 
 0.029 
 
 
 0.012 
 
 
 0.014 
 
 
 
 0.030 
 
 0.029 
 
 0.012 
 
 0.012 
 
 0.014 
 
 0.014 
 
 26 
 
 0.041 
 
 
 0.026 
 
 
 0.016 
 
 
 
 0.041 
 
 0.041 
 
 0.027 
 
 0.026 
 
 0.017 
 
 0.016 
 
 Average 
 
 0.038 
 
 
 0.027 
 
 
 0.026 
 
 Sample 
 14 
 
 15 
 
 16 
 
 19 
 
 20 
 
 22 
 
 23 
 
 24 
 25 
 
 Average 
 
 
 Table 15- 
 
 —Total 
 
 Nitrogen 
 
 
 
 
 Hanford 
 
 Fine Sandy Loam 
 Horizon 
 
 A 
 
 
 
 A 
 
 % 
 
 Average 
 
 % 
 
 B 
 
 % 
 
 Average 
 
 % 
 
 C 
 
 % 
 
 Average 
 
 % 
 
 0.113 
 
 
 0.084 
 
 
 0.060 
 
 
 0.126 
 
 0.119 
 
 0.081 
 
 0.082 
 
 0.057 
 
 0.058 
 
 0.052 
 
 
 0.039 
 
 
 0.028 
 
 
 0.055 
 
 0.053 
 
 0.043 
 
 0.041 
 
 0.027 
 
 0.028 
 
 0.058 
 
 
 0.030 
 
 
 0.020 
 
 
 0.054 
 
 0.056 
 
 
 0.030 
 
 0.023 
 
 0.021 
 
 0.046 
 
 
 0.025 
 
 
 0.024 
 
 0.023 
 
 0.044 
 
 0.045 
 
 0.025 
 
 0.025 
 
 0.023 
 
 0.023 
 
 0.062 
 
 
 0.032 
 
 
 0.024 
 
 
 0.058 
 
 0.060 
 
 0.034 
 
 0.033 
 
 0.022 
 
 0.023 
 
 0.057 
 
 
 0.033 
 
 
 0.025 
 
 
 0.061 
 
 0.059 
 
 0.036 
 
 0.034 
 
 0.023 
 
 0.024 
 
 0.075 
 
 
 0.028 
 
 
 0.020 
 
 
 0.071 
 
 0.073 
 
 0.030 
 
 0.029 
 
 0.016 
 
 0.018 
 
 0.050 
 
 
 0.032 
 
 0.034 
 
 0.028 
 
 0.028 
 
 0.045 
 
 
 0.031 
 
 
 0.022 
 
 
 0.047 
 
 0.046 
 
 0.032 
 
 0.031 
 
 0.024 
 
 0.023 
 
 
 0.062 
 
 
 0.038 
 
 
 0.027 
 
400 
 
 University of California Publications in Agricultural Sciences [Vol. 3 
 
 Humus 
 
 Diablo clay adobe. — The variations in the humus content of the A 
 samples (table 16, and fig. 15) are moderate, 1.1% to 1.4%, while the 
 B and C horizons do not agree so closely with each other or with the 
 
 Loss on 
 Ignition 
 
 
 
 
 
 
 / 
 / 
 
 
 
 
 
 / 
 
 / 
 
 / 
 
 / 
 / 
 
 
 
 
 
 / 
 / 
 / 
 / 
 
 
 
 
 
 
 
 
 / 
 
 / 
 
 
 
 
 
 
 
 
 
 
 
 
 
 / 
 
 
 
 
 
 _. 
 
 / 
 / 
 
 —• — :: -~" 
 
 
 N>.. 
 
 <■ -*K, 
 
 / 
 /. 
 
 
 
 
 X. 
 
 
 
 
 X 
 X 
 \ 
 
 
 . — 
 
 2 .-__ 
 
 MgO 
 
 K 2 
 
 Humus 
 
 ■ CaO 
 
 Soils 
 
 Fig. 15. Graph showing the loss on ignition, the amount of humus, and 
 the percentages of calcium, magnesium, and potassium in the four samples 
 of Diablo clay adobe. 
 
 surface foot. The average content of humus in the A samples is 
 1.26%, in the B samples 0.95%, and in the C samples 0.75%. It is 
 worthy of note that soil no. 2, with the lightest color of the four, and 
 what might be supposed to be a lower humus content, has next to the 
 highest amount. 
 
1919] 
 
 Pendleton: A Study of Soil Types 
 
 401 
 
 Altamont clay loam. — Here the variations in the humus content 
 (table 17, and fig. 16) are small in the A horizon, 1.1% to 1.3%. The 
 average is 1.24%. The B and C samples show a good parallelism 
 among themselves, but not so good when compared with the surface. 
 The average of the B horizon is 0.84%, and of the C horizon 0.57%. 
 
 \ 
 
 \ 
 
 V 
 
 y 
 
 / 
 
 / 
 
 / 
 
 / 
 
 ^L- 
 
 / 
 
 Loss on 
 Ignition 
 
 K 2 
 
 Humus 
 CaO 
 
 MgO 
 
 3 4 7 Soils 
 
 Fig. 16. Graph showing the loss on ignition, the amount of humus, and the 
 percentages of calcium, magnesium, and potassium in the three samples of Alta- 
 mont clay loam. 
 
 San Joaquin sandy loam. — This type contains a considerable quan- 
 tity of humus (table 18, and fig. 17) when one takes into considera- 
 tion the popular criteria for the presence of humus, for the red to 
 reddish brown San Joaquin soils are very different from the brown 
 Altamont or the black Diablo soils. The samples of this type gave 
 
40: 
 
 University of California Publications in Agricultural Sciences [Vol.3 
 
 light colored or nearly colorless humus solutions. But when the ali- 
 quots were ignited, after evaporation, there was a very noticeable 
 blackening and charring of the residue, together with a considerable 
 
 
 
 
 
 
 
 
 
 / 
 
 \ 
 
 
 
 
 
 
 / 
 
 \ 
 
 
 
 
 
 
 / 
 
 \ 
 
 
 
 
 
 
 / 
 
 / 
 
 \ 
 
 
 
 
 
 
 / 
 
 \ 
 
 
 
 
 
 / 
 
 / J 
 / 
 
 i \\ 
 
 
 
 
 / 
 
 / 
 
 
 / 
 
 "v\ 
 
 
 
 
 / 
 / 
 
 / 
 
 / 
 
 
 v 
 
 
 
 / 
 
 \ / 
 
 / 
 
 / 
 
 
 \\ 
 
 
 
 Y 
 
 / 
 
 / 
 
 
 s 
 
 
 
 
 / 
 
 / 
 
 
 V 
 A 
 
 
 
 / \ 
 
 / \ 
 
 
 / 
 
 
 / x 
 
 V-— .. 
 
 
 / 
 / 
 
 
 / 
 
 
 
 \ 
 
 ^^**». 
 
 \ / 
 
 
 
 
 \ 
 
 
 
 \/ 
 
 
 
 
 \ 
 
 \ 
 
 
 / \ 
 
 
 
 
 
 \ 
 
 
 / 
 
 t- : 
 
 " ** 
 
 .... 
 
 ^ 
 
 
 \ 
 
 ""■:./ 
 
 
 
 
 *«« 
 
 ... *"^»l 
 
 ****■••—.. 
 
 \, 
 
 y 
 
 
 
 
 
 •• <Sv ^ 
 
 ->< 
 
 y 
 
 
 
 
 
 "-N... 
 
 ^ 
 
 Loss on 
 Ignition 
 
 K2O 
 
 Humus 
 
 MgO 
 CaO 
 
 10 
 
 12 
 
 L3 
 
 17 
 
 IS 
 
 21 26 Soils 
 
 Fig. 17. Graph showing the loss on ignition, the amount of humus, and 
 the percentages of calcium, magnesium, and potassium in the nine samples of 
 San Joaquin sandy loam. 
 
 loss in weight. This phenomenon, in the light of the work of Gortner, 27 
 shows that these soils have a "humus" content above that which they 
 might be supposed to have, because of the almost complete absence of 
 
 27 soil Science, vol. 2 (1916), pp. 395-442. 
 
1919] Pendleton: A Study of Soil Types 403 
 
 the "black pigment." Soil no. 26, probably the only virgin soil in 
 the series, shows a particularly high content of humus for such a soil, 
 though from the color of the soil one would suspect but very little 
 humus. The agreement between the three horizons of the San Joaquin 
 sandy loam samples is close. The average content of humus was 
 0.68% in the A, 0.51% in the B, and 0.38% in the C horizon. 
 
 Han ford fine sandy loam. — The variations in humus content in this 
 type are greater than in any of the others (table 19, and fig. 18). This 
 is possibly because of two factors : the open texture of the soil, hence 
 the rapid loss of organic matter by oxidation processes ; and secondly, 
 the high agricultural value of this soil, which has led to a greater appli- 
 cation of fertilizers than has been the case with the other soils. The 
 actual variations in the humus content are large, 0.7% to 2.1% with 
 the average of 1.15% for horizon A, from 0.5% to 1.8% with the aver- 
 age of 0.81% for B, and from 0.44% to 1.07% with the average of 
 0.59% for C. The extra-typical sample no. 14 is above any of the 
 others in the total humus content. The variations in the subsoil 
 humus content are more or less parallel to those of the surface soil. 
 
 The following averages of the humus content of horizon A, Diablo 
 1.26%, Altamont 1.24%, San Joaquin 0.68%, Hanford 1.15%, show 
 that there is not much difference between the soils, except for the San 
 Joaquin sandy loam, which has an average of half the others. Within 
 the type the soils may be nearly alike, as in the San Joaquin and Alta- 
 mont, or may be variable to a large degree, as in the Hanford. The 
 variations in the humus content of the soils are small, considering the 
 diverse nature of the soils, and the usual methods for judging the 
 quantity of humus. 
 
 Table 16 — Humus (and Humus Ash) 
 Diablo Clay Adobe 
 
 
 
 
 Humus 
 Horizons 
 
 A 
 
 
 
 
 
 Humus ash 
 Horizons 
 
 A 
 
 
 
 Sample 
 
 A 
 
 % 
 
 Average 
 
 % 
 
 B 
 
 Average C 
 
 % % 
 
 Average 
 
 % 
 
 A Average 
 
 % % 
 
 B 
 
 % 
 
 Average 
 
 % 
 
 C 
 
 % 
 
 Aver- 
 age 
 
 % 
 
 1 
 
 1.08 
 
 
 0.51 
 
 
 0.18 
 
 
 0.55 
 
 
 0.75 
 
 
 0.45 
 
 
 
 1.08 
 
 1.08 
 
 0.51 
 
 0.51 
 
 0.24 
 
 0.21 
 
 0.56 
 
 0.56 
 
 0.73 
 
 0.74 
 
 0.46 
 
 0.46 
 
 2 
 
 1.40 
 
 
 1.16 
 
 
 1.09 
 
 
 1.01 
 
 
 0.96 
 
 
 1.09 
 
 
 
 1.38 
 
 1.39 
 
 1.15 
 
 1.15 
 
 1.02 
 
 1.06 
 
 1.03 
 
 1.02 
 
 0.96 
 
 0.96 
 
 0.96 
 
 1.03 
 
 5 
 
 1.17 
 
 
 0.87 
 
 
 
 
 1.08 
 
 
 1.19 
 
 
 
 
 
 1.12 
 
 1.15 
 
 0.91 
 
 0.89 
 
 
 
 1.10 
 
 1.09 
 
 1.14 
 
 1.17 
 
 
 
 6 
 
 1.48 
 
 
 1.26 
 
 
 0.95 
 
 
 0.98 
 
 
 0.88 
 
 
 0.78 
 
 
 Werag 
 
 1.37 
 
 3 
 
 1.43 
 1.26 
 
 1.26 
 
 1.26 
 0.95 
 
 0.99 
 
 0.97 
 0.72 
 
 0.95 
 
 0.96 
 0.91 
 
 0.91 
 
 0.90 
 0.95 
 
 0.85 
 
 0.81 
 0.77 
 
404 
 
 % 
 
 University of California Publications in Agricultural Sciences [Vol. 3 
 
 Humus 
 
 14 15 H> 19 20 22 23 24 25 Soila 
 
 Pig. 18. Graph showing the loss on ignition, the amount of humus, and 
 the percentages of calcium, magnesium, and potassium in the nine samples of 
 Hanford fine sandy loam. 
 
1919] 
 
 Pendleton: A Study of Soil Types 
 
 405 
 
 Table 17 — Humus (and Humus Ash) 
 
 Altamont Clay Loam 
 
 Humus 
 Horizons 
 
 A Average B Average C Average 
 
 Sample % % % % % % 
 
 3 1.06 0.89 0.59 
 
 1.13 1.09 0.84 0.86 0.58 0.59 
 
 4 1.30 0.69 0.59 
 
 1.33 1.31 0.71 0.70 0.28 0.43 
 
 7 1.32 0.95 0.68 
 
 1.31 1.32 0.96 0.96 0.68 0.68 
 
 Average 1.24 0.84 . 0.57 
 
 Humus ash 
 Horizons 
 
 Aver- 
 
 A Average B Average C age 
 
 % % % % % % 
 
 1.29 1.08 0.95 
 
 1.23 1.26 1.28 1.18 0.95 0.95 
 
 0.80 0.98 0.91 
 
 0.85 0.83 0.98 0.98 1.03 0.97 
 
 0.72 0.87 1.09 
 
 0.75 0.74 0.88 0.88 1.08 1.08 
 
 0.94 1.01 1.00 
 
 Table 18 — Humus (and Humus Ash) 
 San Joaquin Sandy Loam 
 
 
 
 
 Humus 
 Horizons 
 
 A 
 
 
 
 
 
 Humus ash 
 Horizons 
 
 A 
 
 
 
 Sample 
 
 A Average 
 
 % % 
 
 B Average 
 
 % % 
 
 C Average 
 
 % % 
 
 A Average 
 
 % % 
 
 B Average 
 
 % % 
 
 C 
 
 % 
 
 Aver- 
 age 
 
 % 
 
 10 
 
 0.66 
 
 0.66 
 
 0.53 
 
 0.53 
 
 0.27 
 
 0.27 
 
 1.31 
 
 1.31 
 
 1.33 
 
 1.33 
 
 0.67 
 
 0.67 
 
 11 
 
 0.75 
 
 
 0.41 
 
 
 0.37 
 
 
 0.51 
 
 
 0.66 
 
 
 0.58 
 
 
 
 0.71 
 
 0.73 
 
 
 0.41 
 
 
 0.37 
 
 0.69 
 
 0.60 
 
 
 0.66 
 
 
 0.58 
 
 12 
 
 0.62 
 
 
 0.49 
 
 
 0.32 
 
 
 0.88 
 
 
 1.50 
 
 
 0.80 
 
 
 
 0.65 
 
 0.64 
 
 
 0.49 
 
 
 0.32 
 
 0.95 
 
 0.91 
 
 
 1.50 
 
 
 0.80 
 
 13 
 
 0.75 
 
 
 0.50 
 
 
 0.35 
 
 
 1.38 
 
 
 0.90 
 
 
 1.02 
 
 
 
 0.78 
 
 0.77 
 
 
 0.50 
 
 
 0.35 
 
 1.36 
 
 1.37 
 
 
 0.90 
 
 
 1.02 
 
 17 
 
 0.51 
 0.51 
 
 0.51 
 
 0.38 
 
 0.38 
 
 
 
 0.53 
 0.57 
 
 0.55 
 
 1.23 
 
 1.23 
 
 
 
 18 
 
 0.56 
 
 
 0.60 
 
 
 0.42 
 
 
 0.61 
 
 
 0.76 
 
 
 1.79 
 
 
 
 0.60 
 
 0.58 
 
 0.58 
 
 0.59 
 
 
 0.42 
 
 0.56 
 
 0.59 
 
 0.75 
 
 0.76 
 
 
 1.79 
 
 21 
 
 0.52 
 
 
 0.19 
 
 
 0.18 
 
 
 0.53 
 
 
 0.37 
 
 
 0.37 
 
 
 
 0.52 
 
 0.52 
 
 0.21 
 
 0.40 
 
 0.21 
 
 0.19 
 
 0.54 
 
 0.53 
 
 0.37 
 
 0.37 
 
 0.48 
 
 0.42 
 
 26 
 
 1.04 
 
 
 0.79 
 
 
 0.68 
 
 
 0.89 
 
 
 3.57 
 
 
 5.28 
 
 
 
 1.01 
 
 1.02 
 
 0.79 
 
 0.79 
 
 0.82 
 
 0.75 
 
 0.76 
 
 0.83 
 
 3.63 
 
 3.60 
 
 5.46 
 
 5.35 
 
 Average 
 
 
 0.66 
 
 
 0.51 
 
 
 0.38 
 
 
 0.83 
 
 
 1.24 
 
 
 1.51 
 
 Excluding no. 
 
 26 
 
 
 
 
 
 
 
 
 0.95 
 
 
 0.87 
 
 Loss on Ignition 
 
 The loss on ignition of the A horizon varies directly with the tex- 
 ture of the soil, the heavier soils losing more on heating. Obviously 
 the water of combination of the clay is a large factor in this loss. In 
 the San Joaquin sandy loam the loss on ignition was determined in 
 the three horizons. In the other three types the A horizon was the 
 only one examined (tables 20, 21, and figs. 15-18). 
 
406 
 
 University of California Publications in Agricultural Sciences [Vol. 3 
 
 
 
 
 Table 
 
 19 — Humus 
 
 (and 
 
 Humu 
 
 s Ash 
 
 
 
 
 
 
 
 
 
 . 
 
 Hanford Fin 
 
 ,e Sandy Loam 
 
 
 
 
 
 
 
 
 Humus 
 Horizons 
 
 
 
 
 
 Humus ash 
 Horizons 
 
 
 
 Sample 
 
 A 
 
 % 
 
 Average B 
 
 % % 
 
 Average C 
 
 % % 
 
 Average 
 
 A Average 
 
 % % 
 
 B Average 
 
 % % 
 
 C 
 
 % 
 
 Aver- 
 age 
 
 % 
 
 14 
 
 2.11 
 
 
 1.81 
 
 
 1.10 
 
 
 1.14 
 
 
 1.24 
 
 
 1.01 
 
 
 
 2.09 
 
 2.10 
 
 1.78 
 
 1.79 
 
 1.05 
 
 1.07 
 
 1.17 
 
 1.16 
 
 1.27 
 
 1.26 
 
 1.09 
 
 1.05 
 
 15 
 
 1.79 
 
 
 0.88 
 
 
 1.04 
 
 
 1.88 
 
 
 0.94 
 
 
 0.92 
 
 
 
 1.77 
 
 1.78 
 
 0.93 
 
 0.90 
 
 0.67 
 
 0.86 
 
 1.85 
 
 1.86 
 
 0.89 
 
 0.92 
 
 0.91 
 
 0.92 
 
 16 
 
 1.20 
 
 
 0.73 
 
 
 0.41 
 
 
 0.91 
 
 
 0.93 
 
 
 0.90 
 
 
 
 1.20 
 
 1.20 
 
 0.73 
 
 0.73 
 
 0.46 
 
 0.44 
 
 0.91 
 
 0.91 
 
 1.47 
 
 0.93 
 
 0.90 
 
 0.90 
 
 19 
 
 0.73 
 
 
 0.51 
 
 
 0.45 
 
 
 0.48 
 
 
 0.57 
 
 
 0.78 
 
 
 
 0.74 
 
 0.73 
 
 0.50 
 
 0.51 
 
 0.55 
 
 0.50 
 
 0.47 
 
 0.48 
 
 0.58 
 
 0.58 
 
 0.76 
 
 0.77 
 
 20 
 
 1.08 
 
 
 0.86 
 
 
 0.59 
 
 
 0.52 
 
 
 0.90 
 
 
 0.79 
 
 
 
 1.06 
 
 1.07 
 
 0.89 
 
 0.88 
 
 0.50 
 
 0.55 
 
 0.56 
 
 0.54 
 
 0.90 
 
 0.90 
 
 0.78 
 
 0.78 
 
 22 
 
 0.96 
 
 
 0.73 
 
 
 0.58 
 
 
 0.59 
 
 
 0.60 
 
 
 0.58 
 
 
 
 0.96 
 
 0.96 
 
 0.71 
 
 0.72 
 
 0.56 
 
 0.57 
 
 0.59 
 
 0.59 
 
 0.60 
 
 0.60 
 
 0.63 
 
 0.61 
 
 23 
 
 1.04 
 
 
 0.59 
 
 
 0.38 
 
 
 0.58 
 
 
 0.45 
 
 
 0.39 
 
 
 
 1.07 
 
 1.05 
 
 0.62 
 
 0.61 
 
 0.38 
 
 0.38 
 
 0.57 
 
 0.58 
 
 0.41 
 
 0.43 
 
 0.37 
 
 0.38 
 
 24 
 
 0.73 
 
 
 0.55 
 
 
 0.56 
 
 
 0.58 
 
 
 0.69 
 
 
 0.82 
 
 
 
 0.73 
 
 0.73 
 
 0.61 
 
 0.58 
 
 0.51 
 
 0.54 
 
 0.56 
 
 0.57 
 
 0.69 
 
 0.69 
 
 0.80 
 
 0.81 
 
 25 
 
 0.71 
 
 
 0.58 
 
 
 0.45 
 
 
 0.57 
 
 
 0.67 
 
 
 0.74 
 
 
 
 0.69 
 
 0.70 
 
 0.56 
 
 0.57 
 
 0.42 
 
 0.44 
 
 0.61 
 
 0.59 
 
 0.71 
 
 0.69 
 
 0.78 
 
 0.76 
 
 Average 
 
 
 1.15 
 
 
 0.82 
 
 
 0.59 
 
 
 0.81 
 
 
 0.78 
 
 
 0.78 
 
 Diablo clay adobe. — The variation in these samples was from 
 5.6% to 8.6%, with the average of 6.8%. The Altamont clay loam 
 has a variation of from 5% to 8.7%, averaging 6.7%. The San Joa- 
 quin sandy loam has a range of variation between 1.6% and 4.2%, 
 with an average of 2.6%. The loss on ignition of the lower horizons 
 increases over that of the surface, because of the increase in texture. 
 The B horizon shows an average loss of 3.9% and the C horizon of 
 4.67%. The Hanford fine sandy loam range of variation in the loss 
 on ignition is, excluding no. 14, from 2.2% to 3.9%, with an average 
 of 3.4%. Thus the curve for this type is quite uniform, except for 
 no. 14, which shows a loss of 6.9%. 
 
 It is seen that the averages in the loss on ignition of the A horizons 
 of the Diablo and Altamont soils are close, and high, 6.8% and 6.7% 
 respectively. The averages of the San Joaquin and Hanford sam- 
 ples, 2.6% and 3.4% respectively, are low and not widely separated. 
 Since the values for the types overlap considerably, and the averages 
 are not distinct, except between the light and heavy groups, there is 
 no significant distinction between the four types by this determination. 
 
1919] 
 
 Pendleton: A Study of Soil Types 
 
 407 
 
 Table 20 — Loss on Ignition 
 (Surface horizon only) 
 
 Diab 
 
 lo Clay Adobe 
 
 A * 
 
 % 
 
 Altamont Clay 
 
 % 
 
 Loam 
 
 % 
 
 Hanford Fine 
 Loam 
 
 A 
 
 Sandy 
 
 ^ 
 
 
 % 
 
 % 
 
 1-A 
 
 6.62 
 
 
 3-A 
 
 8.74 
 
 
 14-A 
 
 6.90 
 
 
 
 6.66 
 
 6.64 
 
 
 8.82 
 
 8.78 
 
 
 6.95 
 
 6.92 
 
 2-A 
 
 6.57 
 
 
 4-A 
 
 5.05 
 
 
 15-A 
 
 2.27 
 
 
 
 6.64 
 
 6.60 
 
 
 5.05 
 
 5.05 
 
 
 2.30 
 
 2.28 
 
 5-A 
 
 5.61 
 
 
 7-A 
 
 6.58 
 
 
 16-A 
 
 3.26 
 
 
 
 
 5.61 
 
 
 6.46 
 
 6.52 
 
 
 3.24 
 
 3.25 
 
 6-A 
 
 8.67 
 8.71 
 
 8.69 
 
 A 
 
 verage 
 
 6.78 
 
 19- A 
 
 3.10 
 3.13 
 
 3.11 
 
 Average 
 
 6.88 
 
 
 
 
 20-A 
 
 3.90 
 
 
 
 
 
 
 
 
 
 3.94 
 
 3.92 
 
 
 
 
 
 
 
 2 2-A 
 
 3.06 
 3.07 
 
 3.06 
 
 
 
 
 
 
 
 23-A 
 
 3.48 
 3.45 
 
 3.46 
 
 
 
 
 
 
 
 24-A 
 
 2.60 
 2.60 
 
 2.60 
 
 
 
 
 
 
 
 2 5-A 
 
 2.68 
 
 2.72 
 
 2.70 
 
 
 
 
 
 
 
 Average 
 
 3.48 
 
 Table 21 — Loss on Ignition 
 San Joaquin Sandy Loam 
 
 Sample 
 
 A 
 
 % 
 
 Average 
 
 % 
 
 10 
 
 2.13 
 
 
 
 2.17 
 
 2.15 
 
 11 
 
 3.23 
 
 
 
 3.20 
 
 3.21 
 
 12 
 
 5.37 
 
 
 
 3.22 
 
 4.29 
 
 13 
 
 2.94 
 
 
 
 2.96 
 
 2.95 
 
 17 
 
 1.85 
 
 
 
 1.88 
 
 1.86 
 
 18 
 
 1.82 
 
 
 
 1.83 
 
 1.82 
 
 21 
 
 1.68 
 
 
 
 1.69 
 
 1.68 
 
 26 
 
 3.30 
 
 3.30 
 
 Avera 
 
 ge 
 
 2.66 
 
 Ho 
 
 rizon 
 
 A 
 
 B 
 
 % 
 
 Average 
 
 % 
 
 2.32 
 
 
 2.27 
 
 2.29 
 
 6.33 
 
 
 6.16 
 
 6.24 
 
 2.97 
 
 
 3.18 
 
 3.07 
 
 6.58 
 
 
 6.75 
 
 6.66 
 
 2.54 
 
 
 2.61 
 
 2.57 
 
 2.18 
 
 
 2.18 
 
 2.18 
 
 1.60 
 
 
 1.56 
 
 1.58 
 
 6.97 
 
 
 6.95 
 
 6.96 
 
 
 3.94 
 
 c 
 
 % 
 
 3.10 
 3.08 
 6.57 
 6.67 
 
 Average 
 
 3.09 
 
 6.62 
 
 5.54 
 
 5.54 
 
 3.97 
 
 
 6.07 
 
 5.02 
 
 NO! 
 
 sample 
 
 2.90 
 
 
 2.89 
 
 2.89 
 
 3.31 
 
 
 3.33 
 
 3.32 
 
 6.18 
 
 
 
 6.18 
 
 4.67 
 
408 University of California Publications in Agricultural Sciences [Vol. 3 
 
 Calcium 
 
 The Diablo, Altamont, and Hanford soils were analyzed for their 
 calcium in the A horizon only, while the A, B, and C horizons of the 
 San Joaquin sandy loam were analyzed (tables 22, 23, and figs. 15-18). 
 
 Diablo clay adobe. — There is much divergence in the amounts of 
 CaO in this type, varying from 0.36% to 2.05%, with the average 
 of 1.23%. 
 
 Altamont clay loam. — In this type there is a little greater varia- 
 tion than in the Diablo samples, with a range of from 0.78% to 5.64%, 
 averaging 2.44% CaO. In both this soil and in the Diablo the wide 
 variation in the lime content is undoubtedly due to the nature of the 
 parent rock, since the soils are residual: 
 
 San Joaquin sandy loam. — In the CaO content there is no uni- 
 formity among the samples. The A samples of this type contain from 
 0.47% to 2.98%, with an average of 1.65%. It would seem that the 
 materials from which the soils were derived were of varying composi- 
 tion. For from the present climatic conditions soil no. 25 is the one 
 subject to the least leaching, and yet has the least CaO content. The 
 B and C percentages follow the surface very closely — sufficiently so 
 to necessitate no particular explanation. The range of variation in 
 the B horizon is from 0.11% to 2.42%, and the average is 1.42%. 
 The C samples vary from 0.17% to 2.81%, with the average of 1.52%. 
 
 Hanford fine sandy loam. — The A samples of this type contain 
 from 2.56% CaO to 4.69%, with 3.33% as the average. The varia- 
 tions are not so marked among the series of this type as in the cases 
 of the other three soils. The absolute range is nearly as great, but 
 the relative variation is less. 
 
 Even though there are differences between the average CaO con- 
 tent in the several types, the wide variation in the amount found in 
 the several samples of a given type, and the overlapping of these 
 amounts from the different types entirely preclude any statement 
 that as regards the calcium content the soils of any one type are 
 closely similar to one another, or that one type has a higher or lower 
 lime content than another. 
 
1919] 
 
 Pendleton: A Study of Soil Types 
 
 409 
 
 Table 22 — Calcium as CaO 
 (Surface horizons only) 
 
 Bh 
 
 iblo Clay Adobe 
 
 A 
 % 
 
 Altamont Clay 
 
 A 
 
 Loam 
 
 Hanford Fine 
 Loam 
 
 Sandy 
 
 r ~ 
 
 
 % 
 
 % 
 
 % 
 
 % 
 
 1-A 
 
 1.86 
 
 
 3-A 
 
 5.64 
 
 
 14-A 2.91 
 
 
 
 1.80 
 
 1.83 
 
 
 
 5.64 
 
 2.99 
 
 2.95 
 
 2-A 
 
 2.12 
 
 
 4-A 
 
 0.92 
 
 
 15-A 2.98 
 
 
 
 1.98 
 
 2.05 
 
 
 0.88 
 
 0.90 
 
 3.22 
 
 3.10 
 
 5-A 
 
 0.56 
 
 
 7-A 
 
 0.89 
 
 
 16-A 2.48 
 
 
 
 0.17 
 
 0.36 
 
 
 0.67 
 
 0.78 
 
 2.65 
 
 2.56 
 
 6-A 
 
 0.67 
 
 0.67 
 
 A 
 
 verage 
 
 2.44 
 
 19-A 3.28 
 3.17 
 
 3.22 
 
 Average 
 
 1.23 
 
 
 
 
 20-A 2.69 
 
 
 
 
 
 
 
 
 2.73 
 
 2.71 
 
 
 
 
 
 
 
 22-A > 3.80 
 
 
 
 
 
 
 
 
 3.92 
 
 3.86 
 
 
 
 
 
 
 
 23-A 2.88 
 
 
 
 
 
 
 
 
 3.00 
 
 2.94 
 
 
 
 
 
 
 
 24-A 3.88 
 
 
 
 
 
 
 
 
 4.00 
 
 3.94 
 
 
 
 
 
 
 
 25- A 4.58 
 
 
 
 
 
 
 
 
 4.80 
 
 4.69 
 
 
 
 
 
 
 
 Average 
 
 3.33 
 
 Table 23 — Calcium as CaO 
 San Joaquin Sandy Loam 
 Horizon 
 
 Sample 
 
 r 
 A 
 
 % 
 
 Average 
 
 % 
 
 B 
 
 Average 
 
 % 
 
 C 
 
 % 
 
 Average 
 
 % 
 
 10 
 
 0.67 
 
 
 0.82 
 
 
 1.11 
 
 
 
 0.62 
 
 0.64 
 
 1.03 
 
 0.92 
 
 1.12 
 
 1.11 
 
 11 
 
 1.94 
 
 
 1.62 
 
 
 1.65 
 
 
 
 1.26 
 
 1.60 
 
 1.70 
 
 1.66 
 
 1.55 
 
 1.60 
 
 12 
 
 3.12 
 
 
 2.21 
 
 
 2.61 
 
 
 
 3.50 
 
 3.31 
 
 
 2.21 
 
 3.01 
 
 2.81 
 
 13 
 
 2.83 
 
 
 2.38 
 
 
 2.46 
 
 
 
 3.13 
 
 2.98 
 
 2.46 
 
 2.42 
 
 2.79 
 
 2.62 
 
 17 
 
 1.83 
 
 
 1.92 
 
 
 No 
 
 sample 
 
 
 2.08 
 
 1.95 
 
 2.08 
 
 2.00 
 
 
 
 18 
 
 1.40 
 
 
 1.00 
 
 
 1.48 
 
 
 
 1.34 
 
 1.37 
 
 1.45 
 
 1.22 
 
 1.42 
 
 1.45 
 
 21 
 
 0.91 
 
 
 0.89 
 
 
 0.85 
 
 
 
 0.84 
 
 0.87 
 
 0.83 
 
 0.86 
 
 0.89 
 
 0.87 
 
 26 
 
 0.48 
 
 
 0.13 
 
 
 0.17 
 
 
 Avei 
 
 0.47 
 age 
 
 0.47 
 1.65 
 
 0.10 
 
 0.11 
 1.42 
 
 0.17 
 
 0.17 
 1.52 
 
410 
 
 University of California Publications in Agricultural Sciences [Vol. 3 
 
 Magnesium as MgO 
 
 Diablo clay adobe. — This type shows a moderate variability in the 
 magnesium content, with from 1.13% MgO to 3.26%, averaging 
 2.09%. The largest quantity is three times that of the smallest, 
 (tables 24, 25, figs. 15-18). 
 
 Altamont clay loam. — Within the three samples of this type the 
 range in the MgO content is very great, from 0.07% to 1.90%, with 
 the average of 1.05%. The largest is twenty-seven times that of the 
 smallest. 
 
 San Joaquin sandy loam. — The total MgO in the samples of the 
 type is low, considering that some soils reported by Hilgard contain 
 from 1% to 3% magnesia by the acid digestion. The variation within 
 the A horizon is from 0.34% to 0.90%, with the average of 0.62%, i.e., 
 the largest is three times the smallest. The quantities in the B horizon 
 are somewhat erratic as compared with those of the surface, yet in 
 both the B and C horizons the results approach those of the surface 
 sufficiently to give a rough parallelism. The greater amount of clay 
 and fine silts with the increase of depth gives, as one would expect, 
 an increase of magnesium. The average MgO content in the B horizon 
 is 0.81%, and in the C horizon 1.05%. 
 
 Table 24 — Magnesium as MgO 
 (Surface horizon only) 
 
 Diablo Clay Adobe 
 
 j 
 
 ytamont Clav 
 
 A 
 
 Loam 
 
 Hani 
 
 'ord Fine S 
 Loam 
 
 A 
 
 andy 
 
 r 
 
 % 
 
 % 
 
 
 % 
 
 % 
 
 
 % 
 
 % 
 
 1-A 
 
 1.64 
 
 
 3- 
 
 -A 
 
 1.85 
 
 
 14- A 
 
 2.49 
 
 
 
 2.20 
 
 1.92 
 
 
 
 1.95 
 
 1.90 
 
 
 2.49 
 
 2.49 
 
 2-A 
 
 2.16 
 
 
 4- 
 
 -A 
 
 1.21 
 
 
 15-A 
 
 0.93 
 
 
 
 1.95 
 
 2.05 
 
 
 
 1.17 
 
 1.19 
 
 
 1.02 
 
 0.97 
 
 5-A 
 
 1.23 
 
 
 7- 
 
 -A 
 
 0.09 
 
 
 16-A 
 
 1.10 
 
 
 
 1.03 
 
 1.13 
 
 
 
 0.05 
 
 0.07 
 
 
 0.99 
 
 1.04 
 
 6-A 
 
 3.62 
 2.90 
 
 3.26 
 
 
 A 
 
 verage 
 
 1.05 
 
 19- A 
 
 2.11 
 1.99 
 
 2.05 
 
 Average 
 
 2.09 
 
 
 
 
 
 20- A 
 
 1.77 
 1.92 
 
 1.84 
 
 
 
 
 
 
 
 
 22-A 
 
 2.44 
 2.71 
 
 2.57 
 
 
 
 
 
 
 
 
 23-A 
 
 1.94 
 1.70 
 
 1.82 
 
 
 
 
 
 
 
 
 24-A 
 
 2.14 
 2.13 
 
 2.13 
 
 
 
 
 
 
 
 
 25-A 
 
 2.31 
 2.40 
 
 2.35 
 
 
 
 
 
 
 
 
 Average 
 
 1.92 
 
1919] 
 
 Pendleton: A Study of Soil Types 
 
 411 
 
 Han ford fine sandy loam. — The MgO content of the surface soil 
 varies from 0.97% to 2.57%, averaging 1.92%. The relative varia- 
 tion within this type is about that of the Diablo and San Joaquin 
 types. 
 
 Comparing the average amounts of magnesium oxide in the sur- 
 face horizon of the several types, we find the San Joaquin with 0.56%, 
 the Altamont with 1.05%, the Hanford with 1.93%, and the Diablo 
 with 2.09%. The averages do not signify much, however, because of 
 the wide ranges within the types. Therefore as regards magnesium 
 the types are neither distinct nor are the soils within the type 
 closely similar. 
 
 Table 25 — Magnesium as MgO 
 San Joaquin Sandy Loam 
 
 Horizon 
 
 Sample 
 
 A 
 
 % 
 
 Average 
 
 B 
 
 % 
 
 Average 
 
 % 
 
 C 
 
 % 
 
 Average 
 
 % 
 
 10- A 
 
 0.31 
 
 
 0.33 
 
 
 0.53 
 
 
 
 0.30 
 
 0.30 
 
 0.45 
 
 0.39 
 
 0.53 
 
 0.53 
 
 11-A 
 
 0.79 
 
 
 1.21 
 
 
 1.48 
 
 
 
 0.44 
 
 0.61 
 
 1.22 
 
 1.21 
 
 1.25 
 
 1.36 
 
 12- A 
 
 0.83 
 
 
 0.79 
 
 
 1.57 
 
 
 
 0.79 
 
 0.81 
 
 
 0.79 
 
 1.62 
 
 1.59 
 
 13- A 
 
 0.90 
 
 
 1.70 
 
 
 1.67 
 
 
 
 0.80 
 
 0.85 
 
 1.63 
 
 1.66 
 
 1.82 
 
 1.74 
 
 17- A 
 
 0.53 
 
 
 0.51 
 
 
 No sample 
 
 
 0.74 
 
 0.63 
 
 0.77 
 
 0.64 
 
 
 
 18-A 
 
 0.50 
 
 
 0.40 
 
 
 0.64 
 
 
 
 0.48 
 
 0.49 
 
 0.69 
 
 0.54 
 
 0.75 
 
 0.69 
 
 21-A 
 
 0.29 
 
 
 0.28 
 
 
 0.52 
 
 
 
 
 0.29 
 
 0.31 
 
 0.29 
 
 0.56 
 
 0.54 
 
 26-A 
 
 0.50 
 
 
 0.52 
 
 
 0.52 
 
 
 
 0.52 
 
 0.51 
 
 0.44 
 
 0.48 
 
 0.53 
 
 0.52 
 
 Average 
 
 0.56 
 
 
 0.75 
 
 
 1.00 
 
 Phosphorus as P 2 5 
 
 Diablo clay adobe. — The variations in the P 2 5 content in the 
 samples of this type are relatively small, from 0.092% to 0.162%, 
 with 0.108% as the average (tables 26, 27, figs. 11-14). 
 
 Altamont clay loam. — The range of variation in the amount of 
 P 2 5 is large, from 0.031% to 0.265%, the largest quantity being eight 
 times the smallest. The average is 0.132%. 
 
412 University of California Publications in Agricultural Sciences [Vol. 3 
 
 San Joaquin sandy loam. — The variations in the P 2 5 content of 
 the surface soil are from 0.039% to 0.11%, with the average 0.068%. 
 The curve is fairly regular. The subsoils follow the surface in a gen- 
 eral way. The B horizon samples vary in the phosphoric acid con- 
 tent between 0.028% and 0.156%, and average 0.069%. The C sam- 
 ples vary between 0.03% and 0.109%, and average 0.067%. The 
 averages of the three horizons are seen to be almost identical. No 
 particular significance can be attached to the minor variations. 
 
 Hanford fine sandy loam. — The P 2 5 content in the samples of 
 this type is very variable, from 0.195% to 0.819%, with the average 
 of 0.363%. The average of the San Joaquin sandy loam samples is 
 0.069%, of the Diablo clay adobe 0.108%, of the Altamont clay loam 
 0.132%, and of the Hanford fine sandy loam 0.363%. Except between 
 the Diablo and Altamont types these averages would show considerable 
 differences, if it were not that the samples frequently show such wide 
 departures from the averages. The ranges of the several types fre- 
 quently overlap. 
 
 Table 26 — Phosphorus as P 2 5 
 
 (Surface horizon only) 
 
 Hanford Fine Sandy 
 Diablo Clay Adobe Altamont Clay Loam Loam 
 
 A . „ A . A . 
 
 % % % % % % 
 
 1-A 0.088 3-A 0.278 14-A 0.373 
 
 0.096 0.092 0.252 0.265 0.292 0.333 
 
 2-A 0.064 4-A 0.081 15-A 0.287 
 
 0.078 0.071 0.117 0.099 0.260 0.273 
 
 5-A 0.137 7-A 0.034 16-A 0.260 
 
 0.082 0.109 0.028 0.031 0.277 0.268 
 
 6-A 0.143 Average 0.132 19-A 0.303 
 
 0.181 0.162 0.272 0.287 
 
 Average 0.108 20-A 0.190 
 
 0.200 0.195 
 22-A 0.397 
 
 0.401 0.399 
 
 23-A 0.242 
 
 0.270 0.256 
 24- A 0.421 
 
 0.454 0.437 
 25-A 0.879 
 
 0.759 0.819 
 
 Average 0.363 
 
1919] 
 
 Pendleton: A Study of Soil Types 
 
 413 
 
 
 
 Table 27- 
 
 -Phosphorus as P 2 5 
 
 
 
 
 
 San Joaquin Sandy Loam 
 
 
 
 
 
 
 Horizon 
 
 A 
 
 
 
 Sample 
 
 A 
 
 % 
 
 Average 
 
 % 
 
 B 
 
 % 
 
 Average 
 
 % 
 
 C 
 
 % 
 
 Average 
 
 % 
 
 10 
 
 0.118 
 
 
 0.060 
 
 
 0.047 
 
 
 
 0.102 
 
 0.110 
 
 0.068 
 
 0.064 
 
 0.057 
 
 0.052 
 
 11 
 
 0.049 
 
 
 0.047 
 
 
 0.049 
 
 
 
 0.060 
 
 0.054 
 
 0.046 
 
 0.046 
 
 0.028 
 
 0.028 
 
 12 
 
 0.057 
 
 
 0.028 
 
 
 0.064 
 
 
 
 0.071 
 
 0.064 
 
 
 0.028 
 
 0.095 
 
 0.078 
 
 13 
 
 0.049 
 
 
 0.037 
 
 
 0.036 
 
 
 
 0.064 
 
 0.056 
 
 0.038 
 
 0.039 
 
 0.024 
 
 0.030 
 
 17 
 
 0.036 
 
 
 0.041 
 
 
 No sample 
 
 
 0.042 
 
 0.039 
 
 0.082 
 
 0.061 
 
 
 
 18 
 
 0.043 
 
 
 0.097 
 
 
 0.086 
 
 
 
 0.055 
 
 0.049 
 
 0.074 
 
 0.085 
 
 
 0.086 
 
 21 
 
 0.069 
 
 
 0.088 
 
 
 0.094 
 
 
 
 0.068 
 
 0.068 
 
 0.066 
 
 0.077 
 
 0.062 
 
 0.078 
 
 26 
 
 0.117 
 
 
 0.130 
 
 
 0.120 
 
 
 
 0.092 
 
 0.104 
 
 0.182 
 
 0.156 
 
 0.098 
 
 0.109 
 
 Average 
 
 0.068 
 
 
 0.069 
 
 
 0.067 
 
 Potassium as K 2 
 
 Diablo clay adobe. — There is a moderate range in the variation in 
 the amount of K 2 within this type, the lowest amount being 1.48% 
 and the highest 2.06%, the four samples averaging 1.71% (table 28, 
 figs. 15-18). 
 
 Altamont clay loam. — A greater variation, from 1.09% to 2.14%, 
 of K 2 0, occurs in the three samples of this type. The average is 
 1.74%. 
 
 San Joaquin sandy loam. — This type shows the greatest variation, 
 from 0.98% to 2.84%. But even so, the the largest quantity of K 2 
 is less than three times the smallest. 1.88% K 2 is the average of 
 the eight samples. Nos. 11 and 12 of this type show the smallest 
 amounts of K 2 of any of the twenty-four samples. 
 
 Hanford fine sandy loam. — The variation in the K 2 content of 
 the samples of this type is not great — from 1.73% to 3.16%, with 
 the average of 2.33%. This is the highest average, as the Diablo clay 
 adobe samples show 1.71%, the Altamont clay loam 1.74%, and the 
 San Joaquin sandy loam 1.88%. Because of the considerable range 
 in the amounts of K 2 for the several samples of a type, and because 
 of the many overlappings of the values for one type over another, 
 the averages do not mean much and do not show the soils within a 
 type to be closely similar, nor do they show the types distinct. 
 
414 University of California Publications in Agricultural Sciences [Vol. 3 
 
 Table 28 — Potassium as K 2 
 
 (J. Lawrence Smith Method) 
 
 Hanford Fine Sandy 
 
 Dii 
 
 iblo Clay 
 
 Adobe 
 
 Altamont Clay 
 
 Loam 
 
 San Joaqu 
 
 in Sandy Loam 
 
 
 Loam 
 
 
 No. 
 
 % 
 
 Average 
 
 % 
 
 Xo. 
 
 % 
 
 Average 
 
 % 
 
 No. 
 
 % 
 
 Average 
 
 % 
 
 r 
 
 No. 
 
 Average 
 
 % 
 
 1-A 
 
 1.68 
 
 
 3-A 
 
 1.06 
 
 
 14-A 
 
 1.79 
 
 
 10- A 
 
 2.14 
 
 
 
 1.67 
 
 1.67 
 
 
 1.13 
 
 1.09 
 
 
 1.67 
 
 1.73 
 
 
 2.12 
 
 2.13 
 
 2-A 
 
 1.62 
 
 
 4-A 
 
 1.92 
 
 
 15-A 
 
 2.54 
 
 
 11-A 
 
 0.99 
 
 
 
 1.69 
 
 1.65 
 
 
 2.36 
 
 2.14 
 
 
 2.62 
 
 2.58 
 
 
 0.98 
 
 0.98 
 
 5-A 
 
 1.45 
 
 
 7-A 
 
 1.90 
 
 
 16-A 
 
 2.42 
 
 
 12-A 
 
 1.03 
 
 
 
 1.51 
 
 1.48 
 
 
 2.10 
 
 2.00 
 
 
 2.46 
 
 2.44 
 
 
 1.02 
 
 1.02 
 
 6-A 
 
 2.01 
 2.12 
 
 2.06 
 
 A 
 
 verage 
 
 1.74 
 
 I9-A 
 
 2.10 
 2.03 
 
 2.06 
 
 13-A 
 
 1.50 
 
 1.50 
 
 Average 
 
 1.71 
 
 
 
 
 20- A 
 
 2.00 
 
 
 17-A 
 
 2.40 
 
 
 
 
 
 
 
 
 
 1.81 
 
 1.90 
 
 
 2.24 
 
 2.32 
 
 
 
 
 
 
 
 2 2-A 
 
 2.68 
 2.62 
 
 2.65 
 
 18-A 
 
 2.07 
 
 2.28 
 
 2.17 
 
 
 
 
 
 
 
 23-A 
 
 3.10 
 3.23 
 
 3.16 
 
 2 1-A 
 
 2.81 
 
 2.88 
 
 2.84 
 
 
 
 
 
 
 
 24-A 
 
 2.29 
 2.21 
 
 2.25 
 
 2 6-A 
 
 2.04 
 2.09 
 
 2.06 
 
 
 
 
 
 
 
 25-A 
 
 2.18 
 
 
 Average 
 
 1.88 
 
 
 
 
 
 
 
 
 2.21 
 
 2.19 
 
 
 
 
 
 
 
 
 
 
 Average 
 
 2.33 
 
 
 
 
 Bacteriological Data 
 
 The bacteriological work was not entirely satisfactory, partly be- 
 cause the conditions in one of the incubators were not all that might 
 be desired, and partly because of the refractory physical properties 
 of some of the soils. The Diablo and Altamont types, in all three 
 horizons, were very heavy and hard to mix and keep in even fair 
 physical condition. The San Joaquin soils were predominantly of a 
 heavy texture in the B and C horizons, while the surface horizon 
 was light and the crumb structure was entirely lost if even a small 
 excess of water was added to the culture. 
 
 AMMONIFI CATION 
 
 There arc very marked differences between the various types in 
 tli is determination, though the samples in a given type vary among 
 themselves to a large extent. 
 
 Diablo clay adobe. — The highest ammonia production was about 
 three limes the lowest, 7.7 mg. and 26 mg. In both this type and 
 the following, the B and C horizons follow the surface horizon quite 
 
1919] 
 
 Pendleton: A Study of Soil Types 
 
 415 
 
 -a 
 
 £ 40 
 
 O 
 
 ^ 30 
 
 n 
 
 X 
 
 z 
 S 20 
 
 
 
 
 
 \ \ 
 
 
 
 
 — - ^— 
 
 
 N 
 
 
 
 °l £ 5. 6 
 
 Soi Is. 
 
 Fig. 19-A. 
 
 Fig. 19a. Graph showing ammonification in the four samples of Diablo clay 
 adobe. The quantities are expressed in terms of nitrogen produced per 100 
 grams of soil with 2% of dried blood. 
 
 x 
 
 71 
 
 \Q 
 
 15 
 
 SO 
 
 25 
 
 \ 
 
 
 
 ^ 
 
 A 
 
 
 
 
 B^^^" 
 
 
 JZ^~ """" 
 
 ~^c 
 
 
 
 
 A Z. O 6. 
 
 Soils. 
 
 Fiq. 13 -B 
 
 Fig. 19b. Graph showing nitrogen fixation in the three horizons of the four 
 samples of Diablo clay adobe. The quantities are expressed in terms of milli- 
 grams of nitrogen fixed per gram of mannite in 50 grams of soil. 
 
416 
 
 University of California Publications in Agricultural Sciences [Vol. 3 
 
 closely from sample to sample (table 28 and fig. 19a). This may be 
 due to the textures, which are quite similar throughout the soil column. 
 The averages for the three horizons were : A, 18.6 mg. ; B, 12.6 mg. ; 
 and C, 8.9 mg. 
 
 30 
 
 20 
 
 10 
 
 
 3 4 7 Soils 
 
 Mg N. as NH3 Produced 
 
 Fig. 20a. Graph showing ammonifieation in the three horizons of the three 
 samples of Altamont clay loam. 
 
 10. 
 
 7.5 
 B 
 
 
 
 
 
 \ 
 \ 
 
 
 
 
 \ 
 
 V 
 
 N 
 
 \ 
 \ 
 
 
 
 
 W 
 
 \ 
 
 \ 
 
 
 
 
 
 2.5 
 
 3 4 7 Soils 
 
 Mg N. Fixed 
 
 Fig. 20b. Graph showing nitrogen fixation in milligrams in the three horizons 
 of the three samples of Altamont clay loam. 
 
 Altamont clay loam. — As regards horizon A the amount of am- 
 monia produced in one soil is three times that in the lowest, 10 mg. 
 nitrogen and 33 mg. nitrogen as ammonia, with 8.9 mg. as the average 
 (table 30 and fig. 20a). The amount of nitrogen as ammonia pro- 
 duced in the B horizon averaged 12.6 mg., in the C horizon 8.9 mg. 
 
1919] 
 
 Pendleton: A Study of Soil Types 
 
 417 
 
 San Joaquin sandy loam. — The amount of ammonia produced in 
 the A horizon varied between 30.4 mg. of nitrogen and 57.1 mg., the 
 average was 40.2 mg. (table 31 and fig. 21a). The production of 
 ammonia, in milligrams of nitrogen, by the B samples varied between 
 4.5 mg. and 38.1 mg., with 20 mg. as the average. In the C samples 
 the variation was nearly as great, between 5.7 mg. and 32 mg., with 
 the average of 20.9 mg. Thus there are notable variations among the 
 
 12 13 17 18 21 26 Soils 
 
 Mg N. as NH3 produced 
 
 Fig. 21a. Graph showing ammonification in the three horizons of the eight 
 samples of San Joaquin sandy loam. 
 
 samples of this type, the proportional variation being very great, con- 
 sidering the three horizons. Possibly the reason that the B and C 
 horizons are so divergent from the surface is that there is a very 
 marked variation in the texture between the surface horizon and 
 those below the surface. 
 
 Hanford fine sandy loam. — The variation is large here also (table 
 32, fig. 22a), the largest quantity of ammonia produced in the surface 
 soil is twice that of the smallest production, 72 mg. and 35 mg. The 
 subsoil variations, in a general way, parallel those of the surface. 
 The average production of ammonia in the three horizons is as fol- 
 
418 
 
 University of California Publications in Agricultural Sciences [Vol. 3 
 
 lows: A, 56.9 mg. nitrogen; B, 46.3 mg. nitrogen; and C, 38.7 mg. 
 nitrogen. In attempting to correlate the variations in ammonifying 
 powers with the known variations of the soils, or with the known his- 
 tories of the soils, there seem to be no relations of significance. 
 
 The Altamont and Diablo types are about alike in their low am- 
 monifying power. The Hanford and San Joaquin are both higher 
 and nearer to each other than to the two heavy types, yet the Hanford 
 is noticeably higher than the San Joaquin. This is as one would ex- 
 pect, from a knowledge of the soils in the field. Considering the types 
 as a whole, as represented by the A horizon, there are more marked 
 variations between the types than between the samples of a given type 
 though the variations within a given type are very large. 
 
 Average 
 
 
 
 Table 29 — Ammonification 
 
 
 
 
 
 
 Diablo Clay Adobe 
 
 
 
 
 
 Milli 
 
 grams N as 
 
 NH 3 Pi 
 
 -oduced 
 
 
 
 
 A 
 
 A 
 
 
 
 B 
 
 
 
 C 
 
 ( 
 
 Cultures 
 
 Checks 
 average 
 
 Increase 
 
 over 
 
 checks 
 
 Cultures 
 
 Checks 
 average 
 
 Increase 
 
 over 
 checks 
 
 r 
 Cultures 
 
 Increase 
 Checks over 
 average checks 
 
 31.48 
 
 
 
 28.58 
 
 
 
 24.24 
 
 
 40.32 
 
 2.52 
 
 33.38 
 
 22.98 
 
 2.28 
 
 23.50 
 
 14.99 
 
 2.42 17.19 
 
 19.81 
 
 
 
 9.45 
 
 
 
 8.41 
 
 
 17.07 
 
 1.68 
 
 16.76 
 
 9.84 
 
 1.91 
 
 7.73 
 
 9.95 
 
 1.05 8.13 
 
 15.90 
 
 
 
 11.55 
 
 
 
 No sample 
 
 
 1.75 
 
 14.15 
 
 12.54 
 
 1.54 
 
 10.50 
 
 
 
 12.33 
 
 
 
 7.76 
 
 
 
 12.33 
 
 
 3 
 
 2.11 
 
 10.22 
 18.63 
 
 13.55 
 
 2.07 
 
 8.58 
 12.58 
 
 12.33 
 
 2.03 10.30 
 11.87 
 
 Table 30 — Ammonification 
 Altamont Clay Loam 
 
 
 
 
 Milli; 
 
 grams N as 
 
 NH 3 Pi 
 
 reduced 
 
 
 
 
 
 
 A 
 
 A 
 
 
 
 B 
 
 A 
 
 
 
 C 
 
 
 Sample 
 
 r 
 Cultures 
 
 Checks 
 average 
 
 > > 
 
 Increase 
 over 
 checks 
 
 Cultures 
 
 Checks 
 average 
 
 Increase 
 
 over 
 checks 
 
 Cultures 
 
 Checks 
 average 
 
 > 
 
 Increase 
 
 over 
 
 checks 
 
 3 
 
 8.14 
 
 
 
 6.97 
 
 
 
 5.89 
 
 
 
 
 10.58 
 
 1.68 
 
 7.68 
 
 7.15 
 
 1.40 
 
 5.16 
 
 4.91 
 
 1.54 
 
 3.86 
 
 4 
 
 19.75 
 
 
 
 6.59 
 
 
 
 5.41 
 
 
 
 
 19.12 
 
 2.66 
 
 16.77 
 
 6.67 
 
 1.36 
 
 5.27 
 
 5.12 
 
 1.19 
 
 4.07 
 
 7 
 
 28.66 
 
 
 
 19.66 
 
 
 
 8.00 
 
 
 
 
 27.53 
 
 2.03 
 
 26.06 
 
 1 6.25 
 
 1.75 
 
 16.20 
 
 12.37 
 
 1.33 
 
 8.95 
 
 Average 
 
 
 16.84 
 
 
 
 8.88 
 
 
 
 5.63 
 
1919] 
 
 Pendleton: A Study of Soil Types 
 
 419 
 
 Table 31 — Ammonification 
 San Joaquin Sandy Loam 
 Milligrams N as NH 3 Produced 
 B 
 
 Sample 
 10 
 
 Cultures 
 54.24 
 
 Checks 
 average 
 
 Increase 
 
 over 
 
 checks 
 
 r 
 
 Cultures 
 42.63 
 
 Checks 
 average 
 
 Increase 
 
 over 
 checks 
 
 r 
 
 Cultures 
 28.89 
 
 1 
 Checks 
 average 
 
 > 
 ncrease 
 
 over 
 checks 
 
 
 41.95 
 
 1.72 
 
 46.73 
 
 36.11 
 
 1.28 
 
 38.09 
 
 38.25 
 
 1.59 
 
 31.98 
 
 11 
 
 44.47 
 
 
 
 7.47 
 
 
 
 6.05 
 
 
 
 
 73.23 
 
 1.70 
 
 57.15 
 
 12.52 
 
 1.81 
 
 8.18 
 
 6.78 
 
 1.68 
 
 4.78 
 
 12 
 
 44.48 
 
 
 
 18.73 
 
 
 
 10.91 
 
 
 
 
 40.07 
 
 1.56 
 
 40.71 
 
 21.81 
 
 1.50 
 
 18.77 
 
 6.11 
 
 1.14 
 
 7.87 
 
 13 
 
 41.66 
 
 
 
 5.41 
 
 
 
 3.80 
 
 
 
 
 45.04 
 
 1.30 
 
 42.50 
 
 5.36 
 
 0.86 
 
 4.52 
 
 15.17 
 
 0.88 
 
 8.60 
 
 17 
 
 30.19 
 
 
 
 27.59 
 
 
 
 No sample 
 
 
 
 33.88 
 
 1.66 
 
 30.37 
 
 20.68 
 
 1.51 
 
 22.62 
 
 
 
 
 18 
 
 35.04 
 
 
 
 30.56 
 
 
 
 21.96 
 
 
 
 
 35.24 
 
 1.48 
 
 33.66 
 
 22.81 
 
 1.30 
 
 25.38 
 
 16.92 
 
 1.47 
 
 17.97 
 
 21 
 
 34.44 
 
 
 
 37.41 
 
 
 
 25.72 
 
 
 
 
 30.89 
 
 1.48 
 
 31.18 
 
 37.74 
 
 1.38 
 
 36.19 
 
 29.66 
 
 1.42 
 
 26.27 
 
 26 
 
 40.81 
 
 
 
 7.50 
 
 
 
 9.08 
 
 
 
 
 
 1.64 
 
 39.17 
 
 8.41 
 
 1.44 
 
 6.51 
 
 5.43 
 
 1.54 
 
 5.71 
 
 A vera s 
 
 :e 
 
 
 40.18 
 
 
 
 20.03 
 
 
 
 12.89 
 
 Table 32 — Ammonification 
 Hanford Fine Sandy Loam 
 
 Milligrams N as NH 3 Produced 
 B 
 
 Sample 
 
 Cultures 
 
 Checks 
 average 
 
 Increase 
 
 over 
 
 checks 
 
 r 
 Cultures 
 
 Checks 
 
 average 
 
 Horizons 
 
 Increase 
 
 over 
 checks 
 
 r 
 Cultures 
 
 Checks 
 average 
 
 Increase 
 
 over 
 
 checks 
 
 14 
 
 37.35 
 
 
 
 27.96 
 
 
 
 14.39 
 
 
 
 
 43.57 
 
 1.78 
 
 38.68 
 
 48.46 
 
 1.46 
 
 36.75 
 
 41.70 
 
 1.24 
 
 26.80 
 
 15 
 
 33.11 
 
 
 
 45.68 
 
 
 
 59.90 
 
 
 
 
 41.75 
 
 1.75 
 
 35.68 
 
 48.38 
 
 1.70 
 
 45.33 
 
 52.59 
 
 1.62 
 
 54.62 
 
 16 
 
 56.59 
 
 
 
 44.08 
 
 
 
 44.58 
 
 
 
 
 56.77 
 
 1.83 
 
 54.85 
 
 42.10 
 
 1.61 
 
 41.48 
 
 52.10 
 
 1.69 
 
 46.65 
 
 19 
 
 52.92 
 
 
 
 46.70 
 
 
 
 24.56 
 
 
 
 
 51.85 
 
 1.47 
 
 50.91 
 
 38.92 
 
 1.13 
 
 41.68 
 
 28.12 
 
 1.24 
 
 25.10 
 
 20 
 
 72.49 
 
 
 
 45.49 
 
 
 
 22.05 
 
 
 
 
 74.21 
 
 1.36 
 
 71.99 
 
 38.52 
 
 1.03 
 
 40.97 
 
 30.35 
 
 1.00 
 
 25.20 
 
 22 
 
 64.92 
 
 
 
 57.44 
 
 
 
 46.08 
 
 
 
 
 67.56 
 
 1.75 
 
 64.49 
 
 55.34 
 
 1.51 
 
 54.88 
 
 47.55 
 
 1.60 
 
 45.21 
 
 23 
 
 71.56 
 
 
 
 50.84 
 
 
 
 35.15 
 
 
 
 
 68.66 
 
 1.61 
 
 68.50 
 
 43.01 
 
 1.37 
 
 45.55 
 
 35.23 
 
 1.35 
 
 33.84 
 
 24 
 
 65.02 
 
 
 
 50.09 
 
 
 
 37.56 
 
 
 
 
 59.51 
 
 1.50 
 
 60.76 
 
 46.54 
 
 1.32 
 
 46.99 
 
 40.21 
 
 1.33 
 
 37.55 
 
 25 
 
 68.20 
 
 
 
 69.29 
 
 
 
 61.01 
 
 
 
 
 67.29 
 
 1.43 
 
 66.31 
 
 60.03 
 
 1.25 
 
 63.41 
 
 47.70 
 
 1.22 
 
 53.13 
 
 Average 
 
 
 56.91 
 
 
 
 46.34 
 
 
 
 38.67 
 
420 
 
 University of California Publications in Agricultural Sciences [Vol. 3 
 
 Nitrogen Fixations 
 
 Diablo clay adobe. — This type shows the highest quantity of nitro- 
 gen fixed, 9.6 m'g., with the subsoil quantities, much lower than the 
 surface. The variation within the type is seen to be the largest of that 
 in any of the types. 
 
 Altamont clay loam. — The surface samples have 1.0, 4.7, and 9.1 
 mg. nitrogen (table 34 and fig. 20b). The soils shows a wide diver- 
 gence between the surface samples and between the surface and sub- 
 soils. This is to be expected in the heavier soils. 
 
 7.5 
 C 
 
 2.3 
 
 \ 
 
 
 
 
 
 
 
 \ 7* 
 \ 
 \ 
 
 \ \ 
 
 
 
 
 
 
 
 \ 
 
 \ 
 
 \ 
 
 X 
 
 
 ______ _^^+ 
 
 
 ^ 
 
 10 
 
 11 
 
 12 
 
 13 17 
 
 Mg N. Fixed 
 
 IS 
 
 21 
 
 26 Soils 
 
 Fig. 21b. Graph showing nitrogen fixation in the three horizons of the 
 eight samples of San Joaquin sandy loam. 
 
 San Joaquin sandy loam. — The quantity fixed in the A horizon 
 (table 35 and fig. 21b) is small and quite variable. It is between 
 nothing and 5.5 mg., with the average of 1.9 mg. Instead of nitrogen 
 fixation denitrification took place in a number of cases, especially in 
 horizon C. Considering the wide variation in textures of the horizons, 
 it is rather odd that there should not be a greater variation between 
 the soils from the various depths. 
 
 Han ford fine sandy loam. — The amount of nitrogen fixed by the 
 surface soil (table 36, and fig. 22b) averages much higher, 5.7 mg., 
 than that in the San Joaquin sandy loam, though the range of varia- 
 tion is about the same. It is noticeable that the amounts of nitrogen 
 fixed by the B and C horizons of the soils nos. 14 and 19 are much 
 
 28 All of the figures on nitrogen fixation refer to the milligrams of nitrogen 
 fixed per gram of mannite in 50 grams of soil (table 33 and figs. 9-13). 
 
1919] 
 
 Pendleton : A Study of Soil Types 
 
 421 
 
 less (even to denitrification) absolutely and relatively as compared 
 with the surface horizons, than the amount fixed by the B and C 
 horizons of the soils nos. 20 to 25 inclusive. 
 
 Comparing the nitrogen fixation of the various types, there seem 
 to be no characteristic differences between the heavy Altamont and 
 Diablo types, while the lighter Hanford and San Joaquin types are 
 considerably different from each other. As a whole there is but a fair 
 degree of similarity between the samples of a given type. The degree 
 of variation within types is large. 
 
 
 
 
 Table 
 
 33 — Nitrogen Fixation 
 Diablo Clay Adobe 
 
 
 
 
 
 
 
 Millisri 
 
 ams N per 
 
 gram of 
 
 mannite 
 
 
 
 
 
 
 A 
 
 A 
 
 
 
 B 
 
 A 
 
 
 
 C 
 
 A 
 
 
 Sample 
 
 f 
 Cultures 
 
 Checks 
 average 
 
 Increase 
 
 over 
 
 checks 
 
 Cultures 
 
 Checks 
 average 
 
 Increase 
 over 
 
 checks 
 
 r 
 
 Cultures 
 
 Checks 
 average 
 
 Increase 
 
 over 
 
 checks 
 
 1 
 
 60.25 
 
 
 
 31.52 
 
 
 
 22.77 
 
 
 
 
 63.40 
 
 52.22 
 
 9.60 
 
 29.56 
 
 34.67 
 
 -4.13 
 
 24.87 
 
 28.61 
 
 -4.79 
 
 2 
 
 55.34 
 
 
 
 32.92 
 
 
 
 30.47 
 
 
 
 
 49.39 
 
 45.88 
 
 6.48 
 
 38.18 
 
 33.80 
 
 1.75 
 
 32.22 
 
 29.77 
 
 1.57 
 
 5 
 
 48.68 
 
 
 
 35.73 
 
 
 
 
 No sample 
 
 
 48.68 
 
 41.92 
 
 6.76 
 
 37.12 
 
 32.39 
 
 4.03 
 
 
 
 
 6 
 
 45.88 
 
 
 
 39.64 
 
 
 
 35.02 
 
 
 
 
 46.86 
 
 58.49 
 
 -12.12 
 
 42.72 
 
 50.77 
 
 -9.59 
 
 39.01 
 
 39.05 
 
 -2.03 
 
 Average 
 
 
 4.71 
 
 
 
 1.44 
 
 
 
 0.52 
 
 Table 34 — Nitrogen Fixation 
 Altamont Clay Loam 
 
 Milligrams N fixed per gram of mannite 
 B 
 
 Sample 
 
 Cultures 
 
 Checks 
 average 
 
 Increase 
 over 
 
 checks 
 
 r 
 Cultures 
 
 Checks 
 average 
 
 Increase 
 
 over 
 checks 
 
 r 
 Cultures 
 
 Checks 
 average 
 
 Increase 
 
 over 
 
 checks 
 
 3 
 
 71.26 
 
 
 
 49.04 
 
 
 
 37.13 
 
 
 
 
 70.40 
 
 61.71 
 
 9.12 
 
 51.84 
 
 43.78 
 
 6.66 
 
 38.51 
 
 33.76 . 
 
 4.06 
 
 4 
 
 60.25 
 
 
 
 28.02 
 
 
 
 20.31 
 
 
 
 
 52.19 
 
 51.49 
 
 4.73 
 
 27.32 
 
 26.48 
 
 1.19 
 
 21.01 
 
 20.48 
 
 0.18 
 
 7 
 
 52.95 
 
 
 
 37.75 
 
 
 
 30.81 
 
 
 
 
 53.44 
 
 52.12 
 
 1.08 
 
 37.40 
 
 36.60 
 
 1.00 
 
 27.18 
 
 29.94 
 
 -0.94 
 
 Average 
 
 
 4.98 
 
 
 
 2.95 
 
 
 
 1.41 
 
422 University of California Publications in Agricultural Sciences [Vol. 3 
 
 7d 
 
 :.o 
 
 40 
 
 30 
 
 20 
 
 10 
 
 . 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 /^/ 
 
 1 
 
 1 
 1 
 
 N / 
 
 N / 
 
 S / 
 
 
 
 / 
 
 \ 
 \ 
 
 
 / 
 
 /'« 
 
 / / 
 
 t 
 
 1 
 
 1 
 
 1/ 
 
 / \ 
 
 \ 
 \ 
 
 — *— 
 
 
 / 
 / , 
 
 / / 
 
 X 
 
 \ 
 
 \ 
 \ 
 N 
 \ 
 
 -— -"" 
 
 / / 
 
 / 
 / 
 
 / 
 / 
 
 / 
 / 
 / 
 
 
 \ 
 
 \ 
 \ 
 \ 
 
 \ 
 \ 
 
 
 / 
 / 
 / 
 / 
 
 / 
 
 / 
 
 \ 
 
 \ 
 \ 
 \ 
 
 ^" 
 
 / 
 
 / 
 
 < 
 
 
 \ 
 \ 
 
 > 
 
 
 
 / 
 / 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 - 
 
 15 
 
 16 
 
 23 
 
 24 
 
 19 20 22 
 
 Mg N. as NH3 produced 
 Fig. 22a. Graph showing ammonification in the three horizons of the nine 
 samples of Hanford fine sandy loam. 
 
 26 Soils 
 
 10 
 
 7.5 
 
 2.5 
 
 
 
 
 
 
 
 
 
 
 
 
 // 
 
 \\ 
 
 \\ 
 
 
 
 
 
 
 
 / 
 
 
 
 >< 
 
 
 s 
 
 
 
 // 
 
 / 
 / 
 / 
 
 1 
 
 
 
 
 
 
 
 l \ 
 
 23 
 
 21 
 
 15 16 19 20 22 
 
 Mm N. Fixed 
 Pig. 22b. Graph showing nitrogen fixation in the three horizons of the nine 
 sum pies of Hanford fine sandy loam. 
 
 25 Soils 
 
1919] 
 
 Pendleton: A Study of Soil Types 
 
 423 
 
 Table 35 — Nitrogen Fixation 
 San Joaquin Sandy Loam 
 
 Milligrams N fixed per gram of mannite 
 
 
 
 A 
 
 A 
 
 
 
 B 
 
 A 
 
 
 
 C 
 
 
 Sample 
 
 Cultures 
 
 Checks 
 average 
 
 Increase 
 over 
 checks 
 
 r 
 Cultures 
 
 Checks 
 average 
 
 Increase 
 
 over 
 checks 
 
 r 
 Cultures 
 
 Checks 
 average 
 
 Increasi 
 
 over 
 
 checks 
 
 10 
 
 25.01 
 
 
 
 17.16 
 
 
 
 15.83 
 
 
 
 
 23.47 
 
 18.73 
 
 5.51 
 
 16.67 
 
 13.59 
 
 3.32 
 
 18.14 
 
 10.33 
 
 6.65 
 
 11 
 
 27.25 
 
 
 
 22.91 
 
 
 
 21.72 
 
 
 
 
 31.87 
 
 25.15 
 
 4.41 
 
 22.84 
 
 21.78 
 
 1.09 
 
 22.00 
 
 19.43 
 
 2.43 
 
 12 
 
 25.85 
 
 
 
 20.17 
 
 
 
 18.98 
 
 
 
 
 23.82 
 
 23.26 
 
 1.57 
 
 17.09 
 
 16.56 
 
 2.07 
 
 20.10 
 
 20.41 
 
 -0.87 
 
 13 
 
 22.77 
 
 
 
 18.49 
 
 
 
 13.31 
 
 
 
 
 21.58 
 
 20.00 
 
 2.17 
 
 17.86 
 
 20.21 
 
 -2.04 
 
 14.50 
 
 16.35 
 
 -2.45 
 
 17 
 
 13.52 
 13.45 
 
 
 
 9.46 
 10.23 
 
 
 
 
 No samp] 
 
 [e 
 
 18 
 
 15.55 
 
 
 
 8.76 
 
 
 
 9.18 
 
 
 
 
 13.24 
 
 13.73 
 
 0.66 
 
 8.20 
 
 8.09 
 
 0.39 
 
 11.42 
 
 9.74 
 
 0.56 
 
 21 
 
 14.85 
 
 
 
 7.98 
 
 
 
 6.58 
 
 
 
 
 16.11 
 
 14.50 
 
 0.98 
 
 6.44 
 
 5.96 
 
 1.25 
 
 7.28 
 
 7.01 
 
 -0.07 
 
 26 
 
 19.54 
 
 
 
 12.61 
 
 
 
 7.14 
 
 
 
 
 19.34 
 
 20.34 
 
 -0.94 
 
 12.82 
 
 13.34 
 
 -0.72 
 
 7.36 
 
 8.24 
 
 -0.99 
 
 Av 
 
 erage 
 
 
 1.91 
 
 
 
 1.09 
 
 
 
 1.20 
 
 Table 36 — Nitrogen Fixation 
 Hanford Fine Sandy Loam 
 
 
 
 Milligrams 
 
 N fixed per gram 
 
 of mannite 
 
 
 
 
 
 
 A 
 
 A 
 
 
 
 B 
 
 
 
 C 
 
 A 
 
 
 Sample 
 
 r 
 Cultures 
 
 Checks 
 average 
 
 Increase 
 over 
 checks 
 
 r 
 Cultures 
 
 Checks 
 average 
 
 ^ 
 
 Increase 
 
 over 
 checks 
 
 r 
 Cultures 
 
 Checks 
 average 
 
 Increase 
 
 over 
 
 checks 
 
 14 
 
 71.52 
 
 
 
 41.61 
 
 
 
 31.10 
 
 
 
 
 63.05 
 
 59.61 
 
 7.67 
 
 41.69 
 
 41.01 
 
 0.64 
 
 30.19 
 
 29.07 
 
 1.57 
 
 15 
 
 38.18 
 
 
 
 22.07 
 
 
 
 12.40 
 
 
 
 
 29.56 
 
 26.55 
 
 7.32 
 
 21.09 
 
 20.12 
 
 1.46 
 
 14.08 
 
 13.87 
 
 -0.63 
 
 16 
 
 30.33 
 
 
 
 16.46 
 
 
 
 9.67 
 
 
 
 
 32.92 
 
 27.84 
 
 3.78 
 
 16.04 
 
 14.85 
 
 1.40 
 
 8.97 
 
 10.61 
 
 -1.29 
 
 19 
 
 25.56 
 
 
 
 14.43 
 
 
 
 11.77 
 
 
 
 
 26.41 
 
 22.49 
 
 4.49 
 
 13.59 
 
 12.29 
 
 1.72 
 
 12.33 
 
 11.80 
 
 -0.25 
 
 20 
 
 38.04 
 
 
 
 22.84 
 
 
 
 17.09 
 
 
 
 
 38.11 
 
 29.66 
 
 8.41 
 
 23.61 
 
 16.39 
 
 6.83 
 
 20.60 
 
 11.52 
 
 7.32 
 
 22 
 
 35.59 
 
 
 
 22.20 
 
 
 
 17.30 
 
 
 
 
 31.80 
 
 29.17 
 
 4.52 
 
 23.40 
 
 17.23 
 
 5.57 
 
 16.46 
 
 11.87 
 
 5.0T 
 
 23 
 
 38.95 
 
 
 
 19.19 
 
 
 
 11.90 
 
 
 
 
 43.57 
 
 36.10 
 
 5.16 
 
 20.25 
 
 14.57 
 
 5.15 
 
 11.98 
 
 8.90 
 
 3.04 
 
 24 
 
 28.79 
 
 
 
 19.89 
 
 
 
 18.52 
 
 
 
 
 34.61 
 
 25.67 
 
 6.03 
 
 21.52 
 
 16.95 
 
 3.75 
 
 17.51 
 
 13.91 
 
 4.11 
 
 25 
 
 26.55 
 
 
 
 17.86 
 
 
 
 15.55 
 
 
 
 
 26.41 
 
 22.70 
 
 3.78 
 
 17.93 
 
 15.51 
 
 2.38 
 
 13.87 
 
 11.31 
 
 3.41 
 
 Average 
 
 
 5.69 
 
 
 
 3.21 
 
 
 
 2.27 
 
424 
 
 University of California Publications in Agricultural Sciences [Vol.3 
 
 NITRIPICATION29 
 
 The most noticeable thing about the nitrification results is the 
 very wide range of variation in the various representatives of the 
 Hanford fine sandy loam as compared with the quite uniform and 
 consistent results obtained with the other types. 
 
 Diablo clay adobe. — The percentage of nitrogen nitrified (table 
 37, 38, and fig. 23) is uniformly low. The B samples showed a less 
 vigorous nitrifying flora (except in the case of no. 6) than the sur- 
 face ones. Dried blood in the quantities used seems to depress the 
 
 A S. N.+ Cottonseed Meal 
 
 -A S. N.+ (NH 4 ) 2 S04 
 
 
 A S. N. + Dried Blood 
 A Soil Nitrogen 
 
 12 5 6 Soils 
 
 Percentages of N. Nitrified 
 
 Fig. 23. Graph showing the percentages of nitrogen in various nitrogen 
 containing materials nitrified in the four samples of the Diablo clay adobe. 
 
 normal activity (A horizon average 0.81%), while the (NH 4 ) 2 S0 4 
 (A horizon average 3.03%) and the cottonseed meal (A horizon 
 average 2.91%), as compared with the incubated control tend to in- 
 crease the percentage of nitrogen nitrified. It should be kept in mind 
 that an absolute increase in the nitrogen content may accompany a 
 decrease in the percentage, due to the greatly increased amount of 
 nitrogen present after the addition of a nitrogenous substance. The 
 variation of the samples within this type is very moderate as compared 
 with the San Joaquin and Hanford types. 
 
 29 The figures used in the discussion shows the percentages of the nitrogen in 
 the cultures which were nitrified. There are two tables for the samples of each 
 type. The percentages of nitrogen nitrified are rearranged in a second table for 
 greater ease in comparing results. 
 
1919] 
 
 Pendleton: A Study of Soil Types 
 
 425 
 
 Altamont clay loam. — The percentages of nitrogen nitrified (tables 
 39 and 40, fig. 24) are as a whole lower than in the Diablo soils. A 
 similar relative effect of the several nitrogenous materials is seen, for 
 (NH 4 ) 2 S0 4 is first, cottonseed meal, second, the soil's own nitrogen 
 third, and dried blood fourth in the percentages of nitrates produced. 
 As in the Diablo soils the variation is not great from soil to soil. 
 
 San Joaquin sandy loam. — A wide range of variation (tables 41, 
 42, and fig. 25), from 1.2% £o 4.5%, is found in the incubated control, 
 possibly due, in part, to the considerable variations in the physical 
 nature of the samples. The relative action of the nitrogenous ma- 
 
 
 A S. N.+ (NH 4 ) 2 S04 
 A S. N. +Cottonseed Meal 
 A Soil Nitrogen 
 A S. N. + Dried Blood 
 4 7 Soils 
 
 Percentages of N. Nitrified 
 Fig. 24. Graph showing the percentages of nitrogen in various nitrogen 
 containing materials nitrified in the three samples of the Altamont clay loam. 
 
 terials in the soils of the San Joaquin samples as compared with that 
 in the Diablo and Altamont soils is well shown by the following aver- 
 ages of the A horizon: dried blood had 0.02%. cottonseed meal had 
 0.33%, and ammonium sulfate had 0.56% of the nitrogen nitrified, 
 while the incubated control had 2.47% nitrified. The soils are normally 
 low in nitrogen, and this, together with the poor physical condition, 
 made an unfavorable medium for any bacterial activity. This applies 
 especially to horizons B and C. 
 
 Han ford fine sandy loam. — This is by far the most inexplicable 
 set of results in the nitrification studies (tables 43, 44, and fig. 26). 
 The physical nature of this type is admirably suited for bacteriological 
 tumbler cultures, the soil being friable, not puddling readily, and 
 while in the incubator may be kept at the approximately optimum 
 moisture content with little difficulty. This property is fairly con- 
 
426 University of California Publications in Agricultural Sciences [Vol. 3 
 
 stant throughout all the samples (except no. 14) and cannot well 
 be supposed to affect the results greatly. No. 14 has a low nitrifying 
 power throughout, but it is not representative of the type, for it is 
 heavier in texture than the rest. Moreover, it had been submerged 
 by river overflows shortly before the collection of the sample. One 
 would expect these factors to influence the numbers and the activity 
 of the bacterial flora. There is but little similarity in the way the 
 different samples of the A or B horizons behave toward any given 
 
 
 
 
 
 / 
 
 -— _ 
 
 \ 
 
 
 
 
 
 / 
 
 / 
 
 
 \ 
 
 \ 
 
 
 
 
 
 / 
 
 
 \ 
 
 / 
 
 / 
 
 \ 
 
 
 
 / 
 
 / 
 
 
 \ 
 
 \ 
 
 / 
 
 / 
 
 \ 
 
 ^ 
 
 
 
 
 v^ 
 
 
 
 
 
 
 
 \ 
 
 ""•N 
 
 '^^" 
 
 
 
 
 
 
 
 A. Soil Nitrogen 
 
 A. S. N.+ (NHO2SO4 
 
 S. N. -{-Cottonseed Meal 
 
 10 
 
 12 
 
 21 
 
 26 Soils 
 
 13 17 18 
 
 Percentages of N. Nitrified 
 
 Fig. 25. Graph showing the percentages of nitrogen in various nitrogen 
 containing materials nitrified in the eight samples of the San Joaquin sandy 
 loam. 
 
 nitrogen containing material. Variations from 1% to 50%, from 
 0% to 14%, from 4.5% to 8%, or from 15% to 15.5% from soil to 
 soil, without regularity, give slight basis for generalizations. The 
 average effect of the A horizon samples of the Hanford fine sandy 
 loam as regards the several nitrogenous materials is as follows : dried 
 blood, 5.62%; cottonseed meal, 13.72%; ammonium sulfate, 3.29%; 
 incubated control, 1.55%. In a general way there is a similarity 
 between the effects of a given nitrogen containing material on the 
 surface sample, and on the B horizon. This should be so, since these 
 soils are very deep and uniform in texture. However, in the C 
 horizon there were still greater decreases in the bacterial activity. 
 
1919] 
 
 Pendleton: A Study of Soil Types 
 
 427 
 
 As regards nitrification in general there is difficulty in showing 
 any greater resemblance between the samples of a type than there is 
 from type to type. In certain features, however, the types are some- 
 what distinct : ( 1 ) The relation of the nitrification of the soil 's own 
 nitrogen to the soil's action upon added nitrogen is rather distinct 
 for the types. The normal soil in the San Joaquin type gave a much 
 larger per cent of nitrogen than did the soil plus the added nitrogen 
 containing materials. In the Diablo type (fig. 25) the normal soil 
 was about midway in its production as compared with the soils to 
 which the nitrogenous materials were added. In the Hanford fine 
 sandy loam the normal soils gave a much lower percentage nitrifica- 
 tion than in the greater number of instances where the soils were 
 treated with nitrogenous materials. (2) The relative nitrification of 
 the various nitrogenous materials is somewhat distinct for the types. 
 The Diablo, Altamont, and San Joaquin show the ammonium sulfate 
 first, with the cottonseed meal second, and the dried blood third. The 
 Hanford type shows cottonseed meal first, with dried blood second and 
 ammonium sulfate third. 
 
 Table 37 — Nitrification 
 Diablo Clay Adobe 
 
 
 Soil nitrogen 
 
 a 
 
 Soil nitrogen and 
 ammonium sulfate 
 
 A 
 
 Soil nitrogen : 
 dried blood 
 
 A 
 
 and 
 
 Soil nitrogen and 
 cottonseed meal 
 
 A 
 
 Sample 
 
 6 si 
 
 11 
 
 o 
 w . 
 
 a. bfl 
 
 'as 
 
 _, o 
 Eh 
 
 > 
 
 si 
 
 6 si 
 
 ®tJ 
 
 « s 
 
 u $ 
 
 0) 
 
 <k si 
 _ o 
 
 n <° 
 
 o.S 
 
 s>d£ 
 
 O li 
 
 o si 
 
 to • 
 a> Suo 
 
 o.S 
 
 6H 
 
 O U 
 
 o si 
 
 <Dntf 
 
 If 
 
 a> si 
 
 £•1 
 « w 
 
 o.S 
 
 za 
 
 g' 5 
 
 1-A 
 
 0.90 
 
 104.43 
 
 0.86 
 
 5.35 
 
 146.82 
 
 3.65 
 
 2.20 
 
 347.22 
 
 0.63 
 
 5.00 
 
 198.42 
 
 2.50 
 
 1-B 
 
 0.28 
 
 93.34 
 
 0.30 
 
 0.77 
 
 135.74 
 
 0.57 
 
 Tr. 
 
 336.14 
 
 
 Tr. 
 
 187.34 
 
 
 1-C 
 
 0.19 
 
 57.22 
 
 0.33 
 
 0.25 
 
 99.62 
 
 0.25 
 
 0.07 
 
 300.02 
 
 0.02 
 
 0.16 
 
 151.22 
 
 
 2-A 
 
 0.47 
 
 91.76 
 
 0.51 
 
 3.47 
 
 134.16 
 
 2.58 
 
 4.07 
 
 334.56 
 
 1.22 
 
 6.82 
 
 185.76 
 
 3.77 
 
 2-B 
 
 0.33 
 
 67.60 
 
 0.49 
 
 1.17 
 
 110.00 
 
 1.06 
 
 0.08 
 
 310.40 
 
 
 0.19 
 
 161.60 
 
 0.12 
 
 2-C 
 
 0.59 
 
 59.54 
 
 
 0.29 
 
 101.94 
 
 
 0.80 
 
 302.34 
 
 
 0.80 
 
 153.54 
 
 
 5-A 
 
 0.47 
 
 83.82 
 
 0.56 
 
 3.81 
 
 126.22 
 
 3.02 
 
 1.66 
 
 326.62 
 
 0.51 
 
 3.76 
 
 177.82 
 
 2.12 
 
 5-B 
 
 0.36 
 
 64.78 
 
 0.56 
 
 0.42 
 
 107.18 
 
 0.39 
 
 0.19 
 
 307.58 
 
 0.06 
 
 0.97 
 
 158.78 
 
 0.61 
 
 6-A 0.59 116.58 0.51 
 6-B 1.65 101.54 1.63 
 6-C 0.96 78.10 1.23 
 
 4.58 158.98 2.88 
 
 3.00 143.94 2.08 
 
 1.01 120.50 0.84 
 
 3.13 359.38 0.87 
 1.19 344.34 0.35 
 0.37 320.90 0.01 
 
 6.88 210.58 3.26 
 4.55 195.54 2.32 
 0.47 172.10 0.27 
 
I 
 
 428 
 
 University of California Publications in Agricultural Sciences [Vol. 3 
 
 55 
 
 
 
 
 
 
 
 
 
 oil 
 
 1 
 
 \ 
 
 
 
 
 
 
 
 4o 
 
 \ 
 
 \ 
 
 
 
 
 
 
 
 40 
 
 \ 
 
 \ 
 
 
 
 
 
 
 
 35 
 
 \ 
 
 1 
 
 
 
 
 
 
 
 o! ) 
 
 \ 
 
 1 
 
 
 
 
 
 
 
 J.J 
 
 \ 
 
 1 
 
 
 
 
 
 
 
 20 
 
 \ 
 
 1 
 
 
 
 
 
 
 
 1.) 
 
 \ 
 
 1 
 
 
 ! 
 
 \ 
 
 
 
 
 Jo 
 
 \ 
 
 \ 
 
 
 
 
 
 s 
 
 
 5 
 
 
 -^ 
 
 s 
 
 
 / \ 
 
 / \ 
 
 
 s 
 
 s . 
 
 -v 
 
 
 
 
 15 
 
 L6 
 
 23 
 
 24 
 
 Fig. 26. 
 containing 
 loam. 
 
 17 20 22 
 
 Percentages of N. Nitrified 
 
 Graph showing the percentages of nitrogen in various nitrogen 
 materials nitrified in the nine samples of the Hanford fine sandy 
 
 A S. N. + Cottonseed 
 Meal 
 
 ^ A S. N.+ (NH 4 ) 2 S04 
 A Soil Nitrogen 
 A S. N. + Dried Blood 
 
 25 Soils 
 
1919] 
 
 Pendleton: A Study of Soil Types 
 
 429 
 
 Sample 
 1 
 2 
 5 
 6 
 Average 
 
 A 
 0.86 
 0.51 
 0.56 
 0.51 
 0.61 
 
 Table 38 — Nitrification — Percentages of Nitrogen Nitrified 
 
 Diablo Clay Adobe 
 
 Soil nitrogen and Soil nitrogen Soil nitrogen 
 
 Soil nitrogen ammonium sulfate and dried blood cottonseed meal 
 
 — * , , a * , a ; , a * 
 
 BC ABC ABC ABC 
 
 0.30 0.33 3.65 0.57 0.25 0.63 0.02 2.50 
 
 0.49 2.58 1.06 1.22 3.77 0.12 
 
 0.56 3.02 0.39 0.51 0.06 2.12 0.61 
 
 1.63 1.23 2.88 2.08 0.84 0.87 0.35 0.01 3.26 2.32 0.27 
 
 0.74 0.52 3.03 1.02 0.36 0.81 0.10 0.01 2.91 0.76 0.09 
 
 Table 39 — Nitrification 
 Altamont Clay Loam 
 
 
 So 
 
 il nitrogei 
 
 A 
 
 i 
 
 Soil nitrogen and 
 ammonium sulfate 
 
 Soil nitrogen and 
 dried blood 
 
 A 
 
 Soil nitrogen and 
 cottonseed meal 
 
 A 
 
 
 6 &i 
 
 CO • 
 
 eg 
 
 u S 
 
 CD 
 
 a> be 
 
 
 6 tx 
 
 CD 
 
 CD fafi 
 
 
 6 tx 
 
 CD 
 
 tffl 
 0- fcJD 
 
 $ 
 
 J--T3 
 
 Sample 
 
 If 
 
 _ O 
 ^3 cc 
 
 o h 
 
 ®T3 
 
 _ o 
 
 O U 
 
 1* 
 
 Is 
 
 _ o 
 Is M 
 o.S 
 
 Eh 
 
 o u 
 
 IS 
 
 ^_ o 
 
 • ©.a 
 
 
 3-A 
 
 0.60 
 
 123.42 
 
 0.49 
 
 4.12 
 
 165.82 
 
 2.49 
 
 1.17 
 
 366.22 
 
 0.32 
 
 3.57 
 
 217.42 
 
 1.64 
 
 3-B 
 
 0.04 
 
 87.56 
 
 0.05 
 
 0.39 
 
 129.96 
 
 0.32 
 
 0.18 
 
 330.36 
 
 
 0.03 
 
 181.56 
 
 
 3-C 
 
 0.27 
 
 67.52 
 
 0.40 
 
 0.20 
 
 109.92 
 
 0.18 
 
 0.10 
 
 310.32 
 
 
 0.10 
 
 161.52 
 
 
 4-A 
 
 1.30 
 
 102.58 
 
 1.27 
 
 2.95 
 
 144.98 
 
 2.05 
 
 2.34 
 
 345.38 
 
 0.68 
 
 4.83 
 
 196.58 
 
 2.46 
 
 4-B 
 
 0.45 
 
 52.96 
 
 0.85 
 
 
 95.36 
 
 
 0.10 
 
 295.76 
 
 
 
 146.96 
 
 
 4-C 
 
 
 40.96 
 
 
 
 83.36 
 
 
 
 283.76 
 
 
 0.20 
 
 134.96 
 
 0.15 
 
 7-A 
 
 0.50 
 
 104.24 
 
 0.48 
 
 1.35 
 
 146.64 
 
 0.93 
 
 0.40 
 
 347.04 
 
 0.12 
 
 1.27 
 
 198.24 
 
 0.64 
 
 7-B 
 
 0.25 
 
 73.20 
 
 0.34 
 
 0.32 
 
 115.60 
 
 0.28 
 
 
 316.00 
 
 
 
 167.20 
 
 
 7-C 
 
 
 59.88 
 
 
 
 102.28 
 
 
 
 302.68 
 
 
 
 153.88 
 
 
 Table 40 — Nitrification — Percentages of Nitrogen Nitrified 
 Altamont Clay Loam 
 
 
 Soil nitrogen 
 ABC 
 
 Soil nitrogen and 
 ammonium sulfate 
 
 A 
 
 Soil 
 and d: 
 
 nitrogen 
 ried blood 
 
 Soil nitrogen and 
 cottonseed meal 
 
 A 
 
 Sample 
 
 A 
 
 B 
 
 ^ 
 
 c 
 
 A 
 
 B C 
 
 A B 
 
 C 
 
 3 
 
 0.49 
 
 0.05 
 
 0.40 
 
 2.49 
 
 0.32 
 
 0.18 
 
 0.32 
 
 
 1.64 
 
 
 4 
 
 1.27 
 
 0.85 
 
 
 2.05 
 
 
 
 0.68 
 
 
 2.46 
 
 0.15 
 
 7 
 
 0.48 
 
 0.34 
 
 
 0.93 
 
 0.28 
 
 
 0.12 
 
 
 0.64 
 
 
 Average 
 
 0.75 
 
 0.41 
 
 0.13 
 
 1.82 
 
 0.20 
 
 0.06 
 
 0.37 
 
 
 1.58 
 
 0.05 
 
430 
 
 University of California Publications in Agricultural Sciences [Vol. 3 
 
 Table 41 — Nitrification 
 San Joaquin Sandy Loam 
 
 
 Soil nitrogen 
 
 Soil nitrogen and 
 ammonium sulfate 
 
 Soil 
 
 nitrogen and 
 Iried blood 
 
 Soil nitrogen and 
 cottonseed meal 
 
 A 
 
 Sample 
 
 10- A 
 
 O bi 
 
 0.52 
 
 a3 
 a> bi 
 
 &a 
 
 _ o 
 
 n * 
 
 Eh 
 
 37.46 
 
 o u 
 
 u *> 
 
 1.4 
 
 o si 
 
 s a 
 
 0.24 
 
 03 • 
 a> bSt 
 
 'aa 
 |.a 
 
 122.26 
 
 %8 
 
 y 
 
 p U 
 
 0.2 
 
 6 si 
 
 is 
 
 0.06 
 
 Xfl • 
 
 <a he 
 
 'as 
 ©.a 
 
 En 
 302.46 
 
 Sol 
 
 O U 
 I" 
 
 0.02 
 
 6 m 
 
 ^a 
 £% 
 
 0.10 
 
 <v bt 
 
 £a 
 
 _ o 
 
 |.S 
 121.46 
 
 y 
 
 p ^ 
 
 I* 
 
 0.08 
 
 10-B 
 
 0.23 
 
 27.18 
 
 0.9 
 
 0.08 
 
 111.98 
 
 0.07 
 
 
 292.18 
 
 
 
 111.18 
 
 
 10-C 
 
 0.07 
 
 20.66 
 
 0.3 
 
 0.06 
 
 105.46 
 
 0.06 
 
 
 285.66 
 
 
 0.08 
 
 104.66 
 
 0.08 
 
 11-A 
 
 1.25 
 
 50.30 
 
 2.5 
 
 0.50 
 
 135.10 
 
 0.4 
 
 0.27 
 
 315.30 
 
 0.09 
 
 0.95 
 
 134.30 
 
 0.7 
 
 11-B 
 
 
 41.56 
 
 
 0.02 
 
 126.36 
 
 
 0.08 
 
 306.56 
 
 0.03 
 
 0.02 
 
 125.56 
 
 
 11-C 
 
 0.14 
 
 38.86 
 
 0.4 
 
 Tr. 
 
 123.66 
 
 
 Tr. 
 
 303.86 
 
 
 Tr. 
 
 122.86 
 
 
 12- A 
 
 0.80 
 
 46.52 
 
 1.7 
 
 0.55 
 
 131.32 
 
 0.4 
 
 0.09 
 
 311.52 
 
 0.03 
 
 2.05 
 
 130.52 
 
 1.6 
 
 12-B 
 
 0.18 
 
 33.12 
 
 0.5 
 
 0.11 
 
 117.92 
 
 0.09 
 
 Tr. 
 
 298.12 
 
 
 Tr. 
 
 117.12 
 
 
 12-C 
 
 0.14 
 
 40.82 
 
 0.3 
 
 0.06 
 
 125.62 
 
 
 0.06 
 
 305.82 
 
 
 0.06 
 
 124.82 
 
 
 13-A 
 
 0.49 
 
 40.00 
 
 1.2 
 
 0.59 
 
 124.80 
 
 0.5 
 
 0.07 
 
 305.00 
 
 0.02 
 
 0.10 
 
 124.00 
 
 0.08 
 
 13-B 
 
 0.06 
 
 40.41 
 
 
 0.10 
 
 125.21 
 
 0.08 
 
 0.21 
 
 305.41 
 
 
 0.69 
 
 124.41 
 
 
 13-C 
 
 0.35 
 
 32.70 
 
 1.1 
 
 0.25 
 
 117.50 
 
 0.2 
 
 0.00 
 
 297.70 
 
 
 0.96 
 
 116.70 
 
 
 17-A 
 
 0.54 
 
 28.92 
 
 1.9 
 
 0.45 
 
 113.72 
 
 0.4 
 
 Tr. 
 
 293.92 
 
 
 
 112.92 
 
 
 17-B 
 
 
 18.42 
 
 
 
 103.22 
 
 
 Tr. 
 
 283.42 
 
 
 0.08 
 
 102.42 
 
 0.08 
 
 18- A 
 
 1.25 
 
 27.46 
 
 4.5 
 
 1.00 
 
 112.26 
 
 0.9 
 
 
 292.46 
 
 
 Tr. 
 
 111.46 
 
 
 18-B 
 
 Tr. 
 
 16.18 
 
 
 Tr. 
 
 100.98 
 
 
 Tr. 
 
 281.18 
 
 
 Tr. 
 
 100.18 
 
 
 18-C 
 
 
 19.48 
 
 
 0.10 
 
 104.28 
 
 1.0 
 
 
 284.48 
 
 
 
 103.48 
 
 
 21-A 
 
 1.25 
 
 29.00 
 
 4.3 
 
 1.30 
 
 113.80 
 
 1.1 
 
 Tr. 
 
 294.00 
 
 
 0.13 
 
 113.00 
 
 
 21-B 
 
 
 11.92 
 
 
 
 96.72 
 
 
 
 276.92 
 
 
 
 95.92 
 
 
 21-C 
 
 0.01 
 
 14.02 
 
 
 0.01 
 
 98.82 
 
 0.01 
 
 0.15 
 
 279.02 
 
 
 0.15 
 
 98.02 
 
 
 26-A 
 
 0.95 
 
 40.68 
 
 2.3 
 
 0.80 
 
 125.48 
 
 0.6 
 
 Tr. 
 
 305.68 
 
 
 0.19 
 
 124.68 
 
 0.10 
 
 26-B 
 
 Tr. 
 
 26.28 
 
 
 
 111.48 
 
 
 Tr. 
 
 291.68 
 
 
 Tr. 
 
 110.68 
 
 
 26-C 
 
 
 16.48 
 
 
 
 101.28 
 
 
 Tr. 
 
 281.48 
 
 
 
 100.48 
 
 
 Table 42 — Nitrification — Percentages of Nitrogen Nitrified 
 San Joaquin Sandy Loam 
 
 
 Soil 
 
 nitrogen 
 
 Soil nitrogen and 
 ammonium sulfate 
 
 Soil nitrogen 
 and dried blood 
 
 A 
 
 Soil nitrogen and 
 cottonseed meal 
 
 Sample 
 
 r 
 
 A 
 
 B 
 
 c N 
 
 ' A 
 
 B 
 
 c ' 
 
 r 
 A 
 
 B C 
 
 A 
 
 B 
 
 c' 
 
 10 
 
 1.4 
 
 0.9 
 
 0.3 
 
 0.2 
 
 0.07 
 
 0.06 
 
 0.02 
 
 
 0.08 
 
 
 0.08 
 
 11 
 
 2.5 
 
 
 0.4 
 
 0.4 
 
 
 
 0.09 
 
 0.03 
 
 0.7 
 
 
 
 12 
 
 1.7 
 
 0.5 
 
 0.3 
 
 0.4 
 
 0.09 
 
 
 0.03 
 
 
 1.6 
 
 
 
 13 
 
 1.2 
 
 
 1.1 
 
 0.5 
 
 0.08 
 
 0.20 
 
 0.02 
 
 
 0.08 
 
 
 
 17 
 
 1.9 
 
 
 
 0.4 
 
 
 
 
 
 
 0.08 
 
 
 18 
 
 4.5 
 
 
 
 0.9 
 
 
 1.00 
 
 
 
 
 
 
 21 
 
 4.3 
 
 
 
 1.1 
 
 
 0.01 
 
 
 
 0.10 
 
 
 
 26 
 
 2.3 
 
 
 
 0.6 
 
 
 
 
 
 0.1 
 
 
 
 Average 
 
 2.47 
 
 0.17 
 
 0.3 
 
 0.56 
 
 0.03 
 
 0.18 
 
 0.02 
 
 
 0.33 
 
 0.01 
 
 0.01 
 
1919] 
 
 Pendleton: A Study of Soil Types 
 
 431 
 
 Table 43 — Nitrification 
 Eanford Fine Sandy Loam 
 
 Soil nitrogen 
 
 Soil nitrogen and 
 ammonium sulfate 
 
 A 
 
 Soil nitrogen and 
 dried blood 
 
 A 
 
 Soil nitrogen and 
 cottonseed meal 
 
 r - 
 o &i 
 
 c 
 
 ce . 
 
 O bE 
 
 
 O bi 
 
 c 
 
 CO . 
 
 as 
 
 
 o bi 
 
 ^ a 
 
 $ bi) 
 
 
 t — 
 
 O M 
 
 w 
 <U bJD 
 
 fl'g 
 
 |§ 
 
 Sample 2 
 
 _ o 
 o.S 
 
 &S 
 
 O S-, 
 
 ©T3 
 
 o.S 
 Eh 
 
 
 "S © 
 
 £3 
 
 o.S 
 Eh 
 
 I 5 
 
 OT3 
 
 11 
 1* 
 
 o.S 
 
 Eh 
 
 O U 
 
 14-A 0.20 
 
 119.22 
 
 
 
 0.25 
 
 161.62 
 
 0.1 
 
 10.35 
 
 254.22 
 
 4.1 
 
 1.85 
 
 166.22 
 
 i.i 
 
 14-B 0.45 
 
 82.02 
 
 
 0.42 
 
 124.42 
 
 
 0.23 
 
 217.02 
 
 
 0.48 
 
 129.02 
 
 
 14-C 0.07 
 
 58.14 
 
 0.1 
 
 0.75 
 
 100.54 
 
 0.7 
 
 0.15 
 
 193.14 
 
 0.1 
 
 0.10 
 
 105.14 
 
 0.1 
 
 15- A 1.45 
 
 53.10 
 
 2.7 
 
 3.20 
 
 95.50 
 
 . 3.4 
 
 0.40 
 
 188.10 
 
 0.2 
 
 50.85 
 
 100.10 
 
 50.8 
 
 15-B 0.18 
 
 40.24 
 
 0.4 
 
 0.19 
 
 82.64 
 
 0.2 
 
 Tr. 
 
 175.24 
 
 
 1.42 
 
 87.24 
 
 1.6 
 
 15-C 0.03 
 
 27.74 
 
 0.1 
 
 0.01 
 
 70.14 
 
 
 Tr. 
 
 162.74 
 
 
 0.03 
 
 74.74 
 
 
 16-A 0.87 
 
 55.68 
 
 1.6 
 
 2.50 
 
 98.08 
 
 2.5 
 
 0.50 
 
 190.68 
 
 0.2 
 
 4.60 
 
 102.68 
 
 4.5 
 
 16-B 0.11 
 
 29.70 
 
 0.4 
 
 0.08 
 
 72.10 
 
 0.1 
 
 Tr. 
 
 164.70 
 
 
 3.70 
 
 76.70 
 
 4.8 
 
 16-C 0.03 
 
 21.22 
 
 0.1 
 
 Tr. 
 
 63.62 
 
 
 0.05 
 
 156.22 
 
 
 0.17 
 
 68.22 
 
 0.2 
 
 19-A 1.00 
 
 44.98 
 
 2.2 
 
 2.03 
 
 87.38 
 
 2.3 
 
 0.21 
 
 179.98 
 
 0.1 
 
 7.48 
 
 91.98 
 
 8.1 
 
 19-B 0.08 
 
 24.58 
 
 0.3 
 
 0.12 
 
 66.98 
 
 0.2 
 
 
 159.58 
 
 
 0.20 
 
 71.58 
 
 0.3 
 
 19-C 0.16 
 
 23.60 
 
 0.7 
 
 0.15 
 
 66.00 
 
 0.2 
 
 Tr. 
 
 158.60 
 
 
 0.20 
 
 70.60 
 
 0.3 
 
 20-A 0.77 
 
 59.32 
 
 1.3 
 
 1.24 
 
 101.72 
 
 1.2 
 
 27.39 
 
 194.32 
 
 14.1 
 
 6.19 
 
 104.32 
 
 5.9 
 
 20-B 0.12 
 
 32.78 
 
 0.4 
 
 0.11 
 
 75.18 
 
 0.1 
 
 15.50 
 
 167.78 
 
 9.2 
 
 1.45 
 
 77.78 
 
 1.9 
 
 20-C 
 
 23.04 
 
 
 
 65.44 
 
 
 
 158.04 
 
 
 0.07 
 
 68.04 
 
 0.1 
 
 22-A 0.83 
 
 58.34 
 
 1.4 
 
 6.48 
 
 100.74 
 
 6.4 
 
 2.68 
 
 193.34 
 
 1.4 
 
 13.58 
 
 103.34 
 
 13.1 
 
 22-B 0.27 
 
 34.46 
 
 0.8 
 
 0.26 
 
 76.86 
 
 0.3 
 
 0.04 
 
 169.46 
 
 0.02 
 
 1.91 
 
 79.46 
 
 2.4 
 
 22-C 0.85 
 
 23.74 
 
 3.6 
 
 5.40 
 
 66.14 
 
 8.2 
 
 0.52 
 
 158.74 
 
 0.3 
 
 2.50 
 
 68.74 
 
 3.6 
 
 23-A 1.45 
 
 72.20 
 
 2.0 
 
 8.95 
 
 114.6 
 
 7.8 
 
 37.25 
 
 207.20 
 
 17.9 
 
 18.25 
 
 117.20 
 
 15.5 
 
 23-B 0.75 
 
 29.14 
 
 2.6 
 
 8.90 
 
 71.54 
 
 12.5 
 
 0.47 
 
 164.14 
 
 0.3 
 
 2.65 
 
 74.14 
 
 3.6 
 
 23-C 0.32 
 
 17.80 
 
 1.8 
 
 12.40 
 
 60.20 
 
 20.6 
 
 0.02 
 
 152.80 
 
 0.01 
 
 1.30 
 
 62.80 
 
 2.1 
 
 24-A 0.80 
 
 51.34 
 
 1.6 
 
 4.10 
 
 93.74 
 
 4.4 
 
 22.35 
 
 186.34 
 
 11.9 
 
 14.35 
 
 96.34 
 
 14.9 
 
 24-B 0.03 
 
 33.90 
 
 0.1 
 
 0.36 
 
 76.30 
 
 0.5 
 
 0.46 
 
 168.90 
 
 0.3 
 
 5.91 
 
 78.90 
 
 7.5 
 
 24-C 0.33 
 
 27.82 
 
 1.1 
 
 0.33 
 
 70.22 
 
 0.5 
 
 0.63 
 
 162.82 
 
 0.4 
 
 0.73 
 
 72.82 
 
 1.0 
 
 2 5- A 0.56 
 
 45.40 
 
 1.2 
 
 1.30 
 
 87.80 
 
 1.5 
 
 1.30 
 
 180.40 
 
 0.7 
 
 8.65 
 
 90.40 
 
 9.6 
 
 25-B 0.32 
 
 31.01 
 
 1.0 
 
 0.32 
 
 73.41 
 
 0.4 
 
 Tr. 
 
 166.01 
 
 
 0.05 
 
 76.01 
 
 0.06 
 
 25-C 0.11 
 
 22.62 
 
 0.5 
 
 0.16 
 
 65.02 
 
 0.2 
 
 Tr. 
 
 157.62 
 
 
 Tr. 
 
 67.62 
 
 
 Table 44 — Nitrification — Percentages of Nitrogen Nitrified 
 Hanford Fine Sandy Loam 
 
 
 Soil nitrogen 
 
 Soil nitrogen and 
 ammonium sulfate 
 
 Soil nitrogen 
 and dried blood 
 
 Soil nitrogen and 
 cottonseed meal 
 
 Sample 
 
 A 
 
 B 
 
 C 
 
 f 
 
 A 
 
 B 
 
 C * 
 
 ' A 
 
 B 
 
 c N 
 
 r " 
 A 
 
 B 
 
 C 
 
 14 
 
 
 
 0.1 
 
 0.1 
 
 
 0.7 
 
 4.1 
 
 
 0.1 
 
 1.1 
 
 
 0.1 
 
 15 
 
 2.7 
 
 0.4 
 
 0.1 
 
 3.4 
 
 0.2 
 
 
 0.2 
 
 
 
 4.5 
 
 4.8 
 
 0.2 
 
 16 
 
 1.6 
 
 0.4 
 
 0.1 
 
 2.5 
 
 0.1 
 
 
 0.2 
 
 
 
 
 4.5 
 
 4.8 
 
 0.2 
 
 19 
 
 2.2 
 
 0.3 
 
 0.7 
 
 2.3 
 
 0.2 
 
 0.2 
 
 0.1 
 
 
 
 8.1 
 
 0.3 
 
 0.3 
 
 20 
 
 1.3 
 
 0.4 
 
 
 1.2 
 
 0.1 
 
 
 14.1 
 
 9.2 
 
 
 5.9 
 
 1.9 
 
 0.1 
 
 22 
 
 1.4 
 
 0.8 
 
 3.6 
 
 6.4 
 
 0.3 
 
 8.2 
 
 1.4 
 
 0.02 
 
 0.3 
 
 13.1 
 
 2.4 
 
 3.6 
 
 23 
 
 2.0 
 
 2.6 
 
 1.8 
 
 7.8 
 
 12.5 
 
 20.6 
 
 17.9 
 
 0.3 
 
 0.01 
 
 15.5 
 
 3.6 
 
 2.1 
 
 24 
 
 1.6 
 
 0.1 
 
 1.1 
 
 4.4 
 
 0.5 
 
 0.5 
 
 11.9 
 
 0.3 
 
 0.4 
 
 14.9 
 
 7.5 
 
 1.0 
 
 25 
 
 1.2 
 
 1.0 
 
 0.5 
 
 1.5 
 
 0.4 
 
 0.2 
 
 0.7 
 
 
 
 9.6 
 
 0.06 
 
 
 Average 
 
 1.55 
 
 0.66 
 
 0.88 
 
 3.29 
 
 1.59 
 
 3.38 
 
 5.62 
 
 1.09 
 
 0.09 
 
 13.72 
 
 2.55 
 
 0.82 
 
432 University of California Publications in Agricultural Sciences [Vol.3 
 
 Greenhouse Data 
 
 There are objections to all greenhouse work due to somewhat un- 
 natural conditions for the usual indicator crops, the lack of a normal 
 water supply, the small amount of root space, etc. Crowding of the 
 pots is also apt to cause variations. Even the slight change in the loca- 
 tion of a pot on the bench will affect the growth of plants, as some of 
 the elaborate precautions for moving the pots daily, and in a given 
 order, testify. The outstanding advantage of greenhouse work is that 
 with a given indicator crop a group of soils, or soil conditions, may be 
 compared under very similar conditions. 
 
 In the present case, the leaks in the sash allowed rain water to fall 
 into some of the pots to a considerable extent. The pots so affected 
 showed a poorer growth in the cases of the heavy Altamont and 
 Diablo samples, where the soil was readily compacted, while in the 
 poor Hanford and San Joaquin soils the pots receiving leakage water 
 showed markedly better growth. 
 
 To minimize such errors, as much as possible, triplicates were 
 used, as above explained, besides repeating the series. In working 
 out the final averages of the crop it was suggested that a selection be 
 made of the crop dry weights, in case that there was a marked varia- 
 tion between the triplicates, using the two weights close together, and 
 excluding the third if it were widely divergent. However, when one 
 begins to select certain figures from a series, and bases comparisons 
 upon these alone, there is apt to be the tendency to select those figures 
 that will prove the point in question, unless there is some known dis- 
 turbing factor causing the divergence and which warrants the exclu- 
 sion of certain figures. 
 
 Other cases that are rather hard to deal with are those in which 
 the number of plants reaching maturity was not up to the standard to 
 which the series was thinned when the plants were young. This fail- 
 ure may have been due to poor germination, or to accidental destruc- 
 tion of the plants during growth. Sometimes less than the standard 
 number of plants will give a much greater dry weight per plant than 
 the normal number. It was not deemed advisable to use the weight 
 per plant, but rather to use the total dry weight of the crop, and only 
 consider of value the series in which the number of plants per pot 
 was practically constant. 
 
 In the greenhouse work the Diablo clay adobe, the Altamont clay 
 loam, and the Hanford fine sandy loam samples were compared by 
 
1919] 
 
 Pendleton: A Study of Soil Types 
 
 433 
 
 two croppings, while one crop was grown on the San Joaquin sandy 
 loam soils. The infertility of the San Joaquin soils, in some cases 
 extreme, greatly retarded crop growth. 
 
 Diablo clay adobe. First crop. — Due to the presence of wild oat 
 seed in all the four samples of this soil, and the inability to distin- 
 guish the young wild oat plants from the planted oats, wheat, or 
 barley when thinning, the value of the results of the grain crops in 
 this series is much decreased. The averages plotted include the total 
 
 Z5 
 
 20 
 
 *\5 
 
 a 
 
 u 
 
 10 
 
 Oats 
 and 
 
 Bur Clover 
 Bur Clover 
 
 as col us 
 
 Soils 
 
 Fig. 27. Graph showing the total dry matter produced by wheat, barley, 
 oats, Phaseolus, bur clover, and oats and bur clover on the four samples of 
 Diablo clay adobe. First crop. 
 
 crop, whether pure or with a greater or less quantity of the wild oats, 
 though the number of plants harvested was usually six or less. 
 Planting the oats and bur clover together was not a success. In three 
 of the soils the crop of bur clover alone was greater than that of the 
 six bur clover plants plus the six oat plants. Plate 44 shows how, in 
 some cases, the oats dominated, and in others the bur clover was 
 superior. On the soils of this type bur clover was the most satisfactory 
 crop, while the white beans were the most unsatisfactory of all. 
 
 Comparing the total crops (see fig. 27 and tables 45-50), it will 
 be seen that 1, 5, 2, 6 is the order for bur clover, soil no. 1 giving the 
 
4 
 
 434 
 
 University of California Publications in Agricultural Sciences [Vol. 3 
 
 best crop and soil no. 6 the poorest, while nos. 5, 1, 2, 6 is the order 
 for barley and wheat. Oats show nearly double the crop on soil 5 
 that it does on any of the other three soils. There is thus a general 
 agreement between the indicators that the soils are not of the same 
 productivity. 
 
 Table 45 — Diablo Clay Adobe, First Crop 
 Wheat 
 Planted, November 6, 1915. Harvested, July 10, 1916 
 
 Straw Grain Total dry matter 
 
 , A . A „ , A . 
 
 r \ f \ r \ 
 
 No. Average Average Average 
 
 Pot plants Weight weight Weight weight Weight weight 
 
 1-1 Wheat 2 3.65 0.25 
 
 Oats 4 2.15 0.69 6.74 
 
 1-2 Wheat 
 
 Oats 6 4.05 2.47 6.51 
 
 1-3 Wheat 1 1.83 
 
 Oats 5 5.20 5.62 1.64 1.68 8.66 7.30 
 
 2-1 Wheat 5 5.33 0.05 
 
 Oats 1 0.43 i 5.81 
 
 2-2 Wheat 4 3.53 0.03 
 
 Oats 2 0.69 0.04 4.31 
 
 2-3 Wheat 3 2.55 
 
 Oats 3 1.39 4.63 0.49 0.21 4.43 0.84 
 
 Notes 
 
 5-1 
 
 Wheat 2 
 
 4.33 
 
 
 Oats 4 
 
 1.56 
 
 5-2 
 
 Wheat 3 
 
 7.28 
 
 
 Oats 2 
 
 3.23 
 
 5-3 
 
 Wheat 3 
 
 7.09 
 
 
 Oats 2 
 
 0.64 
 
 6-1 
 
 Wheat 2 
 
 2.19 
 
 
 Oats 4 
 
 1.03 
 
 6-2 
 
 Wheat 
 
 
 
 Oats 5 
 
 1.72 
 
 6-3 
 
 Wheat 2 
 
 2.31 
 
 
 Oats 4 
 
 2.51 
 
 8.04 
 
 0.90 
 0.42 
 1.81 
 1.02 
 0.48 
 0.47 
 
 7.21 
 
 13.44 
 
 1.70 8.68 9.74 
 
 3.22 
 
 1.72 
 
 3.25 0.70 0.17 5.53 3.49 
 
1919] 
 
 Pendleton: A Study of Soil Types 
 
 435 
 
 Table 46 — Diablo Clay Adobe, First Crop 
 Barley 
 Planted, November 6, 1915. Harvested, April 28, 1916 
 Straw Grain Total dry matter 
 
 Pot 
 
 No. 
 plants 
 
 r 
 Weight 
 
 Average 
 
 weight 
 
 r 
 Weight 
 
 Average 
 weight 
 
 r 
 Weight 
 
 Average 
 weight 
 
 1-1 
 
 6 
 
 5.19 
 
 
 1.06 
 
 
 6.25 
 
 
 1-2 
 
 Barley 5 
 Oats 1 
 
 4.79 
 
 
 0.75 
 
 
 5.54 
 
 
 1-3 
 
 Barley 4 
 
 5.75 
 
 
 1.34 
 
 
 
 
 
 Oats 2 
 
 
 5.24 
 
 0.98 
 
 1.38 
 
 8.07 
 
 6.62 
 
 2-1 
 
 6 
 
 5.12 
 
 
 1.05 
 
 
 6.17 
 
 
 2-2 
 
 6 
 
 4.87 
 
 
 1.71 
 
 
 6.58 
 
 
 2-3 
 
 Barley 5 
 
 2.78 
 
 
 0.49 
 
 
 
 
 
 Oats 1 
 
 0.69 
 
 4.49 
 
 0.23 
 
 1.16 
 
 4.19 
 
 5.65 
 
 5-1 
 
 6 
 
 6.59 
 
 
 2.12 
 
 
 8.70 
 
 
 5-2 
 
 Barley 5 
 
 
 
 3.01 
 
 
 
 
 
 Oats 1 
 
 2.56 
 
 
 0.25 
 
 
 3.25 
 
 
 5-3 
 
 Barley 5 
 
 
 
 3.01 
 
 
 
 
 
 Oats 1 
 
 8.43 
 
 5.86 
 
 0.04 
 
 1.95 
 
 11.48 
 
 7.81 
 
 6-1 
 
 6 
 
 4.62 
 
 
 1.26 
 
 
 5.88 
 
 
 6-2 
 
 6 
 
 4.36 
 
 
 1.25 
 
 
 5.61 
 
 
 6-3 
 
 Barley 5 
 
 
 
 0.33 
 
 
 
 
 
 Oats 1 
 
 3.49 
 
 4.16 
 
 0.24 
 
 1.02 
 
 4.06 
 
 5.18 
 
 Notes 
 
 Table 47 — Diablo Clay Adobe, First Crop 
 
 Oats 
 
 Planted, November 6, 1915. Harvested, May 8, 1916 
 
 Straw Grain Total dry matter 
 
 Pot 
 
 No. 
 plants 
 
 r 
 Weight 
 
 Average 
 weight 
 
 r 
 Weight 
 
 Average 
 weight 
 
 r 
 Weight 
 
 Average 
 weight 
 
 1-1 
 
 6 
 
 4.11 
 
 
 1.24 
 
 
 5.35 
 
 
 1-2 
 
 6 
 
 6.56 
 
 
 2.59 
 
 
 9.15 
 
 
 1-3 
 
 6 
 
 4.76 
 
 5.14 
 
 1.34 
 
 1.72 
 
 6.10 
 
 6.86 
 
 2-1 
 
 6 
 
 4.36 
 
 
 1.10 
 
 
 5.46 
 
 
 2-2 
 
 6 
 
 total 
 
 only 
 
 total i 
 
 only 
 
 6.92 
 
 
 2-3 
 
 6 
 
 6.66 
 
 5.51 
 
 2.06 
 
 1.58 
 
 8.72 
 
 7.03 
 
 5-1 
 
 7 
 
 7.55 
 
 
 2.59 
 
 
 10.15 
 
 
 5-2 
 
 6 
 
 10.66 
 
 
 4.38 
 
 
 15.04 
 
 
 5-3 
 
 6 
 
 10.10 
 
 
 3.12 
 
 
 13.22 
 
 
 6-1 
 
 6 
 
 4.70 
 
 
 1.48 
 
 
 6.18 
 
 
 6-2 
 
 6 
 
 6.81 
 
 
 1.42 
 
 
 8.22 
 
 
 6-3 
 
 6 
 
 6.78 
 
 
 1.09 
 
 
 7.88 
 
 
 Notes 
 
 One barley plant 
 
436 University of California Publications in Agricultural Sciences [Vol. 3 
 
 Table 48 — Diablo Clay Adobe, First Crop 
 
 Bur Clover 
 
 Planted, November 6, 1915. Harvested, May 8, 1916 
 
 
 No. 
 plants 
 
 St 
 
 raw 
 
 Gi 
 
 rain 
 
 Total dr 
 
 r 
 
 Weight 
 
 y matter 
 
 Pot 
 
 f 
 Weight 
 
 Average 
 weight 
 
 r 
 Weight 
 
 Average 
 weight 
 
 Average 
 weight 
 
 1-1 
 
 5 
 
 11.01 
 
 
 15.13 
 
 
 26.32 
 
 
 1-2 
 
 4 
 
 9.07 
 
 
 14.15 
 
 
 23.22 
 
 
 1-3 
 
 6 
 
 12.18 
 
 10.75 
 
 13.02 
 
 14.16 
 
 25.20 
 
 24.91 
 
 2-1 
 
 6 
 
 8.26 
 
 
 9.89 
 
 
 18.16 
 
 
 2-2 
 
 5 
 
 7.45 
 
 
 8.93 
 
 
 16.39 
 
 
 2-3 
 
 6 
 
 7.97 
 
 7.89 
 
 8.02 
 
 8.98 
 
 15.99 
 
 16.84 
 
 5-1 
 
 7 
 
 11.14 
 
 
 12.33 
 
 
 23.48 
 
 
 5-2 
 
 8 
 
 10.67 
 
 
 13.05 
 
 
 23.72 
 
 
 5-3 
 
 7 
 
 10.55 
 
 10.79 
 
 9.76 
 
 11.71 
 
 20.31 
 
 22.50 
 
 6-1 
 
 6 
 
 7.96 
 
 
 8.73 
 
 
 16.69 
 
 
 6-2 
 
 6 
 
 8.26 
 
 
 9.76 
 
 
 18.02 
 
 
 6-3 
 
 6 
 
 6.87 
 
 7.69 
 
 6.04 
 
 8.18 
 
 12.91 
 
 15.87 
 
 
 
 Table 49— 
 
 Diablo Clay Adobe, First Crop 
 
 Notes 
 
 Oats and Bur Clover 
 Planted, November 6, 1915. Harvested, May 8, 1916 
 
 
 No. 
 plants 
 
 St 
 
 raw 
 
 Grain 
 
 Total di 
 Weight 
 
 •y matter 
 
 Pot 
 
 r 
 
 Weight 
 
 Average 
 weight 
 
 r 
 Weight 
 
 Average 
 weight 
 
 Average 
 weight 
 
 1-1 
 
 Clover 3 
 
 10.37 
 
 
 11.93 
 
 
 22.30 
 
 
 
 Oats 6 
 
 2.38 
 
 
 0.14 
 
 
 2.52 
 
 
 1-2 
 
 Clover 6 
 
 8.19 
 
 
 9.28 
 
 
 17.47 
 
 
 
 Oats 6 
 
 3.48 
 
 
 0.70 
 
 
 4.16 
 
 
 1-3 
 
 Clover 6 
 
 13.53 
 
 
 9.81 
 
 
 23.34 
 
 
 
 Oats 6 
 
 2.65 
 
 13.53 
 
 0.27 
 
 10.71 
 
 2.92 
 
 24.24 
 
 2-1 
 
 Clover 6 
 
 2.13 
 
 
 2.57 
 
 
 4.70 
 
 
 
 Oats 6 
 
 5.77 
 
 
 1.81 
 
 
 7.58 
 
 
 2-2 
 
 Clover 6 
 
 4.24 
 
 
 4.62 
 
 
 8.87 
 
 
 
 Oats 6 
 
 4.56 
 
 
 1.26 
 
 
 5.82 
 
 
 2-3 
 
 Clover 6 
 
 3.43 
 
 
 4.51 
 
 
 7.94 
 
 
 
 Oats 6 
 
 3.20 
 
 7.75 
 
 0.46 
 
 5.08 
 
 3.66 
 
 12.85 
 
 5-1 
 
 Clover 6 
 
 10.88 
 
 
 9.78 
 
 
 20.66 
 
 
 
 Oats 6 
 
 2.45 
 
 
 0.27 
 
 
 2.71 
 
 
 5-2 
 
 Clover 5 
 
 10.52 
 
 
 9.32 
 
 
 19.84 
 
 
 
 Oats 6 
 
 2.19 
 
 
 0.51 
 
 
 2.79 
 
 
 5-3 
 
 Clover 5 
 
 8.31 
 
 
 8.36 
 
 
 16.66 
 
 
 
 Oats 6 
 
 3.45 
 
 12.60 
 
 0.66 
 
 9.63 
 
 4.10 
 
 22.26 
 
 6-1 
 
 Clover 6 
 
 8.90 
 
 
 9.56 
 
 
 18.46 
 
 
 
 Oats 6 
 
 3.10 
 
 
 0.35 
 
 
 3.45 
 
 
 6-2 
 
 Clover 6 
 
 9.01 
 
 
 5.82 
 
 
 14.83 
 
 
 
 Oats 6 
 
 2.09 
 
 
 0.52 
 
 
 2.61 
 
 
 6-3 
 
 Clover 6 
 
 6.51 
 
 
 10.45 
 
 
 16.97 
 
 
 
 Oats 5 
 
 2.33 
 
 10.65 
 
 0.47 
 
 9.06 
 
 2.80 
 
 19.71 
 
 Notes 
 
1919] Pendleton: A Study of Soil Types 437 
 
 Table 50 — Diablo Clay Adobe, First Crop 
 
 Phaseolus vulgaris 
 
 Planted, April 4, 1916. Harvested, October 7, 1916 
 
 Straw Grain Total dry matter 
 
 Notes 
 Growth poor and 
 slow through- 
 
 Pot 
 
 No. 
 plants 
 
 Weight 
 
 Average 
 weight 
 
 r 
 
 Weight 
 
 Average 
 weight 
 
 Weight 
 
 Average 
 weight 
 
 1-1 
 
 8 
 
 2.05 
 
 
 0.58 
 
 
 2.63 
 
 i 
 
 1-2 
 
 1 
 
 0.94 
 
 
 0.87 
 
 
 1.81 
 
 
 1-3 
 
 12 
 
 2.86 
 
 1.95 
 
 1.37 
 
 0.94 
 
 4.23 
 
 2.89 
 
 2-1 
 
 3 
 
 0.53 
 
 
 0.21 
 
 
 0.74 
 
 
 2-2 
 
 10 
 
 0.83 
 
 
 
 
 0.83 
 
 
 2-3 
 
 17 
 
 1.26 
 
 0.87 
 
 0.11 
 
 0.10 
 
 1.37 
 
 0.98 
 
 5-1 
 
 3 
 
 0.53 
 
 
 0.40 
 
 
 0.93 
 
 
 5-2 
 
 2 
 
 0.46 
 
 
 0.41 
 
 
 0.87 
 
 
 5-3 
 
 
 
 0.33 
 
 
 0.27 
 
 
 0.60 
 
 6-1 
 
 2 
 
 0.22 
 
 
 
 
 0.22 
 
 
 6-2 
 
 
 
 
 
 
 
 
 6-3 
 
 1 
 
 0.23 
 
 0.15 
 
 
 
 0.23 
 
 0.15 
 
 Diablo clay adobe. Second crop. — The. crops used in this plant- 
 ing were milo (two series, one following oats and bur clover, and the 
 other following oats alone), cowpeas, millet, and soy beans. The 
 crop was thinned as follows : milo to eight plants, millet to twelve, 
 soy beans to six, and cowpeas to six. The total dry weight (tables 
 51-55) of the largest leguminous crop in this planting is about one- 
 third of that of the bur clover in the first planting ; though the grains 
 are proportionately not nearly so much less than in the first crop. 
 Soil no. 2 has the least pronounced adobe structure, but was the most 
 easily puddled. The plants in one of the pots of soy beans of soil 
 no. 2 were entirely killed by too much water. 
 
 Comparing the relative growth on the soils, the notes made while 
 the crops were growing coincide very closely with the dry weights. 
 As to the relative crop production (fig. 28), it can be said that soils 
 nos. 1 and 5 produced larger crops than soils nos. 2 and 6. Thus the 
 second crop results substantiate those of the first crop. 
 
438 
 
 University of California Publications in Agricultural Sciences [Vol. 3 
 
 So.y Beans 
 
 j-Milo B 
 
 •~*"f' ! ~.? M <r'Cow Peas 
 
 Millet 
 5 6 
 
 Soils 
 
 Pig. 28. Graph showing the total dry matter produced by milo (two 
 series), millet, soy beans, and cowpeas on the four samples of Diablo clay 
 adobe. Second crop. 
 
 Wheat 
 Oats + Bur CI over 
 Barley 
 Oats 
 
 Bur Clover 
 Phaseolas 
 
 Fig. 29. Graph showing the' total dry matter produced by wheat, barley, 
 oats, bur clover, Phaseolus, and oats and bur clover on the three samples of 
 Altamont clay loam. First crop. 
 
 Soy Beans B 
 5qy Beans A 
 Cow Peas A 
 Cow Peas B 
 
 Milo A 
 M.loB 
 
 Fig. 30. Graph showing the total dry matter produced by milo (two series), 
 cowpeas (two series), and soy beans (two series) on the three samples of 
 Altamont clay loam. Second crop. 
 
1919] 
 
 Pendleton: A Study of Soil Types 
 
 439 
 
 Pot 
 
 No. 
 plants 
 
 1-1 
 
 8 
 
 1-2 
 
 8 
 
 1-3 
 
 7 
 
 2-1 
 
 8 
 
 2-2 
 
 8 
 
 2-3 
 
 8 
 
 5-1 
 
 8 
 
 5-2 
 
 6 
 
 5-3 
 
 7 
 
 6-1 
 
 9 
 
 6-2 
 
 8 
 
 6-3 
 
 8 
 
 Table 51 — Diablo Clay Adobe, Second Crop 
 
 Milo A (following oats) 
 
 Planted, June 3, 1916. Harvested, November 16, 1916 
 
 Straw Grain Total dry matter 
 
 A . A . . A . 
 
 r \ r \ r \ 
 
 Average Average Average 
 
 Weight weight Weight weight Weight weight Notes 
 
 4.87 4.87 Excluded from 
 
 10.00 10.00 average 
 
 4.50 4.68 4.50 4.68 
 
 2.59 2.59 
 
 3.73 3.73 
 
 2.92 3.08 2.92 3.08 
 
 4.03 4.03 
 
 5.13 5.13 
 
 8.44 8.44 
 
 3.49 3.49 
 
 3.08 3.08 
 
 2.98 3.18 2.98 3.18 
 
 Pot 
 
 No. 
 
 plants 
 
 1-1 
 
 8 
 
 1-2 
 
 8 
 
 1-3 
 
 8 
 
 2-1 
 
 8 
 
 2-2 
 
 8 
 
 2-3 
 
 8 
 
 5-1 
 
 8 
 
 5-2 
 
 8 
 
 5-3 
 
 8 
 
 6-1 
 
 8 
 
 6-2 
 
 8 
 
 6-3 
 
 8 
 
 Table 52 — Diablo Clay Adobe, Second Crop 
 
 Milo B (following oats and bur clover) 
 
 Planted, June 3, 1916. Harvested, November 16, 1916 
 
 Straw Grain Total dry matter 
 
 . A „ . A „ , A „ 
 
 r \ ( \ r \ 
 
 Average Average Average 
 
 Weight weight Weight weight Weight weight 
 
 6.41 . 6.41 
 
 8.78 8.78 
 
 6.21 7.14 6.21 7.14 
 
 3.92 3.92 
 
 4.52 4.52 
 
 3.63 4.02 3.63 4.02 
 
 10.34 10.34 
 
 6.17 6.17 
 
 5.20 7.24 5.20 7.24 
 
 9.29 9.29 
 
 3.70 3.70 
 
 4.09 5.69 4.09 5.69 
 
 Notes 
 
440 University of California Publications in Agricultural Sciences [Vol. 3 
 
 Table 53 — Diablo Clay Adobe, Second Crop 
 
 Millet (following bur clover) 
 
 Planted, June 3, 1916. Harvested, October 6, 1917 
 
 Notes 
 
 
 No. 
 plants 
 
 Straw 
 
 Gi 
 
 rain 
 
 Total dry 
 
 r 
 
 Weight 
 
 matter 
 
 Pot 
 
 r ' 
 Weight 
 
 Average 
 weight 
 
 r 
 Weight 
 
 Average 
 weight 
 
 Average 
 weight 
 
 1-1 
 
 12 
 
 1.52 
 
 
 1.44 
 
 
 2.96 
 
 
 1-2 
 
 11 
 
 1.34 
 
 
 0.90 
 
 
 2.24 
 
 
 1-3 
 
 11 
 
 2.03 
 
 1.63 
 
 1.15 
 
 1.16 
 
 3.18 
 
 2.79 
 
 2-1 
 
 12 
 
 1.26 
 
 
 1.29 
 
 
 2.55 
 
 
 2-2 
 
 11 
 
 1.49 
 
 
 1.32 
 
 
 2.80 
 
 
 2-3 
 
 12 
 
 0.93 
 
 1.23 
 
 0.88 
 
 1.16 
 
 1.80 
 
 2.39 
 
 5-1 
 
 10 
 
 2.26 
 
 
 2.19 
 
 
 4.45 
 
 
 5-2 
 
 12 
 
 3.35 
 
 
 3.36 
 
 
 6.71 
 
 
 5-3 
 
 12 
 
 2.02 
 
 2.54 
 
 1.51 
 
 2.35 
 
 3.53 
 
 4.90 
 
 6-1 
 
 11 
 
 1.19 
 
 
 0.99 
 
 
 2.18 
 
 
 6-2 
 
 12 
 
 1.59 
 
 
 1.23 
 
 
 2.82 
 
 
 6-3 
 
 13 
 
 1.26 
 
 1.35 
 
 1.04 
 
 1.09 
 
 2.29 
 
 2.43 
 
 Table 54 — Diablo Clay Adobe, Second Crop 
 
 Cowpeas (following wheat) 
 
 Planted, August 10, 1916. Harvested, November 16, 1916 
 
 Straw Grain Total dry matter 
 
 , A . . A „ A 
 
 f \ i ^ r \ 
 
 No. Average Average Average 
 
 Pot plants Weight weight Weight weight Weight weight Notes 
 
 1-1 7 2.66 2.66 
 
 1-2 7 5.30 5.30 
 
 1-3 7 3.73 3.89 3.73 3.89 
 
 2-1 6 2.57 2.57 
 
 2-2 6 4.24 4.24 
 
 2-3 6 2.86 3.22 2.86 3.22 
 
 5-1 6 2.74 2.74 
 
 5-2 6 4.30 4.30 
 
 5-3 6 3.64 3.56 3.64 3.56 
 
 6-1 6 3.28 3.28 
 
 6-2 7 4.10 4.10 
 
 6-3 6 3.41 3.60 3.41 3.60 
 
1919] 
 
 Pendleton : A Study of Soil Types 
 
 441 
 
 Table 55 — Diablo Clay Adobe, Second Crop 
 
 Soy Beans (following barley) 
 
 Planted, June 6, 1916. Harvested, November 14, 1916 
 
 
 No. 
 plants 
 
 Straw 
 
 A 
 
 Gi 
 
 rain 
 
 A 
 
 Total dry matter 
 
 A 
 
 f \ 
 
 Average 
 
 Weight weight 
 
 
 Pot 
 
 r 
 
 Weight 
 
 > 
 Average 
 weight 
 
 r 
 Weight 
 
 Average 
 weight 
 
 Notes 
 
 1-1 
 
 6 
 
 8.48 
 
 
 0.29 
 
 
 8.77 
 
 
 
 1-2 
 
 6 
 
 8.58 
 
 
 0.06 
 
 
 8.64 
 
 
 
 1-3 
 
 6 
 
 6.87 
 
 7.98 
 
 0.41 
 
 0.25 
 
 7.28 
 
 8.23 
 
 
 2-1 
 
 6 
 
 2.12 
 
 
 
 
 2.12 
 
 
 Excluded from 
 
 2-2 
 
 4 
 
 3.62 
 
 
 0.40 
 
 
 4.02 
 
 
 average 
 
 2-3 
 
 5 
 
 6.07 
 
 4.84 
 
 0.38 
 
 0.39 
 
 6.45 
 
 5.23 
 
 
 5-1 
 
 6 
 
 5.84 
 
 
 0.16 
 
 
 6.00 
 
 
 
 5-2 
 
 6 
 
 7.96 
 
 
 0.64 
 
 
 8.60 
 
 
 
 5-3 
 
 6 
 
 6.47 
 
 6.76 
 
 0.69 
 
 0.49 
 
 7.16 
 
 7.25 
 
 
 6-1 
 
 6 
 
 7.61 
 
 
 0.24 
 
 
 7.85 
 
 
 
 6-2 
 
 6 
 
 7.99 
 
 
 0.45 
 
 
 8.43 
 
 
 
 6-3 
 
 6 
 
 7.26 
 
 7.62 
 
 0.17 
 
 0.28 
 
 7.43 
 
 7.90 
 
 
 Altamont clay loam. First crop. — The crops planted in this soil 
 were wheat, barley, oats, bur clover, Phaseolus, and oats and bur 
 clover together. The standard number to which the plants were 
 thinned was six, except in the oats and bur clover series, where three 
 plants of each were allowed to remain. 
 
 With regard to the comparative crop producing power of these 
 soils under these conditions, soil no. 4 is the best, with soil no. 3 as 
 the second, and soil no. 7 was the poorest (tables 56-60, fig. 29). The 
 dry weight data decidedly corroborate the impression given by the 
 greenhouse appearance of the crops. However, as all the crops were 
 so small on all the series, the figures do not show as much as they 
 might have shown had the growth been more nearly optimum for the 
 several crops. 
 
 Table 56 — Altamont Clay Loam, First Crop 
 
 Wheat 
 
 Planted, February 25, 1916. Harvested, July 10, 1916 
 
 Notes 
 
 
 No. 
 plants 
 
 Straw 
 
 A 
 
 Grain 
 
 A 
 
 Total dr 
 Weight 
 
 y matter 
 
 A 
 
 Pot 
 
 Weight 
 
 Average 
 weight 
 
 Weight 
 
 Average 
 weight 
 
 Average 
 weight 
 
 3-1 
 
 6 
 
 2.62 
 
 
 1.23 
 
 
 3.85 
 
 
 3-2 
 
 6 
 
 2.93 
 
 
 1.09 
 
 
 3.92 
 
 
 3-3 
 
 6 
 
 2.86 
 
 2.80 
 
 1.04 
 
 1.12 
 
 3.91 
 
 3.92 
 
 4-1 
 
 6 
 
 4.20 
 
 
 1.78 
 
 
 5.97 
 
 
 4-2 
 
 6 
 
 4.03 
 
 
 1.22 
 
 
 5.25 
 
 
 4-3 
 
 6 
 
 6.20 
 
 4.81 
 
 1.13 
 
 1.38 
 
 7.34 
 
 6.19 
 
 7-1 
 
 6 
 
 2.64 
 
 
 1.11 
 
 
 3.76 
 
 
 7-2 
 
 6 
 
 2.58 
 
 
 0.99 
 
 
 3.64 
 
 
 7-3 
 
 6 
 
 2.90 
 
 2.71 
 
 0.71 
 
 0.93 
 
 3.61 
 
 3.64 
 
442 
 
 University of California Publications in Agricultural Sciences [Vol. 3 
 
 Table 57 — Altamont Clay Loam, First Crop 
 
 Barley 
 
 Planted, April 4, 1916. Harvested, July 11, 1916 
 
 
 No. 
 plants 
 
 St 
 
 raw 
 
 Grain 
 
 Total dr 
 
 r 
 
 Weight 
 
 y matter 
 
 Pot 
 
 f 
 Weight 
 
 Average 
 weight 
 
 Weight 
 
 Average 
 weight 
 
 Average 
 weight 
 
 3-1 
 
 
 1.10 
 
 
 0.76 
 
 
 1.86 
 
 
 3-2 
 
 
 1.45 
 
 
 1.40 
 
 
 2.85 
 
 
 3-3 
 
 
 1.39 
 
 1.31 
 
 1.18 
 
 1.11 
 
 2.57 
 
 2.43 
 
 4-1 
 
 
 1.99 
 
 
 1.43 
 
 
 3.42 
 
 
 4-2 
 
 
 1.90 
 
 
 1.57 
 
 
 3.47 
 
 
 4-3 
 
 
 2.39 
 
 2.09 
 
 1.85 
 
 1.62 
 
 4.25 
 
 3.71 
 
 7-1 
 
 
 0.98 
 
 
 0.90 
 
 
 1.88 
 
 
 7-3 
 
 
 1.06 
 
 1.00 
 
 0.59 
 
 0.71 
 
 1.64 
 
 1.71 
 
 Notes 
 
 Table 58 — Altamont Clay Loam, First Crop 
 
 Oats 
 
 Planted, February 25, 1916. Harvested July 11, 1916 
 
 
 No. 
 
 plants 
 
 6 
 
 SI 
 
 raw 
 
 A 
 
 Grain 
 
 Total dry matter 
 
 Pot 
 3-1 
 
 r 
 Weight 
 
 1.36 
 
 Average 
 weight 
 
 r 
 
 Weight 
 0.38 
 
 Average 
 weight 
 
 Weight 
 1.74 
 
 Average 
 weight 
 
 3-2 
 
 6 
 
 1.60 
 
 
 0.67 
 
 
 2.27 
 
 
 3-3 
 
 6 
 
 1.70 
 
 1.55 
 
 0.47 
 
 0.51 
 
 2.17 
 
 2.06 
 
 4-1 
 
 6 
 
 3.05 
 
 
 1.42 
 
 
 4.47 
 
 
 4-2 
 
 4 
 
 2.62 
 
 
 1.13 
 
 
 3.76 
 
 
 4-3 
 
 4 
 
 3.46 
 
 3.04 
 
 1.81 
 
 1.45 
 
 5.27 
 
 4.50 
 
 7-1 
 
 6 
 
 1.21 
 
 
 0.29 
 
 
 1.51 
 
 
 7-2 
 
 6 
 
 1.00 
 
 
 0.42 
 
 
 1.42 
 
 
 7-3 
 
 6 
 
 0.88 
 
 1.03 
 
 0.35 
 
 0.35 
 
 1.23 
 
 1.38 
 
 Notes 
 
 Table 58 — Altamont Clay Loam, First Crop 
 
 Bur Clover 
 
 Planted, February 25, 1916. Harvested, July 8, 1916 
 
 
 No. 
 plants 
 
 6 
 
 Straw 
 
 A 
 
 Gi 
 
 *ain 
 
 Total dr 
 
 r 
 
 Weight 
 2.53 
 
 y matter 
 
 Pot 
 3-1 
 
 r 
 
 Weight 
 1.50 
 
 Average 
 weight 
 
 Weight 
 1.03 
 
 Average 
 weight 
 
 Average 
 weight 
 
 3-2 
 
 6 
 
 0.88 
 
 
 1.17 
 
 
 2.18 
 
 
 3-3 
 
 6 
 
 0.63 
 
 1.00 
 
 1.34 
 
 1.18 
 
 1.96 
 
 2.18 
 
 4-1 
 
 6 
 
 2.48 
 
 
 1.47 
 
 
 3.95 
 
 
 4-2 
 
 6 
 
 2.57 
 
 
 1.57 
 
 
 4.14 
 
 
 4-3 
 
 4 
 
 2.50 
 
 2.52 
 
 1.31 
 
 1.45 
 
 3.81 
 
 3.97 
 
 7-1 
 
 6 
 
 0.47 
 
 
 0.66 
 
 
 1.13 
 
 
 7-2 
 
 6 
 
 0.53 
 
 
 0.24 
 
 
 0.78 
 
 
 7-3 
 
 6 
 
 0.37 
 
 0.46 
 
 0.20 
 
 0.36 
 
 0.57 
 
 0.82 
 
 Notes 
 
1919] 
 
 Pendleton: A Study of Soil Types 
 
 443 
 
 Table 59 — Altamont Clay Loam, First Crop 
 Oats and Bur Clover 
 
 
 
 
 Planted, 
 
 April 14, 
 
 1916. 
 
 Harvested, July 8, 191 
 
 
 No. 
 plants 
 
 
 Straw 
 
 A 
 
 Grain 
 
 A 
 
 Total di 
 
 height 
 
 •y matter 
 
 K 
 
 Pot 
 
 r 
 
 Weight 
 
 "\ r 
 Average 
 weight Weight 
 
 > r 
 
 Average 
 
 weight V\ 
 
 Average 
 weight 
 
 3-1 
 
 B.C. 
 
 3 
 
 0.98 
 
 
 1.25 
 
 
 2.23 
 
 
 
 Oats 
 
 3 
 
 0.77 
 
 
 0.10 
 
 
 0.88 
 
 
 3-2 
 
 B.C. 
 
 4 
 
 0.79 
 
 
 1.17 
 
 
 1.96 
 
 
 
 Oats 
 
 4 
 
 0.68 
 
 
 0.22 
 
 
 0.90 
 
 
 3-3 
 
 B.C. 
 
 4 
 
 0.48 
 
 
 0.91 
 
 
 1.38 
 
 
 
 Oats 
 
 4 
 
 0.78 
 
 1.49 
 
 0.30 
 
 1.32 
 
 1.07 
 
 2.81 
 
 4-1 
 
 B.C. 
 
 3 
 
 0.67 
 
 
 0.32 
 
 
 0.99 
 
 
 
 Oats 
 
 3 
 
 2.42 
 
 
 1.75 
 
 
 4.17 
 
 
 4-2 
 
 B.C. 
 
 3 
 
 0.40 
 
 
 0.62 
 
 
 1.01 
 
 
 
 Oats 
 
 3 
 
 2.63 
 
 
 1.38 
 
 
 4.01 
 
 
 4-3 
 
 B.C. 
 
 3 
 
 0.51 
 
 
 0.21 
 
 
 0.72 
 
 
 
 Oats 
 
 3 
 
 2.77 
 
 3.14 
 
 1.09 
 
 1.78 
 
 3.86 
 
 4.92 
 
 7-1 
 
 B.C. 
 
 3 
 
 0.20 
 
 
 0.27 
 
 
 0.47 
 
 
 
 Oats 
 
 3 
 
 0.86 
 
 
 0.74 
 
 
 1.60 
 
 
 7-2 
 
 B.C. 
 
 3 
 
 0.28 
 
 
 0.22 
 
 
 0.50 
 
 
 
 Oats 
 
 3 
 
 1.27 
 
 
 0.95 
 
 
 2.22 
 
 
 7-3 
 
 B.C. 
 
 4 
 
 0.42 
 
 
 0.37 
 
 
 0.74 
 
 
 
 Oats 
 
 2 
 
 0.64 
 
 1.22 
 
 0.44 
 
 0.98 
 
 1.08 
 
 2.20 
 
 Notes 
 
 Table 60 — Altamont Clay Loam, First Crop 
 
 Beans (Phaseolus) 
 
 Planted, February 25, 1916. Harvested, July 11, 1916 
 
 
 No. 
 plants 
 
 Straw 
 
 A 
 
 Grain 
 
 Total dr; 
 Weight 
 
 y matter 
 
 Pot 
 
 Weight 
 
 Average 
 weight 
 
 r 
 
 Weight 
 
 Average 
 weight 
 
 Average 
 weight 
 
 3-1 
 
 6 
 
 2.82 
 
 
 0.13 
 
 
 2.96 
 
 
 3-2 
 
 6 
 
 1.24 
 
 
 0.35 
 
 
 1.59 
 
 
 3-3 
 
 6 
 
 1.32 
 
 1.79 
 
 0.32 
 
 0.27 
 
 1.64 
 
 2.06 
 
 4-1 
 
 5 
 
 1.71 
 
 
 0.25 
 
 
 1.96 
 
 
 4-2 
 
 6 
 
 1.41 
 
 
 0.59 
 
 
 2.01 
 
 
 4-2 
 
 6 
 
 1.81 
 
 1.64 
 
 0.59 
 
 0.48 
 
 2.41 
 
 2.12 
 
 7-1 
 
 1 
 
 0.11 
 
 
 0.09 
 
 
 0.20 
 
 
 7-2 
 
 6 
 
 0.53 
 
 
 
 
 0.53 
 
 
 7-3 
 
 5 
 
 0.63 
 
 0.43 
 
 
 0.03 
 
 0.63 
 
 0.46 
 
 Notes 
 
 Altamont clay loam. Second crop. — A slightly different scheme 
 was used in the planting of this series, only three crops were used, 
 i.e., soy beans, cowpeas, and milo. Two sets of pots were planted to 
 each crop, one of the two sets having previously been planted to a 
 legume, and the other to a non-legume. The milo was thinned so that 
 
444 University of California Publications in Agricultural Sciences [Vol. 3 
 
 one pot of each triplicate set would have 8 plants, the second of the 
 set 12 plants, and the last 16 plants. It was found that the wide 
 variation in the number of plants had but little effect upon the dry 
 weight produced per pot (tables 61-66). The effect was indeed so 
 slight that the totals were averaged up as usual. Figure 30 shows 
 distinctly that there was very little variation as regards total produc- 
 tion among these soils, so little as not to warrant any conclusions as 
 regards substantiation of, or disagreement with, the first crop. It 
 will be noticed in the second crop of the Diablo series, as well as in 
 that of the Altamont series, that the maintenance of the soils under 
 the same conditions for a year or more seems to bring them quite 
 rapidly to an average crop producing power. 
 
 Table 61 — Altamont Clay Loam, Second Crop 
 
 Milo A (following wheat) 
 
 Planted, August 10, 1916. Harvested, November 17, 1916 
 
 Straw Grain Total dry matter 
 
 No. Average Average Average 
 
 Pot plants Weight weight Weight weight Weight weight Notes 
 
 3-1 8 0.77 0.77 
 
 3-2 12 1.01 1.01 
 
 3-3 16 0.97 0.92 0.97 0.92 
 
 4-1 8 1.22 1.22 
 
 4-2 12 2.32 2.32 
 
 4-3 16 2.08 1.87 2.08 1.87 
 
 7-1 8 0.59 0.59 
 
 7-2 12 0.99 1.29 
 
 7-3 16 1.29 0.95 1.29 0.95 
 
 Table 62 — Altamont Clay Loam, Second Crop 
 
 Milo B 
 
 Planted, August 10, 1916. Harvested, November 15, 1916 
 
 Straw Grain Total dry matter 
 
 . A . . A . , A . 
 
 t ^ r ^> f \ 
 
 Average Average Average 
 
 Weight weight Weight weight Weight weight Notes 
 
 0.82 0.82 
 
 1.13 1.13 
 
 1.15 1.03 1.15 1.03 
 
 1.28 1.28 
 
 1.82 1.82 
 
 1.45 1.52 1.45 1.52 
 
 0.66 0.66 
 
 0.96 0.96 
 
 0.02 0.85 0.92 0.85 
 
 Pot 
 
 No. 
 plants 
 
 3-1 
 
 8 
 
 3-2 
 
 12 
 
 3-3 
 
 16 
 
 4-1 
 
 8 
 
 4-2 
 
 12 
 
 4-3 
 
 16 
 
 7-1 
 
 8 
 
 7-2 
 
 12 
 
 7-3 
 
 10 
 
1919] 
 
 Pendleton: A Study of Soil Types 
 
 445 
 
 Table 63 — Altamont Clay Loam, Second Crop 
 
 Cowpeas A (following barley) 
 
 Planted, August 10, 1916. Harvested, November 17, 1916 
 
 Straw 
 
 Pot 
 
 No. 
 
 plants 
 
 r 
 
 Weight 
 
 Average 
 weight 
 
 3-1 
 
 6 
 
 3.48 
 
 
 3-2 
 
 6 
 
 4.50 
 
 
 3-3 
 
 6 
 
 3.00 
 
 3.66 
 
 4-1 
 
 6 
 
 2.44 
 
 
 4-2 
 
 6 
 
 2.59 
 
 
 4-3 
 
 6 
 
 3.40 
 
 2.81 
 
 7-1 
 
 6 
 
 2.64 
 
 
 7-2 
 
 6 
 
 1.93 
 
 
 7-3 
 
 6 
 
 2.15 
 
 2.24 
 
 Grain 
 
 A 
 
 Average 
 Weight weight 
 
 Total dry matter 
 
 Weight 
 
 Average 
 weight 
 
 3.48 
 
 
 4.50 
 
 
 3.00 
 
 3.66 
 
 2.44 
 
 
 2.59 
 
 
 3.40 
 
 2.81 
 
 2.64 
 
 
 1.93 
 
 
 2.15 
 
 2.24 
 
 Notes 
 
 Table 64 — Altamont Clay Loam, Second Crop 
 
 Cowpeas B (following oats and bur clover) 
 
 Planted, August 10, 1916. Harvested, November 14, 1916 
 
 Straw Grain Total dry matter 
 
 Pot 
 
 No. 
 plants 
 
 Weight 
 
 Average 
 weight 
 
 Average 
 Weight weight 
 
 r 
 Weight 
 
 Average 
 weight 
 
 3-1 
 
 6 
 
 4.16 
 
 
 
 4.16 
 
 
 3-2 
 
 6 
 
 3.63 
 
 
 
 3.63 
 
 
 3-2 
 
 6 
 
 2.77 
 
 3.52 
 
 
 2.77 
 
 3.52 
 
 4-1 
 
 6 
 
 3.35 
 
 
 
 3.35 
 
 
 4-2 
 
 6 
 
 2.70 
 
 
 
 2.70 
 
 
 4-3 
 
 6 
 
 1.94 
 
 2.66 
 
 
 1.94 
 
 2.66 
 
 7-1 
 
 6 
 
 1.51 
 
 
 
 1.51 
 
 
 7-2 
 
 6 
 
 2.10 
 
 
 
 2.10 
 
 
 7-3 
 
 6 
 
 2.85 
 
 2.15 
 
 
 2.85 
 
 2.15 
 
 Notes 
 
 Table 65 — Altamont Clay Loam, Second Crop 
 
 Soy Beans A (following oats) 
 
 Planted, August 10, 1916. Harvested, November 17, 1916 
 
 Straw Grain Total drv matter 
 
 , A . A . A . 
 
 t "\ t \ t \ 
 
 No. Average Average Average 
 
 Pot plants Weight weight Weight weight Weight weight 
 
 3-1 6 4.85 4.85 
 
 3-2 6 4.25 4.25 
 
 3-3 6 4.50 4.53 4.50 4.53 
 
 4-1 6 3.53 3.53 
 
 4-2 6 3.59 3.59 
 
 4-3 6 4.88 4.00 4.88 4.00 
 
 7-1 6 3.42 3.42 
 
 7-2 6 3.34 3.34 
 
 7-3 6 3.42 3.39 3.42 3.39 
 
 Notes 
 
446 University of California Publications in Agricultural Sciences [Vol. 3 
 
 Table 66 — Altamont Clay Loam, Second Crop 
 
 Soy Beans (following Phaseolus) 
 
 Planted, August 10, 1916. Harvested November 17, 1916 
 
 Straw Grain Total dry matter 
 
 . . A . . A . . A „ 
 
 r \ f \ r \ 
 
 No. Average Average Average 
 
 Pot plants Weight weight Weight weight Weight weight Notes 
 
 3-1 6 5.64 5.64 
 
 3-2 6 4.94 4.94 
 
 3-3 6 4.84 5.14 4.84 5.14 
 
 4-1 6 4.74 4.74 
 
 4-2 6 4.64 4.64 
 
 4-3 6 4.71 4.70 4.71 4.70 
 
 7-1 6 5.25 5.25 
 
 7-2 6 3.28 3.28 
 
 7-3 6 4.39 4.31 4.39 4.31 
 
 Hanford fine sandy loam. First crop. — This soil type, with sam- 
 ples from nine different localities in California, gave a much wider 
 range of conditions and made a much more interesting series. The 
 plants used as indicators in this series were milo (twice), millet, cow- 
 peas (twice), and soy beans. The milo was thinned to eight plants 
 per pot, the millet to twelve plants, and the cowpeas and soy beans 
 to six plants. Set A of cowpeas, and set B of milo were unfavorably 
 located, so that the results of these sets should be discounted. 
 
 It is interesting to note the large differences in the average 
 weights from soil to soil (tables 67-72, and fig. 31), as compared with 
 the photographs, in which little variation appears. See especially the 
 soy bean series. In this series two things are to be noted : 
 
 1. Averages on soils nos. 15 and 25 are hardly representative be- 
 cause in both cases excess moisture, from a leaky roof and too heavy 
 watering, depressed growth. The tendency to become compact and to 
 remain wet and cold shown by soil no. 15 aided the milo and depressed 
 the soy beans. 
 
 2. The loose, open texture of soil no. 22 seemingly favored the soy 
 bean growth, though the other plants did not do as well on this soil 
 as on most of the others. 
 
1919] 
 
 Pendleton: A Study of Soil Types 
 
 447 
 
 Comparing the more satisfactory grains, milo A and millet, it will 
 be seen that there is somewhat of a parallelism from soil to soil. The 
 legumes do not always respond similarly to the grains, as in the Diablo 
 first crop, yet in the Diablo second crop and the Altamont first and 
 second crops the response of grain and legume seems quite similar. 
 Hence, it is not safe in every case to judge as to the relationships 
 shown by legumes and non-legumes. 
 
 SqyB^o/* 
 
 Fig. 31 
 
 Fig. 31. Graph showing the total dry matter produced by millet, milo (two 
 series), cowpeas (two series), and soy beans on the nine samples of Hanford 
 fine sandy loam. First crop. 
 
 Considering all the variations, one might say that soil no. 23 was 
 seemingly among the better soils, and soils nos. 16 and 22 among the 
 poorer soils. Yet when discussing whether the soils be the same or 
 similar, according to the criterion of the dry weight, one of the Han- 
 ford groups will be similar according to one crop, and an overlapping 
 group similar according to the second crop. It can be said with rea- 
 sonable certainty that these Hanford soils are not closely similar to 
 one another. 
 
448 
 
 University of California Publications in Agricultural Sciences [Vol. 3 
 
 Pot 
 14-1 
 14-2 
 14-3 
 
 15-1 
 15-2 
 15-3 
 
 16-1 
 16-2 
 16-3 
 
 19-1 
 19-2 
 19-3 
 
 20-1 
 20-2 
 20-3 
 
 22-1 
 22-2 
 22-3 
 
 23-1 
 23-2 
 23-3 
 
 24-1 
 24-2 
 24-3 
 
 25-1 
 25-1 
 25-2 
 25-3 
 
 No. 
 
 plants 
 
 Table 67 — Hanford Fine Sandy Loam, First Crop 
 
 Milo A 
 
 Planted, June 10, 1916. Harvested, November 18, 1916 
 
 Straw Grain Total dry matter 
 
 „ A A . . A 
 
 ( \ r \ r \ 
 
 Average Average Average 
 
 Weight weight Weight weight Weight weight Notes 
 
 15.34 15.34 Most plants bore 
 
 12.50 12.50 no grain; some 
 
 10.15 12.66 10.15 12.66 ^ rain was im - 
 
 mature at har- 
 vest. These 
 cases noted, 
 but no grain 
 weighed. 
 
 13.14 13.14 
 
 14.50 14.50 
 
 15.21 14.28 15.21 14.28 Not mature 
 
 8.67 8.67 
 
 5.86 5.86 
 
 4.76 6.43 4.76 6.43 
 
 7.65 7.65 
 
 14.11 14.11 
 
 7.01 7.01 
 
 14.10 14.10 
 
 10.15 10.15 
 
 7.68 10.64 7.68 10.64 Not mature 
 
 5.34 5.34 
 
 5.88 5.88 
 
 5.35 5.52 5.35 5.52 
 
 8.90 8.90 Not mature 
 
 10.04 10.04 Not mature 
 
 8.67 9.20 8.67 9.20 
 
 10.82 10.82 
 
 9.92 9.92 Not mature 
 
 6.01 8.92 6.01 8.92 Not mature 
 
 11.26 11.26 
 
 11.26 11.26 
 
 5.70 5.70 
 
 9.33 8.76 9.33 8.76 
 
1919] Pendleton: A Study of Soil Types 449 
 
 Table 68 — Hanford Fine Sandy Loam, First Crop 
 
 Milo B 
 
 Planted, June 10, 1916. Harvested, November 20, 1916 
 
 Straw Grain Total dry matter 
 
 A A. A 
 
 No. Average Average Average 
 
 Pot plants Weight weight Weight weight Weight weight Notes 
 
 14-., 8 10.75 10.75 
 
 14-2 8 10.95 10.95 
 
 14-3 8 8.84 10.18 8.84 10.18 
 
 15-1 5 5.25 5.25 
 
 15-2 4 4.62 4.62 
 
 15-3 2 3.92 4.60 3.92 4.60 
 
 16-1 7 7.36 7.36 
 
 16-2 2 2.18 2.18 
 
 16-3 4 2.74 4.09 2.74 4.09 
 
 19-1 3 3.73 3.73 
 
 19-2 8 4.79 4.79 
 
 19-3 8 9.60 6.04 9.60 6.04 
 
 20-1 8 8.14 8.14 
 
 20-2 8 3.23 3.23 
 
 20-3 8 3.22 4.86 3.22 4.86 
 
 22-1 6 4.74 4.74 
 
 22-2 5 3.01 3.01 
 
 22-3 7 3.19 3.64 3.19 3.64 
 
 23-1 8 5.68 5.68 
 
 23-2 5 7.72 7.72 
 
 23-3 8 6.93 6.78 6.93 6.78 
 
 24-1 3 3.16 3.16 
 
 24-2 6 5.64 5.64 
 
 24-3 6 3.26 4.02 3.26 4.02 
 
 25-1 4 3.07 3.07 
 
 25-2 3 2.34 2.34 
 
 25-3 8 4.34 3.25 4.34 3.25 
 
450 University of California Publications in Agricultural Sciences [Vol. 3 
 
 Table 69 — Hanford Fine Sandy Loam, First Crop 
 Millet 
 
 Planted, June 10, 1916. Harvested: Nos. 15-25, September 20, 1916; No. 14, 
 
 October 6, 1916 
 
 
 No. 
 plants 
 
 Straw 
 
 A 
 
 Grain 
 
 Total dry matter 
 
 A 
 
 Average 
 Weight weight 
 
 
 Pot 
 
 r 
 
 Weight 
 
 Average 
 weight 
 
 r 
 Weight 
 
 Average 
 weight 
 
 Notes 
 
 14-1 
 
 12 
 
 3.75 
 
 
 2.90 
 
 
 6.65 
 
 
 
 14-2 
 
 13 
 
 4.23 
 
 
 2.95 
 
 
 7.18 
 
 
 
 14-3 
 
 14 
 
 3.46 
 
 3.81 
 
 2.01 
 
 2.62 
 
 5.47 
 
 6.43 
 
 
 15-1 
 
 12 
 
 3.63 
 
 
 1.02 
 
 
 4.65 
 
 
 
 15-2 
 
 12 
 
 4.63 
 
 
 1.31 
 
 
 5.93 
 
 
 
 15-3 
 
 12 
 
 3.86 
 
 4.04 
 
 1.12 
 
 1.15 
 
 4.98 
 
 5.19 
 
 
 16-1 
 
 13 
 
 1.96 
 
 
 0.74 
 
 
 2.70 
 
 
 
 16-2 
 
 12 
 
 3.10 
 
 
 1.81 
 
 
 4.91 
 
 
 
 16-3 
 
 12 
 
 1.52 
 
 2.19 
 
 0.73 
 
 1.09 
 
 2.25 
 
 3.29 
 
 
 19-1 
 
 12 
 
 1.85 
 
 
 0.73 
 
 
 2.58 
 
 
 Seed immature 
 
 19-2 
 
 12 
 
 1.71 
 
 
 0.76 
 
 
 2.48 
 
 
 Poor. Lack of 
 
 19-3 
 
 12 
 
 2.00 
 
 1.85 
 
 0.69 
 
 0.73 
 
 2.69 
 
 2.58 
 
 drainage? 
 
 20-1 
 
 12 
 
 6.54 
 
 
 2.78 
 
 
 9.32 
 
 
 Possible error in 
 
 20-2 
 20-3 
 
 12 
 12 
 
 1.70 
 6.57 
 
 6.55 
 
 1.01 
 2.21 
 
 2.50 
 
 2.71 
 
 8.78 
 
 9.05 
 
 grain weight. 
 Original shows 
 6 grams 
 
 22-1 
 
 12 
 
 2.04 
 
 
 0.65 
 
 
 2.69 
 
 
 
 22-2 
 
 12 
 
 2.32 
 
 
 0.68 
 
 
 3.00 
 
 
 
 22-3 
 
 12 
 
 4.44 
 
 2.93 
 
 1.90 
 
 1.08 
 
 6.34 
 
 4.01 
 
 
 23-1 
 
 12 
 
 6.12 
 
 
 1.21 
 
 
 7.33 
 
 
 
 23-2 
 
 12 
 
 6.13 
 
 
 2.14 
 
 
 8.27 
 
 
 
 23-3 
 
 12 
 
 6.01 
 
 6.08 
 
 1.97 
 
 1.78 
 
 7.99 
 
 7.86 
 
 
 24-1 
 
 12 
 
 4.18 
 
 
 1.50 
 
 
 5.69 
 
 
 
 24-2 
 
 12 
 
 2.80 
 
 
 0.91 
 
 
 3.70 
 
 
 
 24-3 
 
 11 
 
 4.89 
 
 3.96 
 
 2.08 
 
 1.50 
 
 6.98 
 
 5.46 
 
 
 25-1 
 
 12 
 
 2.06 
 
 
 0.77 
 
 
 2.83 
 
 
 
 25-2 
 
 12 
 
 2.01 
 
 
 0.51 
 
 
 2.52 
 
 
 
 25-3 
 
 12 
 
 4.31 
 
 2.79 
 
 2.15 
 
 1.14 
 
 6.46 
 
 3.94 
 
 
1919J 
 
 Pendleton: A Study of Soil Types 
 
 451 
 
 Table 70 — Hanford Fine Sandy Loam, First Crop 
 
 Soy Beans 
 
 Planted, June 10, 1916. Harvested, December 11, 1916 
 
 Straw Beans Total dry matter 
 
 f ^ f ^ f A ^ 
 
 No. Average Average Average 
 
 Pot plants Weight weight Weight weight Weight weight Notes 
 
 14-1 6 16.69 16.69 Immature seed 
 
 14-2 6 16.28 16.28 Immature seed 
 
 14-3 6 11.89 14.95 0.44 0.15 12.33 15.10 Immature seed 
 
 15-1 6 14.08 0.23 14.31 Immature seed 
 
 15-2 6 5.17 5.17 Immature seed 
 
 15-3 6 6.53 8.59 0.08 6.53 8.67 Immature seed 
 
 16-1 6 12.63 0.32 12.95 Immature seed 
 
 16-2 6 14.60 14.60 Immature seed 
 
 16-3 6 16.60 14.61 0.11 16.60 14.72 Immature seed 
 
 19-1 6 12.84 12.84 Immature seed 
 
 19-2 6 11.68 11.68 Immature seed 
 
 19-3 6 16.03 13.52 16.03 13.52 Immature seed 
 
 20-1 6 8.77 8.77 Immature seed 
 
 20-2 6 16.33 16.33 Immature seed 
 
 20-3 6 14.27 13.13 14.27 13.13 Immature seed 
 
 22-1 6 20.28 20.28 Immature seed 
 
 22-2 6 19.44 19.44 Immature seed 
 
 22-3 6 15.60 18.44 15.60 18.44 Immature seed 
 
 23-1 6 21.42 21.42 No seed 
 
 23-2 6 20.75 ...... 20.75 No seed 
 
 23-3 6 20.68 20.95 20.68 20.95 Immature seed 
 
 24-1 6 17.37 17.37 Immature seed 
 
 24-2 6 21.24 21.24 Immature seed 
 
 24-3 6 13.70 17.43 13.70 17.43 Immature seed 
 
 25-1 6 5.53 . 5.53 Eained on; exclud- 
 ed from average 
 
 25-2 6 17.85 17.85 No seed 
 
 25-3 6 21.58 19.71 21.58 19.71 Immature seed 
 
452 University of California Publications in Agricultural Sciences [Vol. 3 
 
 Table 71 — Hanford Fine Sandy Loam, First Crop 
 
 Cowpeas A 
 
 Planted, June 10, 1916. Harvested, October 21, 1916 
 
 
 No. 
 plants 
 
 Straw- 
 
 Beans 
 
 A 
 
 Total d 
 f 
 
 Weight 
 
 ry matter 
 
 Pot 
 
 Average 
 Weight weight 
 
 r ^ 
 Average 
 Weight weight 
 
 Average 
 weight Notes 
 
 14-1 
 
 6 
 
 2.99 
 
 0.93 
 
 3.92 
 
 
 14-2 
 
 6 
 
 3.52 
 
 
 3.52 
 
 
 14-3 
 
 6 
 
 4.18 3.56 
 
 
 4.18 
 
 3.87 
 
 15-1 
 
 „ 
 
 
 
 
 
 15-2 
 
 
 
 
 
 
 15-3 
 
 -- 
 
 
 
 
 
 16-1 
 
 1 
 
 2.98 
 
 
 2.98 
 
 Immature seed 
 
 16-2 
 
 3 
 
 3.05 
 
 1.50 
 
 4.58 
 
 
 16-3 
 
 4 
 
 2.60 2.88 
 
 2.16 1.22 
 
 4.76 
 
 4.10 
 
 19-1 
 
 6 
 
 1.49 
 
 0.27 
 
 1.77 
 
 
 19-2 
 
 6 
 
 1.54 
 
 0.28 
 
 1.82 
 
 
 19-3 
 
 2 
 
 1.10 1.38 
 
 0.47 0.34 
 
 1.57 
 
 1.72 
 
 20-1 
 
 6 
 
 2.86 
 
 0.32 
 
 3.18 
 
 
 20-2 
 
 6 
 
 2.08 
 
 0.58 
 
 2.66 
 
 
 20-3 
 
 6 
 
 2.99 2.64 
 
 0.33 0.41 
 
 3.32 
 
 3.05 
 
 22-1 
 
 5 
 
 1.80 
 
 0.23 
 
 2.02 
 
 
 22-2 
 
 .. 
 
 
 
 
 
 22-3 
 
 2 
 
 1.96 1.88 
 
 0.39 0.31 
 
 2.35 
 
 2.19 
 
 23-1 
 
 .. 
 
 
 
 
 
 23-2 
 
 1 
 
 1.80 
 
 0.76 
 
 2.57 
 
 
 23-3 
 
 
 1.80 
 
 0.76 
 
 
 2.57 
 
 24-1 
 
 2 
 
 1.06 
 
 0.25 
 
 1.30 
 
 
 24-2 
 
 1 
 
 1.80 
 
 1.29 
 
 3.09 
 
 
 24-3 
 
 2 
 
 1.75 1.54 
 
 0.45 0.66 
 
 2.20 
 
 2.20 
 
 25-1 
 
 3 
 
 2.74 
 
 2.03 
 
 4.78 
 
 
 25-2 
 
 1 
 
 1.88 
 
 2.28 
 
 4.17 
 
 
 25-3 
 
 2 
 
 2.12 2.25 
 
 1.24 1.85 
 
 3.36 
 
 4.10 
 
1919] Pendleton: A Study of Soil Types 453 
 
 Table 72 — Hanford Fine Sandy Loam, First Crop 
 
 Cowpeas B 
 
 Planted, June 10, 1916. Harvested, November 21, 1916 
 
 Straw Beans Total dry matter 
 
 ' \ » ' * »' " > 
 
 No. Average Average Average 
 
 Pot plants Weight weight "Weight weight Weight weight Notes 
 
 14-1 6 3.94 3.94 
 
 14-2 6 5.93 5.92 
 
 14-3 6 3.32 4.39 3.32 4.39 
 
 15-1 6 7.24 7.24 
 
 15-2 6 5.34 5.34 
 
 15-3 6 4.61 5.74 4.61 5.74 
 
 16-1 6 5.90 5.90 
 
 16-2 6 5.82 5.82 
 
 16-3 6 3.65 5.12 3.65 5.12 
 
 19-1 6 3.34 3.34 
 
 19-2 6 3.38 3.38 
 
 19-3 6 3.87 3.53 3.87 3.53 1 died early 
 
 20-1 6 3.09 3.09 
 
 20-2 6 3.15 3.15 1 died early 
 
 20-3 6 2.80 3.01 ..,. 2.80 3.01 
 
 22-1 6 3.12 3.12 
 
 22-2 6 3.61 3.61 
 
 22-3 6 4.92 3.88 4.92 3.88 
 
 23-1 6 4.59 4.59 
 
 23-2 6 6.04 6.04 
 
 23-3 6 4.08 4.90 4.08 4.90 
 
 24-1 6 3.81 3.81 
 
 24-2 5 4.28 4.28 
 
 24-3 6 6.42 4.84 6.42 4.84 
 
 25-1 5 4.17 4.17 
 
 25-2 6 3.93 3.93 1 died early 
 
 25-3 6 4.86 4.32 4.86 4.32 
 
 Hanford fine sandy loam. Second crop. — Barley (twice), oats, 
 wheat, bur clover (Medicago sp.), and Melilotus indica were the indi- 
 cator crops used when the Hanford soils were planted the second time. 
 In all cases a sufficient quantity of seed was used to insure the growth 
 of more plants than would be raised to maturity. Later the plants 
 in each pot were thinned to six in number, good specimens and well 
 
454 University of California Publications in Agricultural Sciences [Vol. 3 
 
 spaced. The final number of plants varied, but was almost always six. 
 An attempt was made to reduce at least partially the shading and 
 exposure effects. The pots were periodically changed from position 
 to position on the bench. 
 
 The total dry weights produced on the several soils are interesting 
 (tables 73-78, and fig. 33). The grains gave more uniform results in 
 this crop than in the first. Soils nos. 14 and 23 show the best crops, 
 and they are the ones that have the highest amounts of total nitrogen. 
 The legumes selected must have been particularly well adapted to the 
 growing conditions and the soils, because the growth was enormous. 
 In the amount of dry matter produced the parallelism between the 
 two legumes from soil to soil is close. It is noteworthy that soil no. 14, 
 
 Wheat 
 Bur Clover 
 Oats 
 "^Meli lotus 
 
 26 ^ arle ^ 
 
 Fig.3£ 
 
 Fig. 32. Graph showing the total dry matter produced by barley, wheat, 
 oats, rye, bur clover, and Melilotus indica on the eight samples of San Joaquin 
 sandy loam. First and only crop. 
 
 which showed the highest total nitrogen and produced the most dry 
 matter from the grains, gave the poorest crop of legumes. The notes 
 taken during the growing period show that the relative appearances 
 quite early and throughout the period of growth are usually a good 
 index to the relative amounts of dry matter produced. This is so, 
 even though the photographs of the mature plants do not show dif- 
 ferences nearly as great in magnitude as do the dry weights. 
 
 This type does not show any marked tendency for the several soils 
 to approach a more uniform crop producing capacity through being 
 kept under the same conditions. In fact, the second crop shows 
 greater variations than the first. And this type does not show that 
 these nine soils, mapped under a single type name, are closely similar 
 to one another in crop producing power. 
 
1919] Pendleton: A Study of Soil Types 455 
 
 Table 73 — Hanford Fine Sandy Loam, Second Crop 
 
 Wheat (following millet) 
 Planted, October 30, 1916. Harvested, June 21, 1917 
 Straw Grain Total dry matter 
 
 , A . . A „ . A . 
 
 r ^ f ~\ f ^ 
 
 No. Average Average Average 
 
 plants Weight weight Weight weight Weight weight Notes 
 
 3.55 14.30 
 
 2.10 7.30 
 
 10.26 6.45 4.03 21.30 14.30 
 
 1.30 4.65 
 
 1.50 6.35 
 
 3.66 1.10 1.30 3.90 4.96 
 
 Pot 
 
 plants 
 
 Weight 
 
 14-1 
 
 6 
 
 10.75 
 
 14-2 
 
 5 
 
 5.20 
 
 14-3 
 
 6 
 
 14.85 
 
 15-1 
 
 6 
 
 3.55 
 
 15-2 
 
 6 
 
 4.85 
 
 15-3 
 
 6 
 
 2.80 
 
 16-1 
 
 6 
 
 3.20 
 
 16-2 
 
 6 
 
 8.20 
 
 0.95 4.15 
 
 3.70 11.90 Eained on, exclud- 
 
 ed from average 
 
 16-3 6 2.80 3.00 0.70 0.82 3.50 3.82 
 
 0.75 
 
 0.65 
 
 2.60 0.60 0.66 
 
 2.80 
 
 1.55 
 
 4.75 12.90 2.17 
 
 0.90 
 
 0.40 
 
 4.18 0.90 0.73 
 
 1.60 
 
 1.60 
 
 4.46 1.10 1.43 
 
 8.30 
 
 0.90 
 
 3.20 5.40 0.90 
 
 9.05 
 
 0.35 
 
 2.37 0.80 0.57 
 
 19-1 
 
 6 
 
 2.80 
 
 19-2 
 
 6 
 
 2.80 
 
 19-3 
 
 6 
 
 2.20 
 
 20-1 
 
 6 
 
 5.45 
 
 20-2 
 
 6 
 
 4.05 
 
 20-3 
 
 6 
 
 21.35 
 
 22-1 
 
 6 
 
 4.15 
 
 22-2 
 
 6 
 
 3.95 
 
 22-3 
 
 6 
 
 4.45 
 
 23-1 
 
 6 
 
 4.90 
 
 23-2 
 
 6 
 
 4.75 
 
 23-3 
 
 6 
 
 3.75 
 
 24-1 
 
 6 
 
 18.60 
 
 24-2 
 
 6 
 
 3.20 
 
 24-3 
 
 6 
 
 23.75 
 
 25-1 
 
 6 
 
 15.75 
 
 25-2 
 
 6 
 
 2.50 
 
 25-3 
 
 6 
 
 2.25 
 
 3.55 
 
 
 
 3.45 
 
 
 
 2.80 
 
 3.26 
 
 I 
 
 8.25 
 
 
 
 5.60 
 
 
 
 34.25 
 
 6.90 
 
 Eained on, exclud- 
 
 5.05 
 
 
 ed from average 
 
 4.35 
 
 
 
 5.35 
 
 4.92 
 
 
 6.50 
 
 
 
 6.35 
 
 
 
 4.85 
 
 5.90 
 
 
 26.90 
 
 
 Rained on, exclud- 
 ed from average 
 
 4.10 
 
 
 Rained on, exclud- 
 
 29.15 
 
 4.10 
 
 ed from average 
 Rained on, exclud- 
 
 24.80 
 
 
 ed from average 
 
 2.85 
 
 
 
 3.05 
 
 2.95 
 
 
456 University of California Publications in Agricultural Sciences [Vol. 3 
 
 Table 74 — Hanford Fine Sandy Loam, Second Crop 
 
 Oats (following milo A) 
 Planted, November 22, 1916. Harvested, June 18, 1917 
 Straw Grain Total dry matter 
 
 „ A . , A A „ 
 
 t ^ r \ r "i 
 
 No. Average Average Average 
 
 weight Weight weight Weight weight Notes 
 
 2.90 6.70 
 
 1.85 5.25 
 
 3.47 2.40 2.38 5.65 5.86 
 
 Pot 
 
 plants 
 
 Weight 
 
 14-1 
 
 6 
 
 3.80 
 
 14-2 
 
 6 
 
 3.40 
 
 14-3 
 
 6 
 
 3.20 
 
 15-1 
 
 6 
 
 2.45 
 
 15-2 
 
 6 
 
 1.75 
 
 15-3 
 
 6 
 
 2.00 
 
 16-1 
 
 6 
 
 11.15 
 
 16-2 
 
 6 
 
 2.15 
 
 1.85 
 
 
 5.25 
 
 2.40 
 
 2.38 
 
 5.65 
 
 1.35 
 
 
 3.80 
 
 1.25 
 
 
 3.00 
 
 1.50 
 
 1.36 
 
 3.50 
 
 8.40 
 
 
 19.55 
 
 2.30 
 
 
 4.45 
 
 3.50 3.43 
 
 Eained on, exclud- 
 ed from average 
 Pot saturated with 
 soluble salts, ex- 
 cluded from av- 
 erage 
 16-3 6 1.15 2.15 0.70 2.30 1.85 4.45 
 
 19-1 
 
 6 
 
 1.75 
 
 
 1.25 
 
 
 3.00 
 
 
 
 19-2 
 
 6 
 
 4.55 
 
 
 2.95 
 
 
 7.50 
 
 
 
 19-3 
 
 6 
 
 1.35 
 
 2.55 
 
 0.95 
 
 1.72 
 
 2.30 
 
 4.27 
 
 
 20-1 
 
 6 
 
 10.45 
 
 
 6.30 
 
 
 16.75 
 
 
 Eained on, exclud- 
 ed from average 
 
 20-2 
 
 6 
 
 1.55 
 
 
 1.05 
 
 
 2.60 
 
 
 
 20-3 
 
 6 
 
 1.65 
 
 1.60 
 
 1.00 
 
 1.02 
 
 2.65 
 
 2.62 
 
 
 22-1 
 
 6 
 
 1.65 
 
 
 1.10 
 
 
 2.75 
 
 
 
 22-2 
 
 6 
 
 2.10 
 
 
 1.15 
 
 
 3.25 
 
 
 
 22-3 
 
 6 
 
 2.50 
 
 2.08 
 
 1.50 
 
 1.25 
 
 4.00 
 
 3.33 
 
 
 23-1 
 
 6 
 
 2.70 
 
 
 1.55 
 
 
 4.25 
 
 
 
 23-2 
 
 6 
 
 1.90 
 
 
 1.60 
 
 
 3.50 
 
 
 
 23-3 
 
 6 
 
 3.20 
 
 2.60 
 
 2.00 
 
 1.71 
 
 5.20 
 
 4.32 
 
 
 24-1 
 
 6 
 
 4.80 
 
 
 3.10 
 
 
 7.90 
 
 
 
 24-2 
 
 6 
 
 16.75 
 
 
 9.80 
 
 
 26.55 
 
 
 Rained on, exclud- 
 ed from average 
 
 24-3 
 
 6 
 
 3.35 
 
 4.07 
 
 2.35 
 
 2.73 
 
 5.70 
 
 6.80 
 
 
 25-1 
 
 6 
 
 1.95 
 
 
 1.30 
 
 
 3.25 
 
 
 
 25-3 
 
 6 
 
 2.25 
 
 2.00 
 
 1*40 
 
 1.30 
 
 3.65 
 
 3.30 
 
 
 25-2 
 
 6 
 
 1.80 
 
 
 1.20 
 
 
 3.00 
 
 
 

 No. 
 plants 
 
 Straw 
 
 Grain Total dry matter 
 
 K A 
 
 Pot 
 
 r 
 
 Weight 
 
 Average 
 weight 
 
 r y r y 
 Average Average 
 Weight weight Weight weight 
 
 14-1 
 
 6 
 
 4.75 
 
 
 4.30 9.05 
 
 14-2 
 
 6 
 
 9.22 
 
 
 9.00 18.22 
 
 14-3 
 
 6 
 
 11.97 
 
 8.65 
 
 10.85 8.05 22.82 16.69 
 
 1919] Pendleton: A Study of Soil Types 457 
 
 Table 75 — Hanford Fine Sandy Loam, Second Crop 
 
 Barley A (following cowpeas A) 
 Planted, October 30, 1916. Harvested, May 20, 1917 
 
 Notes 
 
 15-1 6 15.47 15.30 30.77 Kained on, exclud- 
 
 ed from average 
 3.29 
 4.39 4.12 3.70 
 
 6.42 
 
 2.55 
 
 4.01 1.71 3.56 
 
 1.80 
 1.91 
 
 2.70 2.25 1.98 
 
 2.90 
 
 2.80 
 
 3.44 7.45 2.85 
 
 2.07 
 
 3.53 
 
 4.10 2.73 2.78 
 
 3.35 
 
 4.23 
 
 6.24 4.20 3.93 
 
 2.54 
 
 9.75 
 
 3.90 3.57 3.05 
 
 1.75 4.22 Eained on, exclud- 
 ed from average 
 Pot broken, ex- 
 cluded from av- 
 erage 
 25-3 6 3.01 2.74 2.18 1.96 5.19 4.70 
 
 15-2 
 
 6 
 
 3.78 
 
 15-3 
 
 6 
 
 5.00 
 
 16-1 
 
 6 
 
 7.28 
 
 16-2 
 
 6 
 
 2.55 
 
 16-3 
 
 6 
 
 2.20 
 
 19-1 
 
 6 
 
 2.82 
 
 19-2 
 
 6 
 
 2.39 
 
 19-3 
 
 6 
 
 2.89 
 
 20-1 
 
 6 
 
 3.57 
 
 20-2 
 
 6 
 
 3.32 
 
 20-3 
 
 6 
 
 19.35 
 
 22-1 
 
 6 
 
 2.73 
 
 22-2 
 
 6 
 
 5.89 
 
 22-3 
 
 6 
 
 3.69 
 
 23-1 
 
 6 
 
 5.29 
 
 23-2 
 
 6 
 
 6.19 
 
 23-3 
 
 6 
 
 7.98 
 
 24-1 
 
 6 
 
 3.07 
 
 24-2 
 
 6 
 
 21.85 
 
 24-3 
 
 6 
 
 4.73 
 
 25-1 
 
 6 
 
 2.47 
 
 25-2 
 
 6 
 
 Lost 
 
 7.07 
 
 
 
 9.12 
 
 8.09 
 
 
 13.70 
 
 
 
 5.10 
 
 
 
 3.91 
 
 7.57 
 
 
 4.62 
 
 
 
 4.30 
 
 
 
 5.14 
 
 4.68 
 
 
 6.47 
 
 
 
 6.12 
 
 
 
 26.70 
 
 6.29 
 
 Eained on, exclud- 
 ed from average 
 
 4.80 
 
 
 
 9.42 
 
 
 
 6.42 
 
 6.88 
 
 
 8.64 
 
 
 
 10.42 
 
 
 
 12.18 
 
 10.41 
 
 
 5.61 
 
 
 
 31.60 
 
 
 
 8.30 
 
 6.95 
 
 
458 
 
 University of California Publications in Agricultural Sciences [Vol. 3 
 
 16-3 
 
 Table 76 — Hanford Fine Sandy Loam, Second Crop 
 
 Barley B (following soy beans) 
 Planted, January 31, 1917. Harvested, June 21, 1917 
 
 
 No. 
 plants 
 
 Straw 
 
 Grain 
 
 Total c 
 r 
 
 Weight 
 
 Lry matter 
 
 Pot 
 
 r "\ 
 Average 
 Weight weight 
 
 r 
 Weight 
 
 Average 
 weight 
 
 > 
 Average 
 weight 
 
 14-1 
 
 6 
 
 9.55 
 
 6.80 
 
 
 16.35 
 
 
 14-2. 
 
 6 
 
 6.05 
 
 5.40 
 
 
 11.45 
 
 
 14-3 
 
 6 
 
 3.80 6.47 
 
 2.10 
 
 4.76 
 
 5.90 
 
 11.23 
 
 15-1 
 
 6 
 
 3.50 
 
 2.80 
 
 
 6.30 
 
 
 15-2 
 
 6 
 
 3.20 
 
 1.70 
 
 
 4.90 
 
 
 15-3 
 
 6 
 
 4.05 3.58 
 
 2.60 
 
 2.36 
 
 6.65 
 
 5.95 
 
 16-1 
 
 6 
 
 3.10 
 
 1.45 
 
 
 4.55 
 
 
 16-2 
 
 6 
 
 9.20 
 
 8.20 
 
 
 17.40 
 
 
 Notes 
 
 7.35 
 
 19-1 
 
 6 
 
 3.05 
 
 19-2 
 
 6 
 
 2.65 
 
 19-3 
 
 6 
 
 2.15 
 
 20-1 
 
 6 
 
 3.35 
 
 20-2 
 
 6 
 
 4.20 
 
 20-3 
 
 6 
 
 2.55 
 
 22-1 
 
 6 
 
 2.05 
 
 22-2 
 
 6 
 
 2.90 
 
 22-3 
 
 6 
 
 3.15 
 
 23-1 
 
 6 
 
 3.10 
 
 23-2 
 
 6 
 
 3.10 
 
 23-3 
 
 6 
 
 3.40 
 
 24-1 
 
 6 
 
 3.10 
 
 24-2 
 
 6 
 
 10.10 
 
 24-3 
 
 3.05 
 
 3.10 
 
 2.62 
 
 3.36 
 
 2.70 
 
 3.20 
 
 2.65 
 
 4.50 
 
 0.80 
 2.20 
 1.85 
 
 2.60 
 3.20 
 2.15 
 
 1.75 
 2.35 
 2.25 
 
 2.05 
 2.95 
 2.75 
 
 1.45 
 
 5.80 
 
 2.35 
 
 1.45 11.85 
 
 3.85 
 4.85 
 4.00 
 
 1.61 
 
 2.65 
 
 2.12 
 
 2.58 
 
 1.90 
 
 5.95 
 7.40 
 4.70 
 
 3.80 
 5.25 
 5.40 
 
 5.15 
 6.05 
 6.15 
 
 3.70 
 15.90 
 
 5.40 
 
 4.55 
 
 4.23 
 
 6.02 
 
 4.82 
 
 Eained on, exclud- 
 ed from average 
 
 Eained on, exclud- 
 ed from average 
 
 Eained on, exclud- 
 ed from average 
 
 4.55 
 
 25-1 
 
 25-2 
 25-3 
 
 3.35 
 3.10 
 4.70 
 
 3.72 
 
 2.90 
 1.85 
 4.60 
 
 3.12 
 
 6.25 
 4.95 
 9.30 
 
 6.83 
 
1919] Pendleton: A Study of Soil Types 459 
 
 Table 77 — Hanford Fine Sandy Loam, Second Crop 
 
 Melilotus indica (following cowpeas B) 
 Planted, November 22, 1916. Harvested, June 21, 1917 
 
 
 No. 
 plants 
 
 Straw 
 
 Unhulled seed 
 
 A 
 
 Total d 
 Weight 
 
 ry matter 
 
 Pot 
 
 r 
 Weight 
 
 Average 
 weight 
 
 r 
 Weight 
 
 Average 
 weight 
 
 Average 
 weight Notes 
 
 14-1 
 
 6 
 
 17.00 
 
 
 15.80 
 
 
 32.80 
 
 
 14-3 
 
 6 
 
 13.25 
 
 
 16.45 
 
 
 29.70 
 
 
 14-3 
 
 6 
 
 4.40 
 
 15.12 
 
 3.10 
 
 16.12 
 
 7.50 
 
 31.25 Excluded from 
 average 
 
 15-1 
 
 6 
 
 35.00 
 
 
 34.75 
 
 
 69.75 
 
 
 15-2 
 
 6 
 
 24.85 
 
 
 27.28 
 
 
 52.05 
 
 
 15-3 
 
 6 
 
 28.95 
 
 29.60 
 
 32.70 
 
 31.58 
 
 61.65 
 
 61.15 
 
 16-1 
 
 5 
 
 23.50 
 
 
 24.90 
 
 
 48.40 
 
 
 16-2 
 
 6 
 
 30.80 
 
 
 25.50 
 
 
 56.30 
 
 
 16-3 
 
 6 
 
 23.65 
 
 25.98 
 
 25.70 
 
 25.37 
 
 49.35 
 
 51.35 
 
 19-1 
 
 6 
 
 20.50 
 
 
 18.35 
 
 
 38.85 
 
 
 19-2 
 
 6 
 
 26.90 
 
 
 23.20 
 
 
 50.10 
 
 
 19-3 
 
 6 
 
 26.20 
 
 24.53 
 
 27.40 
 
 22.98 
 
 53.60 
 
 47.52 
 
 20-1 
 
 6 
 
 20.55 
 
 
 17.80 
 
 
 38.35 
 
 
 20-2 
 
 6 
 
 20.75 
 
 
 21.20 
 
 
 41.95 
 
 
 20-3 
 
 6 
 
 28.85 
 
 23.38 
 
 26.05 
 
 21.68 
 
 54.90 
 
 45.07 
 
 22-1 
 
 6 
 
 28.00 
 
 
 28.10 
 
 
 56.10 
 
 
 22-2 
 
 6 
 
 32.30 
 
 
 34.20 
 
 
 66.50 
 
 
 22-3 
 
 6 
 
 28.25 
 
 29.52 
 
 31.85 
 
 31.38 
 
 60.10 
 
 60.90 
 
 23-1 
 
 6 
 
 38.05 
 
 
 34.25 
 
 
 72.30 
 
 
 23-2 
 
 6 
 
 34.40 
 
 
 36.55 
 
 
 70.95 
 
 
 23-3 
 
 6 
 
 32.25 
 
 34.90 
 
 32.35 
 
 34.38 
 
 64.60 
 
 69.28 
 
 24-1 
 
 6 
 
 37.35 
 
 
 31.40 
 
 
 68.75 
 
 
 24-2 
 
 6 
 
 25.90 
 
 
 28.10 
 
 
 54.00 
 
 
 24-3 
 
 6 
 
 29.05 
 
 30.77 
 
 30.15 
 
 29.88 
 
 59.20 
 
 60.65 
 
 25-1 
 
 6 
 
 25.35 
 
 
 30.45 
 
 
 55.80 
 
 
 25-2 
 
 6 
 
 33.90 
 
 
 35.90 
 
 
 69.80 
 
 
 25-3 
 
 6 
 
 32.10 
 
 30.45 
 
 36.65 
 
 34.33 
 
 68.75 
 
 64.78 
 
460 
 
 University of California Publications in Agricultural Sciences [Vol. 3 
 
 Table 78 — Hanford Fine Sandy Loam, Second Crop 
 
 Bur Clover (following milo B) 
 Planted, November 22, 1916. Harvested, June 25, 1917 
 
 
 No. 
 plants 
 
 Straw 
 
 A 
 
 Burs 
 
 A 
 
 
 Total dry 
 
 r 
 
 Weight 
 
 matter 
 
 Pot 
 
 Weight 
 
 Average 
 weight 
 
 r 
 Weight 
 
 Average 
 weight 
 
 Average 
 weight 
 
 14-1 
 
 7 
 
 6.70 
 
 
 17.55 
 
 
 24.25 
 
 
 14-2 
 
 6 
 
 7.00 
 
 
 16.85 
 
 
 23.85 
 
 
 14-3 
 
 6 
 
 6.10 
 
 6.60 
 
 14.50 
 
 16.30 
 
 20.60 
 
 22.90 
 
 15-1 
 
 6 
 
 13.30 
 
 
 29.10 
 
 
 42.40 
 
 
 15-2 
 
 6 
 
 14.45 
 
 
 33.10 
 
 
 47.55 
 
 
 15-3 
 
 6 
 
 17.10 
 
 14.95 
 
 26.65 
 
 29.62 
 
 43.75 
 
 44.56 
 
 16-1 
 
 6 
 
 8.85 
 
 
 15.40 
 
 
 24.25 
 
 
 16-2 
 
 6 
 
 12.25 
 
 
 29.60 
 
 
 41.85 
 
 
 16-3 
 
 6 
 
 10.05 
 
 10.38 
 
 21.90 
 
 22.30 
 
 31.95 
 
 32.68 
 
 19-1 
 
 6 
 
 9.90 
 
 
 19.90 
 
 
 29.80 
 
 
 19-2 
 
 6 
 
 7.70 
 
 
 17.80 
 
 
 25.50 
 
 
 19-3 
 
 6 
 
 8.20 
 
 8.60 
 
 22.40 
 
 20.03 
 
 30.60 
 
 28.63 
 
 20-1 
 
 6 
 
 7.90 
 
 
 22.50 
 
 
 30.40 
 
 
 20-2 
 
 6 
 
 9.75 
 
 
 23.30 
 
 
 33.05 
 
 
 20-3 
 
 6 
 
 8.70 
 
 8.78 
 
 20.50 
 
 22.10 
 
 29.20 
 
 30.88 
 
 22-1 
 
 6 
 
 15.90 
 
 
 38.00 
 
 
 53.90 
 
 
 22-2 
 
 6 
 
 13.20 
 
 
 23.40 
 
 
 36.60 
 
 
 22-3 
 
 6 
 
 14.50 
 
 14.53 
 
 31.30 
 
 30.90 
 
 45.80 
 
 45.43 
 
 23-1 
 
 6 
 
 14.45 
 
 
 37.40 
 
 
 51.85 
 
 
 23-2 
 
 6 
 
 13.55 
 
 
 27.30 
 
 
 40.85 
 
 
 23-3 
 
 6 
 
 12.05 
 
 13.35 
 
 28.00 
 
 30.90 
 
 40.05 
 
 44.25 
 
 24-1 
 
 6 
 
 10.60 
 
 
 24.30 
 
 
 34.90 
 
 
 24-2 
 
 6 
 
 12.10 
 
 
 34.10 
 
 
 46.20 
 
 
 24-3 
 
 6 
 
 10.25 
 
 10.98 
 
 24.00 
 
 27.46 
 
 34.25 
 
 38.45 
 
 25-1 
 
 6 
 
 17.90 
 
 
 40.00 
 
 
 57.90 
 
 
 25-2 
 
 6 
 
 14.60 
 
 
 30.80 
 
 
 45.40 
 
 
 25-3 
 
 6 
 
 13.35 
 
 15.28 
 
 26.40 
 
 32.40 
 
 39.75 
 
 47.68 
 
 Notes 
 
 San Joaquin sandy loam. — The samples of this type were the last 
 to be weighed into pots and planted, because of the lack of available 
 greenhouse space ; therefore the time allowed for the growing of but 
 one crop, instead of two, on each pot of soil. The crops used were 
 wheat, barley, rye, oats, bur clover (Medioago sp.), and Melilotns 
 indioa. As was done for the other types, an excess of seed was 
 planted. When the plants were well established, thinning reduced 
 the number to six plants per pot. 
 
 Since the specific gravity of this soil was high, because of the large 
 amount of quartz and the small amount of organic matter in its com- 
 position, six kilos of soil, instead of five, were weighed out into each 
 pot. The samples of this type have the very annoying peculiarities 
 of becoming very mushy if an excess of water be added, and of setting 
 
1919] Pendleton: A Study of Soil Types 461 
 
 with a very hard surface on drjdng. This makes the soils hard to 
 handle in greenhouse pot culture work. 
 
 The variation in crop growth from soil to soil, as shown by the 
 total dry matter produced (tables 79-84 and fig. 32), is rather 
 marked. That the several samples do not show equal crop producing 
 powers is very evident, though with regard to the several indicator 
 crops the soils would frequently not maintain the same order. Soil 
 no. 26 gave the poorest yields with all six crops. Except for wheat, 
 the soils nos. 10, 11, and 12 gave low yields with both the grains and 
 the legumes. It is interesting to note that wheat gave relatively high 
 yields with a number of the soils, and wheat has probably been raised 
 on these soils more than any other one crop. This series shows that, 
 as far as the samples represent the type and the crops used represent 
 crops as a whole, the soils mapped under a given type name are not 
 closely similar in crop producing power under greenhouse conditions. 
 
 Table 79 — San Joaquin Sandy Loam 
 
 Rye 
 
 Planted, November 22, 1916. Harvested, June 21, 1917 
 
 
 No. 
 
 plants 
 
 Sti 
 
 raw 
 
 Grain 
 
 Total dry 
 
 r 
 
 Weight 
 
 matter 
 
 Pot 
 
 Weight 
 
 Average 
 weight 
 
 r 
 Weight 
 
 Average 
 weight 
 
 Average 
 
 weight Not 
 
 10-1 
 
 6 
 
 1.70 
 
 
 0.30 
 
 
 2.00 
 
 
 10-2 
 
 6 
 
 2.30 
 
 
 0.35 
 
 
 2.65 
 
 
 10-3 
 
 6 
 
 2.05 
 
 2.02 
 
 0.65 
 
 0.43 
 
 2.70 
 
 2.45 
 
 11-1 
 
 6 
 
 3.15 
 
 
 0.70 
 
 
 3.85 
 
 
 11-2 
 
 6 
 
 2.25 
 
 
 0.70 
 
 
 2.95 
 
 
 11-3 
 
 4 
 
 3.20 
 
 2.87 
 
 0.70 
 
 0.70 
 
 3.90 
 
 3.57 
 
 12-1 
 
 6 
 
 1.65 
 
 
 0.45 
 
 
 2.10 
 
 
 12-2 
 
 6 
 
 2.45 
 
 
 0.85 
 
 
 3.30 
 
 
 12-3 
 
 6 
 
 2.40 
 
 2.17 
 
 0.65 
 
 0.65 
 
 3.05 
 
 2.82 
 
 13-1 
 
 6 
 
 4.20 
 
 
 1.25 
 
 
 5.45 
 
 
 13-2 
 
 6 
 
 4.30 
 
 
 0.80 
 
 
 5.10 
 
 
 13-3 
 
 6 
 
 3.75 
 
 4.08 
 
 1.60 
 
 1.22 
 
 5.35 
 
 5.30 
 
 17-1 
 
 6 
 
 7.55 
 
 
 1.60 
 
 
 9.15 
 
 Rained on 
 
 17-2 
 
 6 
 
 1.95 
 
 
 0.55 
 
 
 2.50 
 
 
 17-3 
 
 6 
 
 1.80 
 
 1.87 
 
 0.45 
 
 0.50 
 
 2.25 
 
 2.37 
 
 18-1 
 
 6 
 
 2.35 
 
 
 0.85 
 
 
 3.20 
 
 
 18-2 
 
 6 
 
 0.90 
 
 
 0.30 
 
 
 1.20 
 
 
 18-3 
 
 6 
 
 3.70 
 
 2.32 
 
 1.20 
 
 0.78 
 
 4.90 
 
 3.10 
 
 21-1 
 
 6 
 
 2.20 
 
 
 0.80 
 
 
 3.00 
 
 
 21-2 
 
 6 
 
 2.70 
 
 
 0.95 
 
 
 3.65 
 
 
 21-3 
 
 6 
 
 6.55 
 
 2.45 
 
 2.35 
 
 0.87 
 
 8.90 
 
 3.33 Rained on 
 
 26-1 
 
 6 
 
 1.50 
 
 
 0.60 
 
 
 2.10 . 
 
 
 26-2 
 
 6 
 
 2.55 
 
 
 0.75 
 
 
 3.30 
 
 
 26-3 
 
 6 
 
 2.50 
 
 2.18 
 
 0.70 
 
 0.68 
 
 3.20 
 
 2.87 
 
462 
 
 University of California Publications in Agricultural Sciences [Vol. 3 
 
 65 
 
 60 
 
 .35 
 
 50 
 
 45 
 
 40 
 
 85 
 
 30 
 
 25 
 
 20 
 
 15 
 
 10 
 
 
 
 
 
 
 / 
 / 
 
 \ 
 
 1 
 
 
 V 
 
 
 
 __L 
 
 / 
 / 
 
 \ 
 \ 
 
 
 / 
 
 \ 
 
 \ 
 
 \ 
 
 
 
 T 
 
 1 
 1 
 
 
 
 
 / 
 
 / 
 
 / 
 
 \ 
 \ 
 
 \ 
 
 
 1 
 1 
 
 
 
 
 / 
 
 / 
 
 / 
 
 
 N 
 
 ^\ 
 
 1 
 
 1 
 
 
 
 
 / / 
 
 
 
 
 
 
 
 
 / / 
 
 / / 
 
 
 
 
 
 
 
 
 / / 
 
 1 / 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 \ 
 
 
 
 
 
 
 
 
 w 
 
 
 
 
 
 
 
 
 \ 
 
 
 
 
 ~~~~~^-' :s *-, 
 
 t 
 
 
 **X' 
 
 
 "■•"^r.""^ 
 
 marAMk - 
 
 ?C 
 
 
 
 
 
 ^"* '"•. *S 
 
 Melilotus 
 
 Bur 
 Clover 
 
 Barley B 
 
 Barley A 
 
 Oats 
 
 Wheat 
 
 14 15 16 19 20 22 23 24 25 Soils 
 
 Fig. 33. Graph showing the total dry matter produced by wheat, oats, 
 
 barley (two series), bur clover, and Melilotus indica on the nine samples of 
 Ilanford fine sandy loam. Second crop. 
 
1919] Pendleton: A Study of Soil Types 463 
 
 Table 80 — San Joaquin Sandy Loam 
 Barley 
 Planted, October 30, 1916. Harvested, June 17, 1917 
 Straw Grain Total dry matter 
 
 Pot 
 
 No. 
 plants 
 
 r 
 Weight 
 
 Average 
 weight 
 
 r 
 Weight 
 
 Average 
 weight 
 
 r 
 
 Weight 
 
 Average 
 
 weight Notes 
 
 10-1 
 
 6 
 
 2.93 
 
 
 0.92 
 
 
 3.85 
 
 
 10-2 
 
 6 
 
 1.87 
 
 
 0.81 
 
 
 2.68 
 
 
 10-3 
 
 6 
 
 1.47 
 
 2.09 
 
 0.85 
 
 0.86 
 
 2.32 
 
 2.95 
 
 11-1 
 
 6 
 
 1.91 
 
 
 0.66 
 
 
 2.57 
 
 
 11-2 
 
 6 
 
 2.02 
 
 
 1.28 
 
 
 3.30 
 
 
 11-3 
 
 6 
 
 2.97 
 
 2.30 
 
 0.90 
 
 0.95 
 
 3.87 
 
 3.25 
 
 12-1 
 
 6 
 
 10.27 
 
 
 4.95 
 
 
 15.22 
 
 Eained on; exclud- 
 
 12-2 
 
 6 
 
 3.60 
 
 
 1.32 
 
 
 4.92 
 
 ed from average 
 
 12-3 
 
 6 
 
 3.49 
 
 3.54 
 
 0.43 
 
 0.87 
 
 3.92 
 
 4.42 
 
 13-1 
 
 6 
 
 2.14 
 
 
 1.46 
 
 
 3.60 
 
 
 13-2 
 
 6 
 
 3.19 
 
 
 1.78 
 
 
 4.97 
 
 
 13-3 
 
 6 
 
 3.28 
 
 2.87 
 
 1.77 
 
 1.67 
 
 5.05 
 
 4.53 
 
 17-1 
 
 6 
 
 3.89 
 
 
 2.17 
 
 
 6.06 
 
 
 17-2 
 
 6 
 
 3.74 
 
 
 1.80 
 
 
 5.54 
 
 
 17-3 
 
 6 
 
 2.44 
 
 3.35 
 
 0.80 
 
 1.59 
 
 3.24 
 
 4.95 
 
 18-1 
 
 6 
 
 4.65 
 
 
 1.93 
 
 
 6.58 
 
 
 18-2 
 
 6 
 
 3.74 
 
 
 1.94 
 
 
 5.68 
 
 
 18-3 
 
 6 
 
 5.61 
 
 4.66 
 
 2.34 
 
 2.07 
 
 7.95 
 
 6.74 
 
 21-1 
 
 6 
 
 2.05 
 
 
 1.53 
 
 
 3.58 
 
 
 21-2 
 
 6 
 
 2.10 
 
 
 1.80 
 
 
 3.90 
 
 
 21-3 
 
 6 
 
 3.81 
 
 2.65 
 
 2.33 
 
 1.88 
 
 6.14 
 
 4.54 
 
 26-1 
 
 6 
 
 1.12 
 
 
 0.63 
 
 
 1.75 
 
 
 26-2 
 
 6 
 
 1.08 
 
 
 0.41 
 
 
 1.49 
 
 
 26-3 
 
 6 
 
 1.20 
 
 1.13 
 
 0.70 
 
 0.58 
 
 1.90 
 
 1.71 
 
464 University of California Publications in Agricultural Sciences [Vol. 3 
 
 Table 81 — San Joaquin Sandy Loam 
 
 Wheat 
 
 Planted, October 30, 1916. Harvested, June 21, 1917 
 
 Straw Grain Total dry matter 
 
 Pot 
 
 No. 
 plants 
 
 Weight 
 
 Average 
 weight 
 
 f 
 Weight 
 
 *> 
 Average 
 weight 
 
 r 
 
 Weight 
 
 Average 
 
 weight Not 
 
 10-1 
 
 6 
 
 3.59 
 
 
 0.85 
 
 
 4.80 
 
 
 10-2 
 
 6 
 
 3.45 
 
 
 0.45 
 
 
 3.90 
 
 
 10-3 
 
 6 
 
 6.35 
 
 4.58 
 
 0.75 
 
 0.68 
 
 7.10 
 
 5.26 
 
 11-1 
 
 6 
 
 5.60 
 
 
 1.15 
 
 
 6.75 
 
 
 11-2 
 
 6 
 
 2.75 
 
 
 0.60 
 
 
 3.35 
 
 
 11-3 
 
 6 
 
 3.45 
 
 3.93 
 
 0.70 
 
 0.81 
 
 4.15 
 
 4.75 
 
 12-1 
 
 6 
 
 6.85 
 
 
 2.00 
 
 
 8.85 
 
 
 12-2 
 
 6 
 
 7.50 
 
 
 1.35 
 
 
 8.85 
 
 
 12-3 
 
 6 
 
 4.45 
 
 6.27 
 
 1.35 
 
 1.56 
 
 5.80 
 
 7.83 
 
 13-1 
 
 6 
 
 3.90 
 
 
 0.85 
 
 
 4.75 
 
 
 13-2 
 
 6 
 
 3.25 
 
 
 0.45 
 
 
 3.70 
 
 
 13-2 
 
 6 
 
 3.95 
 
 3.70 
 
 0.75 
 
 0.68 
 
 4.70 
 
 4.38 
 
 17-1 
 
 6 
 
 2.70 
 
 
 0.25 
 
 
 2.95 
 
 
 17-2 
 
 6 
 
 1.20 
 
 
 0.45 
 
 
 1.65 
 
 
 17-3 
 
 6 
 
 2.75 
 
 2.21 
 
 none 
 
 0.23 
 
 2.75 
 
 2.45 
 
 18-1 
 
 6 
 
 5.90 
 
 
 1.50 
 
 
 7.40 
 
 
 18-2 
 
 6 
 
 7.90 
 
 
 2.40 
 
 
 10.30 
 
 Rained on 
 
 18-3 
 
 6 
 
 5.00 
 
 5.45 
 
 1.00 
 
 1.25 
 
 6.00 
 
 6.70 
 
 21-1 
 
 6 
 
 3.10 
 
 
 1.05 
 
 
 4.15 
 
 
 21-2 
 
 5 
 
 4.30 
 
 
 0.75 
 
 
 5.05 
 
 
 21-3 
 
 6 
 
 8.40 
 
 3.70 
 
 2.45 
 
 0.90 
 
 10.85 
 
 4.60 Rained on 
 
 26-1 
 
 6 
 
 2.35 
 
 
 0.55 
 
 
 2.90 
 
 
 26-2 
 
 6 
 
 0.40 
 
 
 none 
 
 
 0.40 
 
 Rained on 
 
 26-3 
 
 6 
 
 2.60 
 
 2.47 
 
 0.35 
 
 0.45 
 
 2.95 
 
 2.92 
 
1919] Pendleton: A Study of Soil Types 465 
 
 Table 82 — San Joaquin Sandy Loam 
 
 Oats 
 
 Planted, November 22, 1916. Harvested, June 17, 1917 
 
 Straw Grain Total dry matter 
 
 Pot 
 
 No. 
 plants 
 
 r 
 
 Weight 
 
 Average 
 weight 
 
 r 
 Weight 
 
 Average 
 weight 
 
 Weight 
 
 Average 
 weight 
 
 10-1 
 
 6 
 
 2.25 
 
 
 0.90 
 
 
 3.15 
 
 
 10-2 
 
 6 
 
 3.65 
 
 
 1.90 
 
 
 5.55 
 
 
 10-3 
 
 6 
 
 1.70 
 
 2.53 
 
 0.50 
 
 1.10 
 
 2.20 
 
 3.63 
 
 11-1 
 
 6 
 
 2.25 
 
 
 1.25 
 
 
 3.50 
 
 
 11-2 
 
 6 
 
 1.75 
 
 
 0.95 
 
 
 2.70 
 
 
 11-3 
 
 6 
 
 2.10 
 
 2.03 
 
 1.00 
 
 1.07 
 
 3.10 
 
 3.10 
 
 12-1 
 
 6 
 
 1.70 
 
 
 0.90 
 
 
 2.60 
 
 
 12-2 
 
 6 
 
 2.40 
 
 
 1.00 
 
 
 3.40 
 
 
 12-3 
 
 6 
 
 2.35 
 
 2.15 
 
 1.05 
 
 0.98 
 
 3.40 
 
 3.13 
 
 13-1 
 
 6 
 
 2.25 
 
 
 1.20 
 
 
 3.45 
 
 
 13-2 
 
 6 
 
 2.40 
 
 
 1.10 
 
 
 3.50 
 
 
 13-3 
 
 6 
 
 2.70 
 
 2.45 
 
 1.70 
 
 1.33 
 
 4.40 
 
 3.78 
 
 17-1 
 
 6 
 
 0.80 
 
 
 0.55 
 
 
 1.35 
 
 
 17-2 
 
 6 
 
 1.50 
 
 
 0.90 
 
 
 2.40 
 
 
 17-3 
 
 6 
 
 1.25 
 
 1.90 
 
 0.70 
 
 0.72 
 
 1.95 
 
 1.90 
 
 18-1 
 
 6 
 
 1.70 
 
 
 1.00 
 
 
 2.70 
 
 
 18-2 
 
 6 
 
 1.15 
 
 
 0.60 
 
 
 1.75 
 
 
 18-3 
 
 6 
 
 1.10 
 
 1.32 
 
 0.50 
 
 0.70 
 
 1.60 
 
 2.02 
 
 21-1 
 
 6 
 
 1.85 
 
 
 0.95 
 
 
 2.80 
 
 
 21-2 
 
 6 
 
 2.35 
 
 
 1.05 
 
 
 3.40 
 
 
 21-3 
 
 6 
 
 1.00 
 
 1.73 
 
 0.55 
 
 0.85 
 
 1.55 
 
 2.58 
 
 26-1 
 
 6 
 
 1.55 
 
 
 0.60 
 
 
 2.15 
 
 
 26-2 
 
 6 
 
 1.35 
 
 
 0.80 
 
 
 2.15 
 
 
 26-3 
 
 6 
 
 1.65 
 
 1.52 
 
 0.70 
 
 0.70 
 
 2.35 
 
 2.22 
 
 Notes 
 
466 University of California Publications in Agricultural Sciences [Vol. 3 
 
 Table 83 — San Joaquin Sandy Loam 
 
 Bur Clover 
 
 Planted, November 22, 1916. Harvested, June 17, 1917 
 
 Straw Seed in burs Total dry matter 
 
 Pot 
 
 No. 
 plants 
 
 Weight 
 
 Average 
 weight 
 
 r 
 
 Weight 
 
 Average 
 weight 
 
 r 
 
 Weight 
 
 Average 
 
 weight Notes 
 
 10-1 
 
 6 
 
 0.50 
 
 
 0.95 
 
 
 1.45 
 
 
 10-2 
 
 6 
 
 1.50 
 
 
 1.65 
 
 
 3.15 
 
 
 10-3 
 
 6 
 
 0.50 
 
 0.83 
 
 1.75 
 
 1.45 
 
 2.25 
 
 2.28 
 
 11-1 
 
 6 
 
 0.90 
 
 
 2.00 
 
 
 2.90 
 
 
 11-2 
 
 6 
 
 0.25 
 
 
 1.00 
 
 
 1.25 
 
 
 11-3 
 
 6 
 
 0.30 
 
 0.48 
 
 1.10 
 
 1.37 
 
 1.40 
 
 1.85 
 
 12-1 
 
 6 
 
 0.90 
 
 
 3.00 
 
 
 3.90 . 
 
 
 12-2 
 
 6 
 
 2.15 
 
 
 5.30 
 
 
 7.45 
 
 
 12-3 
 
 6 
 
 1.50 
 
 1.52 
 
 1.90 
 
 3.40 
 
 3.40 
 
 4.92 
 
 13-1 
 
 6 
 
 1.55 
 
 
 3.45 
 
 
 5.00 
 
 
 13-2 
 
 6 
 
 0.75 
 
 
 2.80 
 
 
 3.55 
 
 
 13-3 
 
 6 
 
 4.35 
 
 1.15 
 
 5.70 
 
 3.12 
 
 9.05 
 
 4.27 Excluded from av- 
 erage 
 
 17-1 
 
 6 
 
 0.70 
 
 
 2.05 
 
 
 2.75 
 
 
 17-2 
 
 6 
 
 2.35 
 
 
 3.85 
 
 • 
 
 6.20 
 
 Excluded from av- 
 erage 
 
 17-3 
 
 6 
 
 0.90 
 
 0.80 
 
 1.70 
 
 1.87 
 
 2.60 
 
 2.67 
 
 18-1 
 
 6 
 
 1.20 
 
 
 3.40 
 
 
 4.60 
 
 
 18-2 
 
 6 
 
 3.25 
 
 
 6.65 
 
 
 9.90 
 
 Excluded from av- 
 erage 
 
 18-3 
 
 6 
 
 1.80 
 
 1.50 
 
 4.85 
 
 4.12 
 
 6.65 
 
 5.62 
 
 21-1 
 
 6 
 
 3.35 
 
 
 3.70 
 
 
 7.05 
 
 
 21-2 
 
 6 
 
 2.00 
 
 
 3.90 
 
 
 5.90 
 
 
 21-3 
 
 6 
 
 1.75 
 
 2.37 
 
 5.15 
 
 4.25 
 
 6.90 
 
 6.62 
 
 26-1 
 
 6 
 
 0.60 
 
 
 1.45 
 
 
 2.05 
 
 
 26-2 
 
 6 
 
 1.20 
 
 
 2.75 
 
 
 3.95 
 
 
 26-3 
 
 6 
 
 0.40 
 
 0.73 
 
 1.30 
 
 1.83 
 
 1.70 
 
 2.56 
 
1919] Pendleton: A Study of Soil Types 467 
 
 Table 84 — San Joaquin Sandy Loam 
 
 Melilotus indica 
 
 Planted, November 22, 1916. Harvested, June 21, 1917. 
 
 Notes 
 
 
 No. 
 plants 
 
 Sti 
 
 A 
 
 •aw 
 
 Unhull 
 
 ed seed 
 
 A 
 
 Total dry 
 Weight 
 
 matter 
 
 Pot 
 
 r 
 Weight 
 
 Average 
 weight 
 
 r 
 Weight 
 
 Average 
 weight 
 
 Average 
 
 weight 
 
 10-1 
 
 6 
 
 1.20 
 
 
 1.20 
 
 
 2.40 
 
 
 10-2 
 
 6 
 
 1.03 
 
 
 0.92 
 
 
 1.95 
 
 
 10-3 
 
 6 
 
 1.30 
 
 1.18 
 
 1.65 
 
 1.26 
 
 2.95 
 
 2.44 
 
 11-1 
 
 6 
 
 1.05 
 
 
 0.85 
 
 
 1.90 
 
 
 11-2 
 
 6 
 
 0.50 
 
 
 0.35 
 
 
 0.85 
 
 
 11-3 
 
 6 
 
 1.00 
 
 0.85 
 
 0.80 
 
 0.67 
 
 1.80 
 
 1.52 
 
 12-1 
 
 6 
 
 1.07 
 
 
 2.05 
 
 
 3.12 
 
 
 12-2 
 
 6 
 
 1.70 
 
 
 2.45 
 
 
 4.15 
 
 
 12-3 
 
 6 
 
 1.20 
 
 1.33 
 
 1.40 
 
 1.96 
 
 2.60 
 
 3.29 
 
 13-1 
 
 6 
 
 3.05 
 
 
 3.70 
 
 
 6.75 
 
 
 13-2 
 
 6 
 
 3.10 
 
 
 3.95 
 
 
 7.05 
 
 
 13-3 
 
 6 
 
 3.50 
 
 3.22 
 
 4.45 
 
 4.03 
 
 7.95 
 
 7.25 
 
 17-1 
 
 6 
 
 3.05 
 
 
 4.05 
 
 
 7.10 
 
 
 17-2 
 
 6 
 
 2.25 
 
 
 3.55 
 
 
 5.80 
 
 
 17-3 
 
 6 
 
 2.85 
 
 2.72 
 
 3.20 
 
 3.60 
 
 6.05 
 
 6.32 
 
 18-1 
 
 6 
 
 3.25 
 
 
 3.90 
 
 
 7.15 
 
 
 18-2 
 
 6 
 
 2.05 
 
 
 2.65 
 
 
 4.70 
 
 
 18-3 
 
 6 
 
 2.85 
 
 2.42 
 
 3.95 
 
 3.50 
 
 6.80 
 
 6.22 
 
 21-1 
 
 6 
 
 2.50 
 
 
 3.40 
 
 
 5.90 
 
 
 21-2 
 
 6 
 
 2.65 
 
 
 3.95 
 
 
 6.60 
 
 
 21-3 
 
 6 
 
 3.45 
 
 2.87 
 
 3.30 
 
 3.55 
 
 6.75 
 
 6.42 
 
 26-1 
 
 6 
 
 1.10 
 
 
 0.85 
 
 
 1.95 
 
 
 26-2 
 
 6 
 
 0.95 
 
 
 0.85 
 
 
 1.80 
 
 
 26-3 
 
 6 
 
 1.30 
 
 1.12 
 
 1.05 
 
 0.92 
 
 2.35 
 
 2.04 
 
 GENERAL DISCUSSION 
 
 The limited time available for this study made it impossible to 
 make all the determinations upon each of the several horizons of all 
 the soils collected for this study. 
 
 It was believed, however, that the additional data were not re- 
 quired, since that already at hand seemed to give ample evidence upon 
 which to base conclusions. Therefore, in many cases determinations 
 were run on the surface horizon only. This makes some of the tables 
 appear incomplete. 
 
468 University of California Publications in Agricultural Sciences [Vol. 3 
 
 On the basis of the preceding results and discussions some general 
 treatment is possible, as well as a more or less critical discussion of the 
 methods of soil surveying pursued by the Bureau of Soils. 
 
 The types and the localities of collection of the soils studied were 
 as follows : 
 
 Diablo clay adobe: Thalheim (17) 
 
 San Juan Capistrano (1) Madera (18) 
 
 Los Angeles (2) Merced (21) 
 
 Calabasas (5) Del Mar (26) 
 Danville (6) Kan ford fine sandy loam: 
 
 Altamont clay loam Elk Grove (14) 
 
 Walnut (3) Acampo (15) 
 
 San Fernando Valley (4) Woodbridge (16) 
 
 Mission San Jose (7) Waterford (19) 
 
 Sa?i Joaquin sandy loam: Snelling (20) 
 
 North Sacramento (10) Basset (22) 
 
 Lincoln (11) Anaheim (23) 
 
 Wheatland (12) Los Angeles (24) 
 
 Elk Grove (13) Van Nuys (25) 
 
 Note. — Figures following localities designate sample numbers. 
 
 Comparisons of Physical Data 
 
 The mechanical analyses of the soils were carried out with both 
 the Hilgard elutriator and the Bnrean of Soils centrifuge methods. 
 The tedious nature of the elutriator method has been emphasized else- 
 where. The results by this method show that the soils of each type 
 as a whole are somewhat similar, though no two are identical and 
 some samples of a type are widely divergent from the rest. The 
 Bureau of Soils method appears to give a sharper and more satisfac- 
 tory separation into classes than does the elutriator method. This is 
 to be expected since the separates represent greater ranges of particle 
 sizes. As a check on the texture of the samples collected, it shows that 
 some of the soils are not true to name, therefore that all soils mapped 
 under a given type name are not closely similar to one another. Of 
 course, this is the belief of many soil surveyors, but it seems strange 
 that in the present work, where there was the attempt to select soils 
 representative of the class and type chosen for study, that such diver- 
 gences developed. It is an interesting commentary on the personal 
 equation of the field worker, in this case of the writer, who collected 
 the samples. 
 
1919 j Pendleton: A Study of Soil Types 469 
 
 With regard to the methods of mechanical analysis, one should not 
 overlook Mohr's work on The Mechanical Analysis of Soils of Java, 30 
 which gives an excellent discussion of the relative merits of the better 
 known systems of mechanical analysis. He describes a modified cen- 
 trifuge method preferred by him. 
 
 Under a discussion of the physical constants of soils, Free 31 dis- 
 cusses the value of mechanical analysis as a soil constant, and shows 
 that there are three serious errors in the determination, all of which 
 impress themselves upon one making and using such analyses. They 
 are: "(1) disunity of expression; (2) failure to express conditions 
 within the limits of individual groups; and (3) failure to take 
 account of variations in the shapes of the particles." Yet he empha- 
 sizes, and rightly so, i l that mechanical analysis is by no means useless 
 nor to be belittled as a means of soil investigation." 32 
 
 Moisture equivalents. — This determination showed quite distinct 
 averages for the types, though there was considerable variation within 
 each of the types. Eliminating those samples shown to be non-typical 
 according to the mechanical analysis, the variation within the type is 
 reduced considerably. Yet it cannot be said that as regards this con- 
 stant that all soils mapped under a given type name, or even those 
 soils under a given type name which the mechanical analysis has 
 shown to be true to name, have closely similar moisture equivalents. 
 Briggs and McLane 33 express the belief that ultimately moisture 
 equivalent determinations will replace mechanical analysis in the 
 classification of soils, because the determination is simple and the 
 result can be expressed as a single constant. 
 
 Hygroscopic coefficient. — The two heavy types show averages dis- 
 tinct from those of the two light types, but the wide and erratic varia- 
 tion within the type, together with the nearly universal failure of 
 Briggs and Shantz's formula 34 to convert these values into values 
 even approximating those of the moisture equivalent, leads one to 
 doubt the accuracy of these figures of the hygroscopic coefficient. It 
 is because of the ease of determining the moisture equivalent, and 
 because of the difficulties involved in correctly carrying out the hygro- 
 scopic coefficient, that the doubt is cast upon the latter determination. 
 
 so Bull. Dept. of Agr., Indes Neerland, 1910, no. 41, pp. 33. 
 3i Free, E. E., Studies in Soil Physics, Plant World, vol. 14 (1912), nos. 2, 
 5, 7, 8. 
 
 32 ibid., p. 29. 
 
 33 Proc. Amer. Soc. Agron., vol. 2 (1910), pp. 138-47. 
 
 34 U. S. Bur. PI. Ind., Bull. 230 (1912), p. 72. 
 
470 University of California Publications in Agricultural Sciences [Vol. 3 
 
 Comparison of Chemical Data 
 
 The total nitrogen content of the samples of each type varies 
 within somewhat wide limits. The average amounts for the several 
 types are distinct, though the variations are such that some of the 
 quantities of one type overlap those of another type. It is believed 
 that for the types selected the field differentiations do indicate dif- 
 ferences. 
 
 Eegarding the humus content of the four types under considera- 
 tion, the results are somewhat different. The average amounts of 
 humus are almost alike in three of the four types, while the nitrogen- 
 poor San Joaquin soil has an average of about half that of the others. 
 Within the type the soils may be very nearly alike in the humus con- 
 tent, as is the case in two of the types, or may be widely variable, as 
 in the Hanford fine sandy loam. It should be noted that the amount 
 of humus as shown by the method used, is not indicated by the inten- 
 sity of the color either of the soil or of the resulting extract. This 
 confirms the findings of Gortner, which are cited elsewhere. 
 
 There was quite a wide range shown in the results of the deter- 
 mination of the loss on ignition. The Diablo and Altamont soils, be- 
 cause of the heavier textures and the relatively large amounts of com- 
 bined water, and of considerable amounts of CaC0 3 in at least one 
 case, gave high losses on ignition. The averages were close, 6.8% for 
 the Diablo, and 6.7% for the Altamont. The Hanford soils were 
 lower, though with a wider range. Soil no. 14, with 6.9% loss on igni- 
 tion, shows almost double that of any other soil in the type. The San 
 Joaquin soils, with an average of 2.6%, show the lowest average loss 
 on ignition. The smaller amounts of organic matter in these soils is 
 one reason for the smaller loss. The two heavier types have averages 
 close together, and the lighter types have averages not far apart, but 
 because of the wide variations within each type, the results of the 
 determination of the loss on ignition certainly do not show that all 
 soils classified in one type are closely similar. 
 
 Hall and Russell, in their discussion of the soils of southeastern 
 
 England, 35 consider of value the ratio of Q-. — — : A — but apply- 
 
 % loss on ignition, 
 
 ing this ratio to the California soils under consideration does not seem 
 
 to give any relations of value. The Diablo ratio varies from 0.0136 to 
 
 0.0158, the Altamont from 0.0141 to 0.0204, the San Joaquin from 
 
 0.0144 to 0.0232, and the Hanford from 0.011 to 0.0172. 
 
 85 Jour. Agr. Sci., vol. 4 (11)11), pp. 182-223. 
 
1919] Pendleton: A Study of Soil Types 471 
 
 The calcium (as CaO) content of the soils is interesting especially 
 because of the variability. The Altamont samples show the greatest 
 variation, for the largest quantity of CaO is about seven times the 
 smallest. The San Joaquin samples are second, with the largest over 
 six times the smallest. The Diablo samples are third, with the largest 
 over five times the smallest, while the Hanford soils show the least 
 variation, the largest being less than twice the smallest. There are 
 quite marked differences between the averages of the Diablo, Alta- 
 mont, and Hanford soils (the San Joaquin samples are intermediate), 
 but the wide variations within the types greatly minimize any sig- 
 nificance the averages might have. Hence it is not possible to state 
 that one or another type, as represented by these samples, is charac- 
 terized by high, low, or moderate amounts of calcium. 
 
 As the analyses of the samples for calcium failed to point out any 
 striking characteristics, unless it be that of variability, so it is with 
 magnesium. Magnesium (as MgO) is variable within each of the four 
 types. The largest quantity is about three times the smallest in the 
 Diablo, San Joaquin, and Hanford types, while in the Altamont the 
 largest is twenty-seven times the smallest. Considering the Hanford 
 and San Joaquin, or the Diablo and San Joaquin, it is seen that the 
 curves do not overlap, while the Diablo and Altamont, or the Diablo 
 and Hanford curves do. The averages of the four types are distinct, 
 except between the Hanford and Diablo, which are quite close. But, 
 here again, because of the more or less wide range of values within 
 each of the types, the averages are of little significance. The lime- 
 magnesia ratio is very variable in these soils. Comparing the calcium 
 and magnesium curves for the several soils gives a good idea of the 
 relations. The Diablo curves are quite similar except for soil no. 6, 
 which shows 3% MgO and 0.5% CaO. In the Altamont soils the 
 curves are somewhat similar in direction, though the ratios differ 
 widely. In the Hanford and San Joaquin types the ratios of CaO and 
 MgO are also far from constant, yet it is readily seen from the graphs 
 that the amount of magnesium varies more or less directly with the 
 amount of calcium. 
 
 Respecting the total phosphorus (as P 2 5 ), if the San Joaquin and 
 Hanford samples alone be considered, there would be no doubt as to 
 the significance of the field separation, the variations within the type 
 notwithstanding. But when the other two types are considered, the 
 case is not so good in favor of the field classification. The Diablo soils 
 show considerable variation in the amount of P r ,0 2 , while the three 
 
472 University of California Publications in Agricultural Sciences [Vol. 3 
 
 Altamont samples show much variation. Therefore with reference to 
 the amount of phosphorus, and the types studied, the separation into 
 types may or may not be of significance. 
 
 If the results of the potassium (K 2 0) determinations are com- 
 pared, it is very evident that but one conclusion can be drawn, and 
 that is that the variations in the amount of potassium within each 
 type are great enough so that any differences between the averages 
 of the several types have no significance whatsoever. Therefore, with 
 regard to total potassium the field separation of soils as represented 
 by these twenty-four samples of four types means nothing. 
 
 Comparison of Bacteriological Data 
 
 The wealth of the data obtained from over nine hundred bacteri- 
 ological tumbler cultures is hardly of sufficient significance to com- 
 pensate for the effort involved. There is one outstanding conclusion 
 from all this work, namely, the lack of any very definite, distinct, and 
 constant bacteriological activity of the samples of one type that is not 
 to a considerable extent shared by the samples of the other types. 
 There are tendencies in certain types with regard to bacteriological 
 activity which show that some of the types as a whole are more or less 
 distinct from one or more of the others. 
 
 Ammonification. — The amount of ammonia produced from dried 
 blood varies to a great extent. The Altamont samples gave between 
 10 and 33 mg. nitrogen as ammonia; the Diablo samples gave between 
 7 and 26 mg., and the Hanford samples gave between 35 and 72 mg. 
 The Altamont and Diablo types are thus seen to be about alike in their 
 low ammonifying power, as compared with the higher ability of the 
 San Joaquin types and still greater ability of the Hanford types. 
 And since there are somewhat greater variations between the types 
 than between the samples of a given type, the ammonifying power 
 may be significant. 
 
 Nitrogen fixation. — The two heavy types, Diablo clay adobe and 
 Altamont clay loam, show no characteristic differences, while the two 
 lighter types show considerable differences. As a whole the types are 
 different one from another, yet the variations within the type are 
 sufficient to prevent any statement that the rate of nitrogen fixation 
 is a function of the type as determined in the field, or vice versa. 
 
 Nitrification. — The nitrification data are the most puzzling. The 
 figures are extremely variable within a given type ; the erratic way 
 
1919] Pendleton: A Study of Soil Types 473 
 
 in which the Hanford samples behave is not paralleled by any other 
 type. There are certain ways in which the types are distinct : 
 
 The nitrification of the soil's own nitrogen as compared with the 
 soil's action upon added nitrogen is in some degree separate for each 
 type. The San Joaquin samples nitrified their own nitrogen to a 
 greater degree than they did the nitrogen added to the soil. 
 
 The relative nitrification of the several nitrogenous materials 
 (dried blood, cottonseed meal, ammonium sulfate) is in some measure 
 distinct for the several types. The Diablo, Altamont, and San Joaquin 
 types show ammonium sulphate to be nitrified the best, cottonseed meal 
 less, and dried blood still less. The Hanford samples show cottonseed 
 meal to give the highest percentage of nitrates, with dried blood less, 
 and ammonium sulfate still less. 
 
 When any one soil is compared through the three sets of deter- 
 minations there are no apparent similarities. The Hanford type 
 shows the greatest bacterial activity, while the San Joaquin shows 
 less, with the heavier types showing sometimes greater activity and 
 sometimes less than that of the San Joaquin. 
 
 Work in Other States 
 
 In connection with the original chemical work reported in this 
 paper, there should be mentioned the large amount of work done in a 
 number of states on the analysis of the types of soils as mapped by 
 the Bureau of Soils. Apparently, these analyses have been made 
 without any question as to the validity of the. existing subdivisions 
 into types. The various analyses have been reported with some com- 
 ment, but that which does appear usually deals with the "adequacy" 
 or " inadequac3 T " of the plant food present. Blair and Jennings 36 
 present a large amount of data on chemical composition, some of 
 which on rearrangement show interesting relationships (table 85). 
 From the data the four series of soils with the largest number of 
 analyses were selected (see following table). Under each series there 
 are from 2 to 4 soil tj^pes, and from 2 to 6 analyses under each type. 
 The averages from each type are tabulated, also the averages of all 
 the types within the series. This is both for the strong acid extraction 
 and the fusion methods of analysis for significant plant food elements. 
 There are no doubts but that each series of soils shows characteristic 
 chemical peculiarities, peculiarities which are to a great extent con- 
 
 36 The Mechanical and Chemical Composition of the Soils of the Sussex Area, 
 New Jersey, Geol. Surv. N. J., Bull. 10, 1910. 
 
474 
 
 University of California Publications in Agricultural Sciences [Vol.3 
 
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1919] Pendleton: A Study of Soil Types 475 
 
 stant throughout the several representatives of the type. In some 
 cases, the differences or similarities are more clearly seen in the total 
 analyses, and in other cases, they appear in the acid analyses and not 
 in the fusion analyses. Within any series the variations between 
 analyses of any one type are about the same as the variations from 
 type to type. There are many other papers 37 which provide material 
 for similar comparisons. 
 
 A paper by Van Dyne and Ashton 38 reports chemical analyses for 
 lime, phosphoric acid, potash, and nitrogen on the samples collected 
 in the course of the survey of Stevens County, Washington. Though 
 sometimes there is a much greater range within a type than between 
 types, in a general way the analyses for any one type agree quite 
 well. As a whole the chemical analyses seem to show that the field 
 criteria are also a basis for grouping soils into certain chemical 
 groups. It should be mentioned that the work of Blair and Jennings, 
 also that of Van Dyne and Ashton, deals with individual areas, and 
 not with samples from several scattered areas. The work of Fraps and 
 Williams, and the original work here reported represent scattered 
 areas. 
 
 The Greenhouse Cultures 
 
 By far the most interesting results were obtained in the pot culture 
 work. It is realized that there are variations in the physical nature 
 of the samples of a given type, yet since these samples were collected 
 with considerable care by one familiar with field classifications, the 
 samples so selected should be fairly representative of the type. It is 
 probable that if all the soils in each of the types used were exactly the 
 same in texture, i.e., if the mechanical analysis showed the same 
 results for the several soils, the crops produced on the several soils of 
 a type would be less divergent in appearance or weight. Yet it is 
 not at all likely that the crops would be the same. Pot cultures pre- 
 sume that the conditions in all the pots can be kept uniform, but this 
 is obviously impossible. Greenhouse work is subject to many interfer- 
 ing factors. Nevertheless, the results are believed to be significant, 
 
 37 Williams, and others, Eeport on the Piedmont Soils, North Carolina Dept. 
 Agr., Bull. 206, 1915. 
 
 Fraps, G. S., Composition of the Soils of South Texas, Texas Agr. Exp. Sta., 
 Bull. 161, 1913; Composition of the Soils of the Texas Panhandle, ibid., Bull. 
 173, 1915. 
 
 38 Van Dyne and Ashton, Soil Survey of Stevens County, Washington, Field 
 Operations, U. S. Bur. Soils, 1913, pp. 2165-2295. 
 
476 University of California Publications in Agricultural Sciences [Vol.3 
 
 despite the large correction that the consideration of the probable 
 error might introduce. 
 
 The differences in the crop producing power of the soils are very 
 marked in the Diablo clay adobe, where the second crop, as well as 
 the first, shows evident variations in the ability to support a crop. 
 In the Altamont clay loam the second crop almost loses the variations 
 seen in the first crop from pot to pot. The samples of both types 
 seem to show one thing in common — the approach of the several sam- 
 ples toward a uniform ability to produce crops, as the soils are kept 
 for longer periods under the same conditions. The Hanford soils did 
 not show, with the several crops, the parallelism in the fertility from 
 crop to crop as did the Diablo and Altamont soils. Some soils pro- 
 duced good crops of grain and poorer crops of legumes, others did the 
 opposite. The low nitrogen content in this type seemed to be a limit- 
 ing factor. This would account for the variation between the grain 
 and the leguminous crops. Also, the presence, or absence of Bacillus 
 radicuola inoculation in this connection might greatly affect the total 
 crop produced. 
 
 There does not seem to be much doubt but that the soils of the 
 several types compared in this way are not the same, though they are 
 in certain respects similar. 
 
 The Place of Soil Classification. — With all these evidences that the 
 soils within the several types are not closely similar, though they are 
 classified the same by the Bureau of Soils, what conclusion is one to 
 reach as to the value of such a classification ? If it were true that there 
 were no appeal from the findings of such laboratory and greenhouse 
 <l<-1<'rminations as these, and that these determinations were a final 
 proof of the fertility or infertility of a soil, obviously there would be 
 but one thing to do — discard all such field classifications as useless. 
 But the writer is one of a great many soilists who are not willing to 
 rely on laboratory or even greenhouse results for an absolute deter- 
 mination of fertility, and for the grouping together of soils into a 
 workable classification. Not enough is definitely known as to the mean- 
 ing of such findings, though there are certainly many valuable points 
 shown by laboratory analyses. 89 
 
 As examples of the value of natural classifications we may con- 
 sider those of botany, /oology, or mineralogy. If available, a wholly 
 satisfactory classification of soils would be equally useful. The appre- 
 
 89 Jordan, W. H., Measurements of Soil Fertility, New York Agr. Exp. Sta. 
 Geneva', Bull. 424, L916. 
 
1919] Pendleton: A Study of Soil Types 477 
 
 ciation of this is shown in the many systems of soil classification that 
 have been proposed. 
 
 Despite the foregoing facts that have been obtained showing the 
 divergent properties of different samples of one type presumabi}' 
 alike, yet it must be admitted that soil surveys, even such as are no 
 more refined than those of the Bureau of Soils, have considerable 
 value for field use. 
 
 It is felt that the additional effort required to modify the practices 
 of the Bureau of Soils in the mapping and classifying of soils would 
 be more than justified by the increased accuracy and usefulness of 
 the maps. To point out some of the causes of the present practices 
 and to give suggestions for possible methods of improvement, the 
 following discussion of the Bureau of Soils methods has been 
 prepared. 
 
 Discussion of the Bureau of Soils' methods. — The methods of map- 
 ping and classifying soils, as devised and used by the Bureau, have 
 resulted from some definite and important considerations. 
 
 1. The necessity for keeping down the cost of surveying and map- 
 ping prevents the use of laboratory and culture methods in the study 
 of the soils classified, even if it were not for the fact that one of the 
 outstanding policies of the Bureau apparently denies the validity of 
 such studies in the classification of soils. This does not include the 
 mechanical analysis of soils, which is not a separate laboratory deter- 
 mination, but a method of checking the field man's decision as to the 
 texture. It should also be added that some of the reports as published 
 in the Field Operations of the Bureau of Soils, for 1913, show the 
 subdivision of the soils into two groups based upon the CaC0 8 content. 
 Keeping down the cost has also prevented the use of sufficient time to 
 map the soils correctly, even according to the criteria admittedly of 
 value in the system adopted. Many of the other methods of classify- 
 ing and mapping soils, even if applicable to most of the agricultural 
 regions of the United States, would be absolutely out of the question 
 on account of cost. 
 
 2. The large and widely diversified area of the United States, and 
 the attempt to map representative areas in various parts of the coun- 
 try, early led to difficulties. There seemed to be a lack of understand- 
 ing as to what criteria to use in the classification of the soils. Re- 
 cently, some of the areas first mapped in the state of California have 
 been resurveyed. The texture, series, and province differences of the 
 early mapping seem not to have been clear. For example, we may con- 
 
478 University of California Publications in Agricultural Sciences [Vol.3 
 
 sider the differences between the older and the recent survey of two 
 localities east of Los Angeles. The notes were made by C. J. Zinn, 
 a member of the party which made the recent survey : 
 
 Locality A — About 15 square miles with Eaton Wash on the west, center of 
 Monrovia on the east, mountains on the north, and a line about 3 miles south of 
 mountains as the south boundary. The old survey^ has four types of three series 
 and two miscellaneous types: San Gabriel gravelly loam, San Gabriel gravelly 
 sand, Placentia sandy loam, San Joaquin black adobe, and Eiverwash and Moun- 
 tains. The new survey (1915, unpublished) has 13 types of 6 series and 3 mis- 
 cellaneous types: Hanford stony sand, gravelly sand, loam, sandy loam, fine 
 sandy loam, and sand; Tejunga stony sand; Zelzah loam and stony loam; Pla- 
 centia loam, Holland loam, Chino loam and silt loam. The miscellaneous types 
 are Eough Mountain land, Eough Broken land, and Eiverwash. 
 
 Locality B — In the city of Pasadena, comprising about 3.5 square miles, with 
 the southwest corner at the center of the city. The old survey 41 shows San 
 Gabriel loam occuping about 0.6 of the area, San Gabriel gravelly sand about 0.3, 
 and Placentia sandy loam about 0.1. The new survey (1915, unpublished) shows 
 Zelzah gravelly loam occupying about 0.9 of the area, Zelzah loam about 0.1, with 
 a very small body of Holland loam. The older survey showed a recent alluvial 
 soil where the recent one shows an old valley filling soil. 
 
 Besides these errors (detected as such by the practical man, who 
 might attempt to use the soil maps in the field) there are in addition 
 those of another nature which were the source of much criticism in the 
 earlier history of the survey — the so-called "procrustean classification" 
 criticism of Hilgard. 42 Due apparently to an insufficient study of the 
 soils of the United States, there was the attempt to classify in the same 
 series soils of widely differing properties — differences of an important 
 nature being ignored. 
 
 At the present time there is an increasing tendency toward limit- 
 ing series groups of soils to a more or less definite climatological 
 region. In this connection see the later changes in the correlation of 
 many soils. 43 These changes tend to limit the geographic range of the 
 series, and make these series narrower and more exact. Moreover, it 
 is understood that as the knowledge of the soils has increased, the 
 changes in correlation have been proceeding rapidly since the above 
 list was issued. This indicates that as the facts accumulate the "pro- 
 erustean classification" criticism is losing its force. 
 
 40 Field Operations of the U. S. Bur. of Soils, 1901, San Gabriel sheet. 
 
 4i Ibid. 
 
 « Hilgard, E. W., arid Loughridge, R. H., Proc. Second Intern. Agrogeol. 
 Conf., Stockholm, 1910, pp. 228-29; Hilgard, E. W., U. S. Office Exp. Sta., Bull. 
 142 (1904), p. 119; Hilgard, E. W., Proc. First Intern. Agrogeol. Conf., Budapest, 
 1909, y.p. 52-54. 
 
 M II. S. Bur. Soils, Bull. 90, 1913. 
 
1919] Pendleton: A Study of Soil Types 479 
 
 3. There was a lack of trained men early in the work. This was 
 to be expected. As has been shown, the early surveys were very crude 
 in certain places. It must be added that some of the errors and omis- 
 sions made in the more recent maps are not due to a lack of training, 
 but to the carelessness of the field men with respect to details. 
 
 4. The policy of the Bureau has been to recognize the physical 
 characteristics of the soil as factors in fertility to the virtual exclusion 
 of the chemical or biological factors. Therefore the use of physical 
 criteria is necessary. Besides, the criteria must be such as can be 
 applied in the field, and are: "(1) color, (2) texture, determined by 
 rubbing between the thumb and finger, (3) structure, (4) nature of 
 subsoil, (5) presence of hardpan, (6) height of water table, (7) pres- 
 ence of alkali, (8) topography, (9) physiographic form and hence 
 mode of formation, and (10) source of material (sedimentary, igne- 
 ous, or metamorphic rocks). Humus, and the presence or absence of 
 appreciable quantities of lime, also the reaction of the soil (acid or 
 alkaline) are frequently guessed at. These criteria are practically 
 the only ones that can be applied in field work. It is believed that 
 these same criteria indicate the chemical nature of the soil, though 
 there has been no attempt to correlate some of the factors. However, 
 the original work reported in this paper would indicate that the chem- 
 ical nature is not the same, of soils classified the same by the Bureau 
 of Soils criteria. 
 
 5. The desire to limit the number of groups of soils is a wholly 
 sound one. In discussing the problems of classifying soils there 
 should always be kept in mind the fact that some of the problems are 
 not very different, fundamentally, from some of the problems that 
 have been causing perplexity among biologists for a long while. 
 The tendency, as seen in some of the recent surveys, to make the 
 series more inclusive and to introduce the term, phase, is heartily 
 commended. By making the series broader there will be less difficulty 
 in placing a soil in its proper group. The phase will take care of many 
 of the series differences between area and area. 
 
 6. It seems certain that if there were more emphasis placed upon 
 the inspection of the area, during the progress of the field work and 
 after its completion, there would be a much closer approach to 
 accuracy throughout the map and report. At the present time the 
 field man is not closely checked up. The careless or indifferent worker 
 can map more or less as he pleases, especially in the out-of-the-way 
 places. 
 
480 University of California Publications in Agricultural Sciences [Vol. 3 
 
 7. Whether the soil survey should include more than a simple 
 classification of the soils or not, is an unsettled question. It is thought 
 hardly possible that in a soil survey the field man could handle all the 
 phases of an agricultural survey of an area, when his energies should 
 be fully employed in the classification of the soils. It is believed that 
 the place of the survey, in this country at least, is to handle the 
 classification of the soils, leaving the study of the remaining factors 
 largely to other specialists, who would use the soil survey as a basis. 44 
 But to make the soil maps of more general use for such work, they 
 must be more accurate. These maps never can become the basis of 
 other agricultural studies as long as many experiment station workers 
 ridicule them. Hence, the ultimate effort of the survey should be 
 toward better work, rather than covering a wide range of agricultural 
 studies. 
 
 8. There is not the incentive to make as many separations of the 
 soils in the field, as the field man might think best, because frequently 
 the feeling of the editors is that there would be too many small bodies 
 of soil shown on the manuscript maps which would not warrant the 
 additional cost of publication. 
 
 In conclusion, the Bureau of Soils' system has much to commend 
 it as a field method, and the resulting maps and classification are be- 
 lieved to be of distinct value. It is felt that a more general under- 
 standing of: (1) the limitations under which the maps, the earlier 
 ones especially, have been made; (2) the difficulties under which the 
 field work is at present carried on; (3) the meaning of the correlation 
 of soils; and (4) the general policy of the Bureau of Soils would give 
 people more sympathy with their work. 
 
 44Fippin, E. O., Proc. Amer. Soc. Agron., vol. 1 (1908), pp. 191-97. 
 
1919] Pendleton: A Study of Soil Types 481 
 
 SUMMARY 
 
 Presumably typical samples of four soil types were collected for 
 laboratory and greenhouse study from widely distributed localities in 
 the state of California. The field appearance of each sample was 
 usually sufficient to warrant the classification as it exists. 
 
 Physical Relations 
 
 1. The mechanical analysis by the Hilgard elutriator shows that 
 the soils of a given type are in some cases quite divergent from each 
 other in their content of certain of the sizes of particles. The mechan- 
 ical analysis by the Bureau of Soils method shows that 6 of the 24 
 soils were not true to their type names, and that of those soils within 
 the type there is considerable variation. 
 
 2. The moisture equivalents for the several types show distinct 
 enough values to substantiate the field separation. 
 
 3. The hygroscopic coefficients vary widely within each type and 
 the types are not shown to be distinctly different by this criterion. 
 
 Chemical Relations 
 
 1. The total nitrogen averages vary markedly from type to type, 
 with the Altamont clay loam containing three times that in the San 
 Joaquin sandy loam. 
 
 2. The average humus content of the San Joaquin samples is 
 about half that of the other types. The variations in the humus con- 
 tent between the types are small, considering the diverse nature of the 
 types and the large range in the amount of humus within the type. 
 
 3. The loss on ignition shows a considerable variation within the 
 type and no significant distinction between the four types. 
 
 4. The average total calcium content of the types is distinct, 
 though the wide range within each type minimizes the significance of 
 the variation in the averages. 
 
 5. With regard to magnesium, the types are neither distinct nor 
 are the soils within the type closely similar. 
 
 6. The average phosphorus content of the types is distinct, though 
 the ranges within the several types frequently overlap. 
 
 7. The total potassium results do not show the types to be distinct 
 nor the soils within a type closely similar. 
 
482 University of California Publications in Agricultural Sciences [Vol. 3 
 
 Bacteriological Relations 
 
 1. The ammonifying power shows rather larger variations from 
 type to type than between the samples of a type. 
 
 2. The nitrogen fixation data do not show characteristic differences 
 for the several types. 
 
 3. Regarding nitrification as a whole there may be a greater 
 divergence between the samples of a type than between types. The 
 relative nitrification of the soil's own nitrogen varies with the type, 
 as does the relative nitrification of the several nitrogenous materials 
 added. 
 
 Pot Cultures in the Greenhouse 
 
 In addition to the effect of the probable error, the impossibility 
 under the conditions herein described of growing the same crops on 
 all the soils, during the same season of the year in the greenhouse, 
 prevents close comparisons between the types, or between the first and 
 second crops on a given soil. The comparison of several samples of a 
 given soil type and the comparisons of various soil types, according 
 to the previously outlined greenhouse methods show that : 
 
 1. Different representatives of a given type are not the same in 
 their ability to produce crops. 
 
 2. The arrangement of the samples of a given type according to 
 their fertility may or may not vary with the special crops used as the 
 indicators. 
 
 3. The types are distinct with respect to their fertility, considering 
 their average production. 
 
 Therefore it is concluded that with regard to the 24 soils of 4 
 types examined, all soils mapped under a given name by the Bureau 
 of Soils method may or may not be closely similar, depending upon 
 the criteria used. The greater number of the criteria show the soils 
 of a type to be not closely similar, and the types to be but litle differ- 
 entiated from each other. 
 
 In connection with the results of the author's study of the soils, 
 there is given an historical sketch of the development of soil classifica- 
 tion and mapping, also a discussion of certain of the methods em- 
 ployed by the Bureau of Soils of the United States Department of 
 Agriculture. It is pointed out that despite its defects, the work of 
 the Bureau of Soils is of value, and is practically the only type of soil 
 classification and mapping possible under the conditions imposed. 
 
1919] Pendleton: A Studij of Soil Types 483 
 
 APPENDIX A 
 METHODS AND TECHNIQUE 
 
 Collection of Samples 
 
 There was difficulty in finding types that would meet the requirements of wide 
 distribution and of differing from one another as to series as well as texture. The 
 types chosen were: 
 
 Diablo clay adobe, a residual soil. 
 
 Altamont clay loam, a residual soil. 
 
 San Joaquin sandy loam, an "old valley filling" (old alluvial soil). 
 
 Hanford fine sandy loam, a recent alluvial soil. 
 
 The first task was the collection of the samples of soil for study in the labora- 
 tory and in the greenhouse. Of course, there were kept in mind the errors and 
 difficulties involved in the collection of representative samples. The selection of 
 the localities in which to collect samples was frequently made in consultation with 
 the persons who had originally mapped the areas under the Bureau of Soils. 
 This was done so that the soil chosen might as nearly as possible represent what 
 the surveyor had in mind as characteristic of the type within the area. It was to 
 be expected that the ideal type which one man would use as a guide as he did the 
 mapping in one area would not always be identical with that which another man 
 might use in mapping another area, despite the aid of the inspector in keeping the 
 ideal types of the field men as nearly alike as possible. Some of the accompanying 
 index maps, showing the places where the soil samples were collected, are dupli- 
 cates of the same locality. As the dates show, one is a portion of a less recent, 
 and the other of a more recent survey. In many cases the index maps have been 
 copied from the manuscript maps, a number of surveys in this state not yet being 
 published. For a discussion of the differences in these maps, see below the section 
 on The Criticism of the U. S. Bureau of Soils Method of Surveying. 
 
 Not only were the field men questioned about the locality, but as nearly as 
 possible an exact designation was obtained on the soil map itself. In the collec- 
 tion of some of the samples the writer had the good fortune to have the assistance 
 of the man or men who actually mapped the soils in question. Sometimes there 
 was no trouble at all in locating a typical body of the soil where a sample might 
 be taken. On the other hand, as in the case of the collection of the Hanford fine 
 sandy loam from Woodbridge (nos. 15 and 16), more than two hours were spent 
 in driving about, trying to find a place that seemed a typical fine sandy loam. 
 Experience shows that the personal equation in field work is very important and 
 is hard to control. 45 
 
 No special attempt was made to obtain virgin soil, for the types of soils that 
 had been selected for study were mainly agricultural, and most of the soils have 
 been at some time under cultivation, if they are not now. Also, there has been 
 little, if any modification of the agricultural soils by the addition of fertilizers. 
 Hence the small tracts of the Hanford fine sandy loam, for instance, that are still 
 virgin are largely non-agricultural, waste land areas, and would not illustrate the 
 properties of the type as a whole. Not so large a part of the San Joaquin sandy 
 loam is under cultivation now, though almost all of it has been farmed to grain 
 in the past. The two minor types studied, the Altamont clay loam and the Diablo 
 clay adobe, being of residual origin and occupying rolling to hilly or mountainous 
 land are also not very extensively farmed. The topography is the limiting factor 
 in most cases. 
 
 45 Fippin, E. O.. Practical Classification of Soils, Proc. Amer. Soc. Agron., vol. 3 (1911), 
 pp. 76-89 ; Increasing the Practical Efficiency of Soil Surveys, Proc. Amer. Soc. Agron., 
 vol. 1 (1907-1909), pp. 204-06. 
 
484 University of California Publications in Agricultural Sciences [Vol.3 
 
 The ideal way to collect a representative sample of soil for laboratory studies 
 is to make a number of borings scattered about the field or fields, so that the sam- 
 ple will approximate an average. But in the case of collecting the samples for this 
 study it was considered best not to attempt such a procedure, for the reason that 
 it was desired to have the samples for the greenhouse work and for the physical, 
 chemical, and bacteriological studies, come from the same lot of soil. The collec- 
 tion of such a large amount of soil, about 250 pounds in all, from a number of 
 places about the selected field would be very tedious. Hence as nearly a typical 
 place as possible Avas selected, close to a wagon road, in order that the samples 
 could be transported readily. Care was used that the location be far enough out 
 into the field to allow the sample to be representative of the conditions in the field. 
 
 The subsequent procedure was as follows: The selected spot was cleared of 
 grass or other surface material or accumulation that did not belong to the soil. 
 A hole was dug, usually one foot deep (the depth depending entirely upon the 
 nature of the surface soil and any noticeable changes toward the subsoil), and 
 big enough to give sufficient soil to make up the greenhouse sample of from 225 
 to 250 pounds. The soil was shoveled directly into tight sugar or grain sacks, no 
 attempt being made to mix the sample at this time. Some sacks of the soil would 
 contain more of the surface material, and others more of the lower portion, but a 
 later thorough mixing and screening at the greenhouse gave a uniform sample. 
 After the large sample was collected, the hole was usually dug two feet deeper, 
 giving a hole three feet deep. One side of this hole was made perpendicular, and 
 from this side the small samples were collected. The A, B, and C horizons were 
 marked off on this wall, and the samples collected by digging down a uniform 
 section of the designated portion, using a geologic pick and catching the loosened 
 material on a shovel. About ten pounds of soil were so collected, and placed in 
 clean, sterile canvas sample sacks. Care was used not to contaminate the samples, 
 so that the bacterial flora might remain nearly unaltered. It seemed imprac- 
 ticable to attempt to collect the laboratory sample under absolute sterile condi- 
 tions, especially since some of the deeper (B and C) samples were obtained by 
 means of the soil auger. When the auger was used to collect the samples from 
 greater depths the boring was done from the bottom of the hole made in collect- 
 ing the larger sample. The size of the laboratory sample required the boring of 
 five or six holes with the usual 1.5 inch soil auger. The laboratory sample of the 
 first foot, or the A sample, was always collected from the side of the large hole. 
 Notes regarding the sample, field condition, the place of collection, together with 
 photographs and marked maps are given in appendix B. 
 
 As described above, the soils were collected in separate portions from the sur- 
 face to the 12 inch, from the 12 to 24 inch depth, and from the 24 to 36 inch 
 depths where there were no abrupt or marked changes in the color, texture, or the 
 like, as in the Hanford fine sandy loam. But since in some cases, as most fre- 
 quently in the San Joaquin sandy loam, the samples do not represent the first, 
 second, or third foot depths, as the case might be, the term, horizon, has been 
 used. Horizon A indicates the surface sample, horizon B the second sample, and 
 horizon C the third sample. 
 
 Laboratory Preparation of Samples 
 
 The large samples were stored in the greenhouse until ready for use. The lab- 
 oratory samples were allowed to remain in the sacks until air dry, when they were 
 passed through a 2 mm. screen. This was a difficult matter, with the heavy soils, 
 as well as with the heavy subsoils of the San Joaquin sandy loam. Cautious use 
 
1919 J Pendleton: A Study of Soil Types 485 
 
 of the iron mortar "was necessary to supplement the rubber pestle. 40 The samples 
 were thoroughly mixed after screening, when they were weighed and placed in 
 sterile containers — glass jars and large bottles. Precautions were taken as far 
 as possible to avoid contamination of the samples during this preparatory process. 
 The screens, mortars, scoop, and pans were flamed out between samples. Obvi- 
 ously contamination could not be avoided absolutely without too great a prolonga- 
 tion of the work. 
 
 The material not passing the 2 mm. screen was subsequently washed on the 
 screen, with a stream of water to remove the finer material. The residue not 
 passing the screen by this treatment was dried and weighed. It seemed unneces- 
 sary to adopt elaborate precautions, like those described by Mohr, 47 to obtain the 
 exact quantities. 
 
 Mechanical Analysis 
 
 The Hilgard elutriator was used for the purpose of making the mechanical 
 analysis of the samples (surface horizon only). For the purpose of this work 
 the method described by Hilgard 48 has been modified in several respects. The pre- 
 liminary preparation by sifting through the 2 mm. sieve in the dry state, and 
 through the 0.5 mm. sieve by the aid of water was used. One hundred grams was 
 sifted with the 0.5 mm. sieve, and the fine material plus the water was evaporated 
 to dryness on the water bath. The dry material was broken up and from this 
 the samples were weighed out for the analysis. 
 
 The samples were not disintegrated by boiling, since it was believed that such 
 treatment would affect the "colloid" content of the sample. Instead, the samples 
 were shaken with water in sterilizer bottles for three hours, similar to the treat- 
 ment preparatory to the mechanical analysis by the Bureau of Soils method. 
 However, not boiling the samples caused more work later. 
 
 The colloidal clay was removed by placing the previously shaken sample in a 
 large precipitating jar and stirring up with several liters of distilled water. (Dis- 
 tilled water was used throughout the analysis.) The quantity of water was not 
 important, but rather the depth of the suspension, which was 200 mm. After 
 allowing to stand for 24 hours the supernatant turbid water was siphoned off, 
 when the residue in the bottom of the jar was again stirred up with water and 
 the clay again allowed to settle out of a 200 mm. column. This was repeated 
 until the supernatant liquid contained practically no material in suspension after 
 standing for 24 hours. The clay suspensions were placed in large enamelware 
 preserving kettles, and the solutions reduced in volume by boiling. The final 
 evaporations were carried on over the water bath, so as to avoid too high a tem- 
 perature. 
 
 A large portion of the finest sediment (0.25 mm. hydraulic value) was removed 
 as follows : After the greatest portion of the clay had been removed by the 24 
 hour sedimentation and decantation, the sample was placed in a 1 liter beaker and 
 stirred up with sufficient water to make a 100 mm. column. After standing 6 
 to 8 minutes the suspended material was decanted off. This was repeated until 
 the supernatant solution was practically clear. The entire time for these decanta- 
 tions usually occupied 2.5 or 3 hours. The decanted material was allowed to stand 
 for 24 hours, as before, and the 200 mm. column decanted as with the original 
 clay suspension. This was continued until the clay was practically all removed. 
 
 46 Hilgard, Calif. Agri. Exp. Sta., Circ. 6, June, 1903. 
 
 47 Bull. Dept. Agr. Indes Neerland., no. 41, 1910. 
 
 48 Calif. Agr. Exp. Sta., Circ. 6 (1903), pp. 6-15; see also Wiley, Agricultural Analysis, 
 vol. 1 (1906), pp. 246-62. 
 
486 University of California Publications in Agricultural Sciences [Vol. 3 
 
 The residue constituted the main portion of the 0.25 mm. hydraulic value sep- 
 arate. The residue from the 6 to 8 minute decantation was placed in the elutri- 
 ator, and separated by the usual method into the various sizes. Since, however, 
 the sample was not prepared by boiling previous to the separation of the clay, the 
 clay was never as thoroughly removed from the coarser particles and the finer 
 aggregate particles were not completely broken down. Hence when the sample 
 was placed in the elutriator and subjected to the violent agitation of the stirrer 
 an appreciable amount of clay passed off with the finest separate. Therefore, 
 instead of allowing the water to return to the carboy from the settling bottle, 
 during the running off of the finest separate, the following procedure was em- 
 ployed: The water was run into precipitating jars and allowed to stand for 24 
 hours, and the clay water was then decanted off and boiled down with the other 
 clay water. 
 
 A further modification of the Hilgard method was found advisable after the 
 change from the large elutriator tube to the small one, preparatory to running off 
 the coarser separates. The mechanical defects in the elutriator always allowed 
 for the collection of a portion of the sample in crevices where the stream of water 
 could not reach to carry off the particles. Hence, when the large tube was 
 removed, and cleaned, there was found an appreciable amount of the finer sedi- 
 ments that had not passed over. These were all added to the small tube of the 
 elutriator, and the additional material of the smaller sizes run off, using an hour 
 or so for each size. This seemed a better method than the separation of such 
 sediments by the beaker method, as was done by Dr. Loughridge. 
 
 The separates, after decanting most of the water, were dried first on the water 
 bath and later in the drying oven at 100°C-110°C and weighed. All of the deter- 
 minations were made on the water free basis. 49 
 
 Additional Physical Determinations 
 
 Upon the surface or A horizon samples of the 24 soils considered in this study 
 additional physical determinations were made by the Division of Soil Technology, 
 through the courtesy of Professor Charles F. Shaw. These determinations were 
 of the mechanical analysis by the Bureau of Soils method, 50 of the moisture equiva- 
 lent by the Briggs and McLane method, 51 and of the hygroscopic coefficient accord- 
 ing to Hilgard 's method. 52 
 
 Chemical Methods 
 
 At first the chemical work was based upon the ' ' strong acid extraction ' J 
 method, so well known through the work of Dr. Hilgard. 53 There are some very 
 pertinent objections, as well as advantages, to the method of acid extraction for 
 the purpose of comparing soils among themselves. 54 
 
 in the analysis 2.5 gram samples, air dry, were used throughout. The acid 
 extraction results are not included in this paper. 
 
 49 The writer wishes to emphasize the tedium of the elutriator process, and to advise 
 Strongly against the use of the apparatus for the comparison of the soils as to texture. The 
 elutriator is excellent from a theoretical point of view, but the results do not at all warrant 
 the extravagant use of time in the laboratory that the apparatus requires. 
 
 ""('. 8. Bur. Soils, Bull. 84, 1912. 
 
 "'' Ibid., Bull. 45, 1907; Proc. Amer. Soc. Agron., vol. 2 (1910), pp. 138-47. 
 
 02 Calif. Agr. Exp. Sta., Circ. 6 (1903), p. 17; Soils, pp. 197-99. 
 
 "Calif. Agr. Kxp. Sta., Circ. 6 (1903), pp. 16ff; Soils, pp. 340ff. 
 
 :A Sec Ilissink, Intern. Mitt, fur Bodenkunde, vol. 5 (1915), no. 1. 
 
1919] Pendleton: A Study of Soil Types 487 
 
 The sodium peroxide fusion method 55 was carried out on the two larger series 
 of soils, the Hanford and the San Joaquin. The elements sought were phosphorus, 
 calcium, and magnesium. Five gram samples, air dry, were used throughout. 
 The general method of analysis, as set forth by Hopkins, Avas employed, though 
 there were a number of refinements used to increase the accuracy of the results. 
 As such might be mentioned the double precipitation of the iron, aluminum, and 
 phosphorus. 
 
 Phosphorus was determined volumetrically, according to the method of Hib- 
 bard. 56 
 
 Total nitrogen was determined by the modified Gunning-Kjeldahl method, 
 using ten gram samples. 
 
 Loss on ignition was determined upon the 10 gram, air dry samples that were 
 used for the determination of the hygroscopic moisture of the samples used in 
 the chemical analysis. The soils were ignited in a muffle furnace to constant 
 weight. 
 
 Humus was determined by the Grandeau-Hilgard method, 57 using 10 gram 
 samples, air dry. 
 
 Potassium was determined by the J. Lawrence Smith method, using one gram 
 samples. 
 
 Bacteriological Methods 
 
 The only bacteriological methods employed were the determination by the tum- 
 bler or beaker method of the ammonifying, the nitrifying, and the nitrogen fixing 
 powers of the soils. 58 All cultures were run in duplicate. 
 
 Ammonification tests were made using 50 grams of soil and 2 grams (4%) of 
 dried blood. The checks were distilled at once, and the cultures kept in the incu- 
 bator at 24°C-30°C for one week. (The incubator thermostat was unsatisfactory 
 in its action, hence the variation in the temperature.) 
 
 The nitrifying power of the soil was tested as regards the soil's own nitrogen, 
 dried blood, cottonseed meal, and ammonium sulfate. In the Diablo clay adobe 
 and the Altamont clay loam 50 grams of soil were used, to which was added 1 
 gram (2%) of dried blood, or of cottonseed meal, or 0.1 gram (0.2%) of am- 
 monium sulfate. In the case of the San Joaquin sandy loam 50 grams of soil were 
 used, together with 1 gram (2%) of dried blood or of cottonseed meal, or 0.2 gram 
 (0.4%) of ammonium sulfate. In the series run on the Hanford fine sandy loam 
 100 grams of soil were used, to which were added 1 gram (1%) of dried blood or 
 of cottonseed meal or 0.2 gram (0.2%) of ammonium sulfate. It is to be regret- 
 ted that the several series could not all be run on exactly the same basis as the 
 Hanford series. But the small amount of stock soils of the samples of the earlier 
 series precluded the use of larger original samples, not to speak of the impossi- 
 bility of repeating these series. The cultures were incubated for four weeks at 
 24°C-30°C. At the end of this period the cultures were dried in the oven at about 
 90 °C and the nitrate content determined by the phenoldisulfonic acid method 
 according to the modifications of Lipman and Sharp. 59 
 
 Nitrogen fixation. For this determination uniform quantities of soil were 
 used throughout — 50 grams, to which was added 1 gram of mannite. These cul- 
 
 55 Hopkins, Soil Fertility and Permanent Agriculture, pp. 630-33; Hopkins and Pettit, 
 Soil Fertility Laboratory Manual (Boston, Ginn, 1910), pp. 42-45. 
 
 56 Jour. Ind. Eng. Chem., vol. 5, pp. 993-1009. 
 "Calif. Agr. Exp. Sta., Circ. 6 (1903), p. 21. 
 
 58 Burgess, P. S., Soil Bacteriology Laboratory Manual, Easton, Pa., The Chemical Pub- 
 lishing Co., 1914. 
 
 59 Univ. Calif. Publ. Agr. Sci., vol. 1 (1912), pp. 21-37. 
 
488 University of California Publications in Agricultural Sciences [Vol.3 
 
 tures were incubated for four weeks at 24°C-30°C, at the end of which time bac- 
 terial action was stopped by drying in the oven for 24 hours. Subsequently, the 
 samples were broken up in a mortar, and 10 grams weighed out for the determina- 
 tion of the total nitrogen. 
 
 Pot Cultures in the Greenhouse 
 
 The large samples of the surface foot of soil were stored in the greenhouse 
 until used. The preparation of the samples was in most cases as follows: The 
 sample was placed on a large table and screened through a quarter inch sieve. 
 This treatment of screening was attempted with the Diablo clay adobe and the 
 Altamont clay loam, but was abandoned as practically hopeless. The samples of 
 these two types had been collected in the late summer, when the ground was very 
 hard and dry, hence the clods defied any efforts to break them up. As an alterna- 
 tive the samples were as thoroughly mixed as possible and weighed out into the 
 pots. Several waterings during a week, together with carefully breaking up the 
 lumps by hand, rendered the soils finely divided enough to permit the planting of 
 the seeds. The Hanford and San Joaquin types were readily screened. 
 
 All the soils were weighed out into nine inch flower pots. In most cases the 
 pots had been previously paraffined. Care was taken to clean the pots thor- 
 oughly, as far as surface material was concerned; many of the pots were scrubbed 
 with a brush and water. All previously used pots were examined to exclude the 
 use of such as had formerly been used for soils containing high percentages of 
 soluble salts, but such examination was not always successful in eliminating the 
 undesirable pots, as was afterwards evident. In the Diablo, Altamont, and Han- 
 ford soils the quantity of soil used was five kilos per pot. In the San Joaquin 
 soils six kilos were used. 
 
 Enough soil was collected to fill eighteen pots. This would allow for the 
 arrangement of six sets of triplicates of every sample; and the planting of a dif- 
 ferent crop in each of the sets would allow for the growing simultaneously of six 
 different crops on every soil. For example, there were placed together in the 
 greenhouse and considered as a unit in the culture work the series of the Diablo 
 clay adobe, including three pots of the sample taken from San Juan Capistrano, 
 three from that taken near Los Angeles, three from that of the San Fernando 
 valley, and lastly three from the sample taken in the Danville region. This group 
 of pots was planted to oats, barley, bur clover, or any one other crop. The pots 
 were kept together in the greenhouse, that the conditions for each one in the set 
 would be as nearly uniform as possible, for even a slightly different location in 
 the greenhouse was found to affect the crop appreciably. The other five sets of 
 pots were similarly treated. No fertilizing materials were added to any of the 
 soils. All were used in their normal condition. The aim was to compare the crop 
 producing power of the representatives of a given type of soil from various 
 localities. 
 
 Several crops were grown, as the desire was to get a series of plants that 
 would grow well under greenhouse conditions, and act as indicators. It was 
 known that barley was about the best crop to use, but supplementary plants were 
 desired. Barley, wheat, oats, rye, millet, milo, cowpeas (black eye beans), soy 
 beans, beans (small white), bur clover (Mcdicago denticulata) , sweet clover (Meli- 
 lotus indica), and oats and bur clover in combination were tried. Some were 
 a marked success under greenhouse conditions, and others were practically total 
 failures; the better crops were given by barley, soy beans, bur clover, and millet. 
 Sweet clover gives excellent results. This wide range of varieties of plants was 
 
1919] Pendleton: A Study of Soil Types 489 
 
 necessary because of the fact that it was desired to grow two crops a year on the 
 soils. The winter crops will not do well in summer, and vice versa, even though 
 the summers in Berkeley are relatively cool, and though the greenhouse was 
 whitewashed during the summer months. 
 
 The seed was obtained in most cases from the Division of Agronomy of the 
 Department of Agriculture of the University of California. Such varieties as 
 were not available from this source were obtained from the commercial seed 
 houses in San Francisco. 
 
 Usually the seed was planted directly in the pots, using sufficient seed to be 
 sure that enough would germinate and grow to give the desired number of plants 
 per pot, usually six. After the plants were well established, and before there was 
 any crowding in the pots, the plants were thinned. In some cases an insufficient 
 number of plants germinated to give the desired number per pot. Difficulty was 
 found in getting the soy beans and cow T peas to germinate, especially in the 
 heavier soils. This was overcome by sprouting the seeds in an incubator and 
 planting them when the radicle was half an inch long or more. An excellent stand 
 was thus obtained. 
 
 Xo actual measurements of the height of the plants, or the length of leaves 
 were made in the greenhouse work. But photographs were taken, and in these 
 photographs the attempt was made to secure representative records of the entire 
 series, without photographing the crop in every pot. The usual procedure in the 
 Altamont and Diablo series was to photograph two pots out of each set of tripli- 
 cates, an attempt being made to select average, representative pots. In the large 
 Hanford series one representative pot of each set of triplicates in each crop 
 series was photographed, and three representative sets of triplicates were also 
 photographed. Thus some of the pots appear twice, and allow of comparisons. 
 
 If any doubt be entertained as to the relative weights of the crops in the pots 
 photographed as compared with those not so recorded, the relative weights of the 
 crops may be easily obtained by referring to the tables of dry weights. In prac- 
 tically every case the pot label can be read from the photograph. The method of 
 labeling is exemplified as follows: 
 
 6 Soil sample no. 6 (Diablo clay adobe from Danville). 
 
 W Wheat, first crop. 
 2 Pot 2 of the triplicate set first planted to wheat. 
 
 CP Cowpeas, second crop. 
 
 During the growth of the crops, notes were taken as to the relative growths and 
 the general conditions of the plants. 
 
 When the crop had ceased growing it was harvested, whether or not it was 
 mature in the sense of having set and developed seed. The plants from a given 
 pot were put in a paper bag, labeled, and placed in the drying oven for 2! hours. 
 The plants were weighed when dry and cool. If any mature seed was produced 
 it was weighed separately. 
 
 Between the first and second crops the soil was allowed to rest from two to 
 three weeks or longer. Each pot was emptied and the soil passed through a 
 quarter inch screen before replacing in the pot. This broke up the lumps and 
 removed most of the roots. The roots were not saved. The weight of the roots 
 would have been interesting, but their recovery, especially from the heavy soils, 
 would have involved careful washing, and the loss of much of the soil. It was 
 thought that some washing would be necessary, even in the Hanford series, in 
 order that the resulting figures might be at all accurate. 
 
490 University of California Publications in Agricultural Sciences [Vol. 3 
 
 APPENDIX B 
 SOIL SAMPLE LOCATIONS 
 
 Field Notes on the Soil Samples Collected 
 
 No. 1 — Diablo Clay Adobe 
 Location: A little over a mile east of San Juan Capistrano, Orange County. On 
 the lower slopes of the hills to the south of San Juan Creek. Sample sta- 
 tion is on a little shoulder running northwest, between Mr. Echenique's 
 house and the fence following the road to Prima Deshecka Canada. Ap' 
 proximately one-quarter mile from the above house. 
 Soil: 0-12 inches — Dark gray adobe; much cracked. 
 
 12-36 inches — Soil becomes gradually lighter in color, approaching a light 
 
 bluish gray mottled Avith brown. 
 36 inches — The subsoil becomes a silty clay loam in the lower depths. 
 History: The field was pastured up to and including 1906. From 1907 to date 
 the field has been annually planted to barley. Data from Mr. Echenique, 
 the owner. Sample collected August 19, 1917. 
 Depths of horizons: 
 
 1-A 0-12 inches. 1-B 12-24 inches. 1-C 24-36 inches. 
 
 No. 2 — Diablo Clay Adobe 
 
 Location: One and three-quarter miles east of southeast of Eastlake Park, Los 
 Angeles. Station is 0.7 mile by secondary road south of Pacific Electric 
 railroad crossing, and 1.2 miles southeast of the Southern Pacific railroad 
 crossing. Station is about 150 feet up the hill to the west of the road, in 
 grain field, and 75 feet south of a 10 or 12 year old eucalyptus grove. 
 The road, going south, emerges from the grove, and is then flanked by pep- 
 per trees. 
 
 Soil: 0-12 inches — Dark gray to almost black, but with a shade of brown rather 
 than a bluish gray. 
 12-24 inches — Dark grayish brown clay adobe, becoming a little lighter with 
 
 depth. 
 24-36 inches — Dark brown with soft, whitish fragments. Fragments probably 
 the partially weathered parent rock, though no outcrops of the rock were 
 seen in the vicinity. Previous to the collection of the sample, Mr. E. C. 
 Eckman, who mapped the area as the Bureau of Soils representative, said 
 in substance: "We have no good Diablo in the area; the body I am 
 directing you to is as good as any, but it is pretty brown. ' ' 
 
 History: Property owned by Mr. Huntington. Farmed to grain the past 2 
 years; pasture previously. Data from the son of the tenant. Sample col- 
 lected August 20, 1915. 
 
 Depths of horizons: 
 
 2-A 0-12 inches. 2-B 12-24 inches. 2-C 24-36 inches. 
 
 No. 3 — Altamont Clay Loam 
 Location: 1.4 miles southeast of Walnut, Los Angeles County, on the shoulder of 
 a low hill, about 200 feet east of the wagon road running south through 
 the hills. The station was selected so that the texture was about right, 
 for in a very short distance there were variations from a heavy dark clay 
 loam or clay adobe to the light clay loams. 
 
1919] Pendleton: A Study of Soil Types 491 
 
 Soil: 0-36 inches — A medium textured brown friable clay loam. The soil column 
 throughout was more or less filled with small soft whitish fragments, por- 
 tions of the parent rock. 
 36 inches — The weathered parent rock was encountered. 
 History : A. T. Currier, owner. The field is in pasture, and has not been culti- 
 vated for forty years, to the knowledge of the ranch foreman. The soil is 
 probably virgin. Sample collected August 20, 1915. 
 Depths of horizons: 
 
 3-A 0-12 inches. 3-B 12-24 inches. 3-C 24-36 inches. 
 
 No. 4 — Altamont Clay Loam 
 
 Location: On a hillside a few feet above the Cahuenga Pass (Burbank road), 
 near Oak Crest, Los Angeles County. Just a few feet from the U. S. 
 Bureau of Soils station for the type in the San Fernando area. (For map, 
 see the map under sample no. 25.) 
 
 Soil: 0-14 inches — A dark brown clay loam. 
 
 14-36 inches — A yellowish brown loam, grading into the weathered, thin bed- 
 ded shales at about 36 inches. 
 
 History : Roadside, above the big cut on the road, probably never tilled. The sur- 
 face is not so steep but that it could be well tilled; some of the soil in 
 the immediate vicinity is cultivated to grain. Sample collected August 21, 
 1915. 
 
 Depths of horizons: 
 
 4-A 0-12 inches. 4-B 12-24 inches. 4-C 24-36 inches. 
 
 No. 5 — Diablo Clay Adobe 
 
 Location: About % a mile north of Calabasas, San Fernando Valley, Los Angeles 
 County. The station is some distance up the hill to the west of the road 
 running north from the Calabasas store. The sample was collected near 
 the top of the hill, to the northeast of the oak tree. 
 
 Soil: A dark gray to black typical clay adobe. Distinctly heavy. Digging was 
 very difficult, the soil coming up in large, very hard clods. The soil was of 
 about the same color and texture down to the bedrock at 26 inches. The 
 bedrock is a heavy claystone or shale. 
 
 History : John Grant, Calabasas P. O., owner. The land has been dry farmed 
 to grain. Presumably there had been no additions of fertilizing materials 
 to the soil. Sample collected August 21, 1915. 
 
 Depths of horizons: 
 
 5-A 0-14 inches. 5-B 14-26 inches. 26 inches. Parent rock. 
 
 No. 6 — Diablo Clay Adobe 
 
 Location: In Contra Costa County, % mile west of Tassajero; 6 miles east 
 and a little south of Danville. Station about 150 feet up the hill to the 
 south of the road, that is, about one-third of the way up the hill. 
 
 Soil: 0-34 inches — A black or dark gray clay adobe, moist at 10 inches. 
 
 34-72 inches — A dark grayish brown subsoil, becoming lighter below the third 
 foot. No bedrock within the 6 foot section, nor was there any sign of any 
 outcrop in the vicinity. The slope of the hill moderate, the exposure 
 north. The sample was collected with the assistance of Mr. L. C. Holmes 
 and Mr. E. C. Eckman, both of the U. S. Bureau of Soils. They pro- 
 nounced the station typical. 
 
492 University of California Publications in Agricultural Sciences [Vol. 3 
 
 History: Property owned by J. J. Johnson. The field has been farmed to grain 
 for probably 60 years. Formerly the rotation was pasture one year, and 
 grain one year; now the practice is grain two years, and pasture one year. 
 Sample collected September 2, 1915. 
 
 Depths of horizons: 
 
 6-A 0-12 inches. 6-B 12-24 inches. 6-C 24-36 inches. 
 
 No. 7 — Altamont Clay Loam 
 
 Location: On the Mission Pass road, a little less than 2 miles south and a little 
 
 west of Sunol, Alameda County. About 100 feet above the road, between 
 
 wooden electric power poles nos. 92/30 and 92/31. 
 Soil: 0-34 inches — A medium brown clay loam, considered typical by Mr. L. C. 
 
 Holmes and Mr. E. C. Eckman of the U. S. Bureau of Soils. There were 
 
 slight changes in texture. 
 34 inches — A stiff clay horizon. 
 Inspection of a deep cut on the roadside near the location of the sample 
 
 station showed that at 6 feet and deeper there existed a heavy reddish clay. 
 
 In the immediate locality the road sections showed that the parent rock 
 
 was deeper than the 6 foot section. The slope of the land at the sample 
 
 station was quite steep. 
 History: Tom Burns, Irvington, owner. Field has been in pasture for the past 3 
 
 years at least, and probably for a much longer time. Sample collected 
 
 September 2, 1915. 
 Depths of horizons: 
 
 7-A 0-12 inches. 7-B 12-24 inches. 7-C 24-36 inches. 
 
 No. 10 — San Joaquin Sandy Loam 
 
 Location: North Sacramento, Sacramento County; }4 mi le east of tile factory, 
 across the road; opposite poles 57/32 and 57/33, 75 feet southeast from the 
 State Highway. 
 
 Soil: 0-26 inches — A brownish red sandy loam, slightly hog wallowed, and very 
 slightly rolling. 
 26-36 inches — A sandy clay loam. 
 36 inches — A hard hardpan. 
 
 History : Owner not known, the district now being subdivided, the property being a 
 portion of the old ' ' Hagan Grant. ' ' A near-by resident gave the following 
 information : ' ' The land has not been cultivated for the past 15 years or 
 more. The land is said to have been farmed to grain at one time for a few 
 years, but the ' soil is too light for wheat, it grows nothing but filaree. ' ' ' 
 The principal use has been for cattle and sheep pasture. Sample collected 
 March 28, 1916. 
 
 Depths of horizons: 
 
 10-A 0-12 inches. 10-B 12-24 inches. 10-C 24-36 inches. 
 
 No. 11 — San Joaquin Sandy Loam 
 
 Location : Four miles west of Lincoln, Placer County, at the l ' Road Corners, ' ' 
 in the southeast field, 10 feet east of the west fence and 60 feet south of 
 the north fence. 
 
1919J Pendleton: A Study of Soil Types 493 
 
 Soil: A gently hog wallowed, sandy loam, with some deeper depressions, prob- 
 ably stream channels. Sample slightly gravelly. 
 0-12 inches — Brownish or reddish brown sandy loam. 
 12-17 inches — Sandy clay loam or clay, color the same. 
 17-23 inches — A stiff reddish brown clay. 
 23 inches — A hard hardpan. 
 History: Mr. Frank Dowd, owner. The land has been planted to wheat for the 
 past 20 or 25 years; previous to that time it was used for pasture. Six 
 to 10 or 12 bushels of wheat, and 8 to 20 bushels of barley is the production 
 of this soil in the locality. The soil is usually fallowed on alternate years. 
 Land held at from $30 to $50 per acre. Sample collected March 28, 1916. 
 Depths of horizons: 
 
 11-A 0-11 inches. 11-B 11-17 inches. 11-C 17-23 inches. 
 
 No. 12 — San Joaquin Sandy Loam 
 
 Location: About 6 miles west of Wheatland, Sutter County. Near a road corner, 
 in a little swale west of a knoll, 15 feet east of the westerly fence of field, 
 and 150 feet south of the north line of the westerly road. 
 Soil: Texture slightly heavy, and barely enough sand for a sandy loam, but the 
 best found for several miles. Color brownish red, the same throughout the 
 entire depth. 
 0-18 inches — Light, fine textured, sandy loam. 
 18-31 inches — Heavy sandy clay loam, running into a stiff clay. 
 
 31 inches — Hardpan, sandy and somewhat soft. The ground was very 
 moist at this time. 
 History: Very evidently pasture for sheep and cattle. No signs of having been 
 cultivated for several years, at least. The cover is of a number of low 
 annuals — Orthocarpus, Trifolium, Centaurea, and others. Sample collected 
 March 29, 1916. 
 Depths of horizons: 
 
 12- A 0-12 inches. 12-B 12-18 inches. 12-C 18-31 inches. 
 
 No. 13 — San Joaquin Sandy Loam 
 
 Location: Three and three-quarters miles east of Elk Grove, Sacramento County. 
 On the Sheldon road, about 30 feet northwest from the fence on the north 
 side of the road. About 200 feet southwest from where a house formerly 
 stood. 
 Soil: A reddish brown sandy loam, approaching a loam; becoming redder in 
 color with increasing depth. 
 0-14 inches — Heavy sandy loam. 
 14-22 inches — Clay loam. 
 22-29 inches — Heavy clay loam. 
 29 inches — Compact hardpan. 
 History: Wackman Brothers, Elk Grove, owners. The land has not been plowed 
 or farmed for at least 15 years. The land is held at about $50 per acre. 
 Sample collected March 30, 1916. 
 Depths of horizons: 
 
 13-A 0-12 inches. 13-B 12-22 inches. 13-C 22-29 inches. 
 
494 University of California Publications in Agricultural Sciences [Vol. 3 
 
 No. 14 — Hanford Fine Sandy Loam 
 
 Location: One mile southeast of the Sheldon road, 3^ miles east of Elk Grove, 
 Sacramento County. On the southwest side of the secondary road, in al- 
 falfa field, about 25 feet from the fence. Station on a little rise. 
 Soil: 0-11 inches — A medium brown micaceous heavy fine sandy loam. 
 
 11-24 inches — A dark gray to black fine sandy loam, grading into the fol- 
 lowing. 
 24-36 inches — Brown fine sandy loam. Water table at 32 inches. 
 History: Mrs. A. C. Freeman, Elk Grove, owner. Land planted to alfalfa. Good 
 growth. No irrigation. Willows as well as alders and river ash along the 
 sloughs. Many scattering valley oaks. The land is subject to overflow 
 from the Cosumnes Eiver, as it lies low in the river bottom, and shallow 
 stream channels and sloughs are frequent. Sample collected March 30, 1916. 
 Depths of horizons: 
 
 14-A 0-12 inches. 14-B 12-24 inches. 14-C 24-36 inches. 
 
 No. 15 — Hanford Fine Sandy Loam 
 
 Location: North of Woodbridge, San Joaquin County, along the State Highway, 
 less than *4 mile south of the road running westerly from Acampo to the 
 highway. Station in a vineyard, with almond trees along the roadside, 20 
 feet northeast of "change telephone pole," 200 feet north of pine tree 
 at the gateway on the opposite side of the highway. (For map, see under 
 sample 16.) 
 
 Soil: Texture a rather coarse fine sandy loam; it was hard to find a good fine 
 sandy loam. Color when moist was a medium brown throughout the 3 foot 
 section ; the field color was a light grayish brown. 
 
 History: Mike Nolan estate, owner. The vineyard is of Tokay grapes, 10 to 12 
 years old. The land is held at $300 to $400 per acre. It is said to be a 
 losing game to farm this land to grapes at this valuation. Sample col- 
 lected March 30, 1916. 
 
 Depths of horizons: 
 
 15-A 0-12 inches. 15-B 12-24 inches. 15-C 24-36 inches. 
 
 No. 16 — Hanford Fine Sandy Loam 
 
 Location : Along the road north of Woodbridge, San Joaquin County. In a young 
 pear orchard about 65 feet west of the highway, and about 95 feet north 
 of the north abutments of the bridge over Mokelumne Eiver. 
 
 Soil: A medium brown fine sandy loam, similar throughout the soil column of 
 three feet. This soil is of the recent, flood-plain phase of the type, though 
 this station is not known to have been under water for a number of years, 
 at least. There is only a comparatively narrow shelf of this phase between 
 the older, higher phase, and the river. 
 
 History: A. Pen-in, Woodbridge, owner. The land had always been in brush 
 and pasture until it was cleared and planted to pears in 1911. Value 
 about $500 per acre. Sample collected March 30. 1916. 
 
 Depths of horizons: 
 
 16-A 0-12 inches. 16-B 12-24 inches. 16-C 24-36 inches. 
 
1919] Pendleton: A Study of Soil Types 495 
 
 No. 17 — San Joaquin Sandy Loam 
 Location : A short distance south of the east and west road that runs east to 
 Thalheim, San Joaquin County. The station was on a slight knoll 75 feet 
 south of a canal, and the same distance east of the secondary road running 
 north and south; not far from a vacant barn. 
 Soil: 0-12 inches — Eeddish brown. 
 12-21 inches — Slightly redder. 
 21 inches — Hardpan. 
 
 The surface had the characteristic hog wallows, and the usual scant vegeta- 
 tion of grasses and herbs, "filaree" being abundant; yet all vegetation 
 was more abundant than that in pastured fields. 
 History : Rev. Frank Hoffman, Acampo, owner. Apparently, the land has not 
 
 been cultivated in recent years. Sample collected March 31, 1915. 
 Depths of horizons: 
 
 17-A 0-12 inches. 17-B 12-21 inches. 
 
 No. 18 — San Joaquin Sandy Loam 
 Location : Two and one-half miles northwest of Madera, Madera County. Along- 
 State Highway, 75 to 100 feet southwest of the paved road, at telephone 
 pole 92/29; across the highway from the driveway to the house. 
 Soil: 0-5 inches — A light reddish brown sandy loam. A noticeable plow pan at 
 5 inches. 
 5-21 inches — A light brownish red sandy loam, becoming heavier below. 
 21-30 inches — Quite compact heavy sandy loam. 
 30 inches and deeper — A very compact hardpan. 
 
 Topography very gently rolling, hog wallows well developed, though consider- 
 ably degraded by cultivation. Barley grain not growing well in the lower 
 spots. 
 History: Cropped for probably 20 years to grains; barley at present. Land used 
 for pasture previous to grain farming. A good yield is 8 sacks, varying 
 from that down to little or nothing. Miller and Lux, owners. Sample col- 
 lected April 11, 1916. 
 Depths of horizons: 
 
 18-A 0-12 inches. 18-B 12-24 inches. 18-C 24-30 inches. 
 
 No. 19 — Hanford Fine Sandy Loam 
 
 Location: Eight miles east of Waterford, Stanislaus County, near Robert's Ferry 
 bridge. About 75 feet west of the road that runs south from the bridge 
 onto the bluff. About 450 feet north of the driveway to the Sawyer place. 
 Twenty-five feet inside of the fence, in the alfalfa field. 
 
 Soil: Medium brown fine sandy loam; a good brown color when moist. Texture 
 somewhat variable, some rounded gravels up to the size of a hen's egg. 
 Topography undulating, and more or less terraced, due to the old stream 
 channels. 
 
 History: G. H. Sawyer, Waterford, owner. Alfalfa planted in 1915, looks well. 
 Land previously planted to barley and wheat, with a production about as 
 follows: barley, 14 sacks is considered good; wheat with 12 sacks is good, 
 with 6 sacks a low average. Value of the land as recently determined in 
 court, in a case of flood damage by a canal break, is $100 per acre. On an 
 adjoining piece of land young walnut trees are doing very well. Sample 
 collected April 11, 1916. 
 
 Depths of horizons: 
 
 19-A 0-12 inches. 19-B 12-24 inches. 19-C 24-36 inches. 
 
496 University of California Publications in Agricultural Sciences [Vol. 3 
 
 No. 20 — Han ford Fine Sandy Loam 
 
 Location : Near Hopeton, Merced County, 14 miles north of Merced. Less than 
 14 mile north from the road corners, 15 feet east of the east fence of the 
 road, and 150 feet south of irrigating ditch. 
 
 Soil: A good medium brown fine sandy loam. The color is especially good when 
 the soil is moist. The topography is slightly uneven because of the old 
 stream channels. Going north along the road from the cross roads the 
 soil is quite gravelly at first, but the texture gradually becomes heavier, 
 with less gravel. At the sample station the texture is a rather heavy fine 
 sandy loam. 
 
 History: J. G. Euddle, Snelling, owner. The field is planted to alfalfa, as are 
 most of the Hanford soils in the locality. The land is not subject to 
 overflow. Sample collected April 13, 1916. 
 
 Depths of horizons: 
 
 20-A 0-12 inches. 20-B 12-24 inches. 20-C 24-36 inches. 
 
 No. 21 — San Joaquin Sandy Loam 
 
 Location: Near Nairn Station, Merced County. About 14 mile west of the rail- 
 road, 50 feet north of the private ranch road, and 120 feet east of the field 
 gate across the road. About 4 miles northwest of Merced. 
 Soil: A good brownish red San Joaquin color. Texture a sandy loam, grading 
 
 into a clay loam or clay at about 24 inches. 
 Depths of horizons: 
 
 24-27 inches — A heavy clay. 
 27 inches — Hardpan. 
 
 The same was taken from near the top of one of the hog wallow elevations. 
 The topography is gently rolling. 
 History: F. W. Henderson, Merced, owner. At the present time the land is used 
 as pasture. It has been plowed at some time in the past. The present 
 growth of wild herbage {Lepidium, small grasses, Cryptanthe, etc.) is 
 meager. Sample collected April 13, 1916. 
 Depths of horizons: 
 
 21-A 0-12 inches. 21-B 12-24 inches. 21-C 24-27 inches. 
 
 No. 22 — Hanford Fine Sandy Loam 
 
 Location: A short distance north of Basset, Los Angeles County, on the main 
 road north from Basset station. The sample was collected in a walnut 
 grove 100 feet east of the road and 250 feet south of the driveway to the 
 ranch house. 
 
 Soil: A good medium brown when moist, and a light grayish brown when dry. 
 Mr. L. C. Holmes, of the U. S. Bureau of Soils, described the soil at the 
 time of collection as being "all a little browner, and with a little more 
 color than a good Hanford. ' ? There was a very slight color change at 
 about a foot, the soil below was grayer. Texture a good fine sandy loam, 
 with practically no change in the 3 foot column. Topography smooth. 
 The texture varies quite rapidly from place to place in the field. Some 
 big washes of typical intermittent streams are found not far to the north 
 and west. 
 
1919] Pendleton: A Study of Soil Types .497 
 
 History: C. N. Basset, of Basset and Nebeker, Santa Monica, owner. The land 
 is planted to walnuts, and the trees are about 10 years old. They are 
 doing well, some replants are found. The trees are irrigated. Sample col- 
 lected May 22, 1916. 
 
 Depths of horizons: 
 
 22-A 0-12 inches. 22-B 12-24 inches. 22-C 24-36 inches. 
 
 No. 23 — Hanford Fine Sandy Loam 
 
 Location: South and west of the town of Anaheim, Orange County. Within a 
 radius of 20 feet of where the official Bureau of Soils sample was taken. 
 Thirty feet east of side road, and 100 feet north of main east and west road. 
 
 Soil: Brown fine sandy loam, possibly a little more silty than no. 22, but not 
 heavy enough for a heavy fine sandy loam. Dry field color a light, grayish 
 brown. Topography smooth, no stream channels visible. Irrigation in fur- 
 rows. Soil similar to about 62 inches, a little more grayish at 18 inches, 
 the change being gradual. At 62 inches a gray clean sand, or fine sand, 
 was found. 
 
 History: S. J. Luhring, R. F. D. no. 4, owner. The field was planted to Valencia 
 oranges in 1913 ; previously to grapes and miscellaneous crops. Sample 
 collected May 23, 1916. 
 
 Depths of horizons: 
 
 23-A 0-12 inches. 23-B 12-24 inches. 23-C 24-36 inches. 
 
 No. 24 — Hanford Fine Sandy Loam 
 
 Location: Southeast of the center of Los Angeles, half way from Magnolia Ave- 
 nue on Fruitland Road, to Salt Lake Railroad on the east. South side of 
 the road about 60 feet from center, in edge of corn field. Just across 
 road from east end of east cypress trees. 
 Soil : A medium brown fine sandy loam when moist ; color in the field is a grayish 
 brown. Micaceous. Topography level, no stream channels seen nearby. 
 Color of body variable. Sample location in the browner phase. Toward 
 south and east along the railroad and Arcadia Avenue the color is much 
 grayer, and even black when moist. Texture within the body is very vari- 
 able, though always within the fine sandy loam group. 
 0-36 inches — Fine sandy loam, grayer below. 
 36-37 inches — Layer of grayish sand and fine sand. 
 37-72 inches — Fine sandy loam, heavier in streaks. 
 History : C. D. Templeman, R. F. D. no. 2, Box 178, Los Angeles, owner. Land 
 has been in truck for 10 or 12 years. Only fertilizer, barnyard manure. 
 Sample collected May 24, 1916. 
 Depths of horizons: 
 
 24-A 0-12 inches. 24-B 12-24 inches. 24-C 24-36 inches. 
 
 No. 25 — Hanford Fine Sandy Loam 
 
 Location: Near Van Nuys, Los Angeles County; near official sample station. 
 Seventy-five feet west of center of road, between fourth and fifth rows of 
 apricot trees north from boundary. 
 
498 University of California Tuolications in Agricultural Sciences [Vol. 3 
 
 Soil: A good medium brown fine sandy loam; the field color a grayish brown. 
 The texture uniform throughout the 3 foot section, with a little gravel occa- 
 sionally. Also the texture is variable to about the usual degree, in the 
 field distribution. The color is slightly lighter at about 2 feet and below 
 throughout the C feet, with a little variation in an increasing amount of 
 coarser sands. 
 
 History: Chase, Eiverside, owner (?). Planted to apricots, 2 years old. Inter- 
 planted to melons. Sample collected May 24, 1916. 
 
 Depths of horizons: 
 
 25-A 0-12 inches. 25-B 12-24 inches. 25-C 24-36 inches. 
 
 No. 26 — San Joaquin Sandy Loam 
 
 Location: On the high bluffs about iy± miles southeast of Del Mar station, San 
 Diego County, close to the road that runs back along the main ridge. About 
 50 feet north of the road where it swings south to get around the head of 
 the big arroyo from the north. 
 Soil: A brownish red sandy loam. Surface covered with a moderate growth of 
 the low chapparal common to these exposed ridges. Soil heavily laden with 
 iron concretions. Surface has the usual hog wallows characteristic of the 
 San Joaquin series. 
 0- 6 inches — Eeddish brown sandy loam, many concretions. Dry. 
 j6— 13 inches — Clay (sandy), reddish in cracks, and bluish inside of lumps and 
 
 where not weathered. 
 13-22 inches — Clay, mostly bluish gray. 
 22-38 inches — Boring very difficult, due to the heavy nature of the clayey 
 
 moist material. Color bluish. 
 About 40 inches — Hardpan. Very compact. 
 History : Probably never farmed. Recently streets cleared, and an attempt made 
 to sell lots for building. Value for agriculture — none without irrigation. 
 Sample collected May 25, 1916. 
 Depths of horizons: 
 
 26-A 0-6 inches. 26-B 6-13 inches. 26-C 13-22 inches. 
 
UNIV. CALIF. PUBL. AGR, SCI. VOL. 3 
 
 [PENDLETON] PLATE 43 
 
 A general view in the greenhouse, where all the pot culture work was carried 
 on. The entire right hand bench was devoted to this study, also half again as 
 much space not visible in the print. 
 
UNIV. CALIF. PUBL. AGR. SCI. VOL. 3 
 
 [PENDLETON] PLATE 44 
 
 Diablo Clay Adobe — First Crop 
 Pots of same and different representatives of a given soil type compared. 
 Fig. 1. Oats and bur elover. Left to right — Soil 1, pot 1; soil 2, pot 2; 
 soil 5, pot 1 ; soil 6, pot 3. 
 
 Diablo Clay Adobe — First Crop 
 Pots of same and different representatives of a given soil type compared. 
 Fig. 2. Oats. Left to right— Soil 1, pot 1; soil 2, pot 3; soil 5, pot 2; soil 6, 
 pot 2. 
 
UNIV. CALIF. PUBL. AGR. SCI. VOL. 3 
 
 [ PENDLETON ] PLATE 45 
 
 Diablo Clay Adobe — First Crop 
 Pots of same and different representatives of a given soil type compared. 
 Fig. 1. Bur clover. Left to right — Soil 1, pot 1; soil 1, pot 2; soil 1, pot 3. 
 
 Diablo Clay Adobe — First Crop 
 Pots of same and different representatives of a given soil type compared. 
 Fig. 2. Bur clover. Left to right— Soil 2, pot 1; soil 2, pot 2; soil 2, pot 3. 
 
UNIV. CALIF. PUBL. AGR. SCI. VOL. 3 
 
 [ PENDlLETON ] PLATE 46 
 
 
 % 
 
 1S& >W^v 
 
 W&H 
 
 
 %il 
 
 .* : : ; f 
 
 Diablo Clay Adobe — First Crop 
 Pots of same and different representatives of a given soil type compared. 
 Fig. 1. Bnr clover. Left to right — Soil 5, pot 1; soil 5, pot 2; soil 5, pot 3. 
 
 m 
 
 Diablo Clay Adobe — First Crop 
 Pots of same and different representatives of a given soil type compared. 
 Fig. 2. Bur clover. Left to right— Soil 6, pot lj soil 6, pot 2; soil 6, pot 3. 
 
UNIV. CALIF. PUBL. AGR. SCI. VOL. 3 
 
 [ PENDLETON ] PLATE 47 
 
 Diablo Clay Adobe — First Crop 
 Pots of same and different representatives of a given soil type compared. 
 Bur clover. Left to right — Soil 1, pot 1; soil 2, pot 2; soil 5, pot 2; soil 6, 
 pot 1. 
 
UNIV. CALIF. PUBL. AGR. SCI. VOL, 3 
 
 [PENDLETON] PLATE 48 
 
 t 
 
 Diablo Clay Adobe — Second Crop 
 Pots of same and different representatives of a given soil type compared. 
 
 Dwarf milo («) following oats. Left to right — Soil 1, pot 2; soil 1, 
 
 Fig. 1. 
 
 pot 3; soil 2, pot 1 ; soil 2, pot 3; soil 5 
 pot 3. 
 
 pot 1 ; soil 5, pot 3; soil 6, pot 2; soil 6, 
 
 • 
 
 Diablo Clay Adobe — Second Crop 
 Pots of same and different representatives of a given soil type compared. 
 Fig. 2. Dwarf milo (b) following oats and bur clover. Left to right — Soil 1, 
 
 pot 1; soil 1, pot 3; soil 2, pot 1; soil 2, pot 3; soil 
 pot 1 ; soil 6, pot 3. 
 
 5, pot 1; soil 5, pot 3; soil 6, 
 
UNIV. CALIF. PUBL. AGR. SCI. VOL. 3 
 
 [ PENDLETON 1 PLATE 49 
 
 Diablo Clay Adobe — Second Crop 
 Pots of same and different representatives of a given soil type compared. 
 Fig. 1. Cowpeas, following wheat. Left to right — Soil 1, pot 1 ; soil 1, pot 2; 
 soil 2 pot 1 ; soil 2, pot 2; soil 5, pot 1 ; soil 5, pot 2; soil (i, pot 2; soil <i, pot 3. 
 
 Diablo Clay Adobe — Second Crop 
 Pots of same and different representatives of a given soil type compared. 
 Fig. 2. Soy beans, following barley. Left to right — Soil 1, pot 1; soil 1, 
 
 pot 2; soil 2, pot 1; soil 2, pot 3; soil 5, pot 1; soil 5, pot 2; soil 6, pot 1; soil 6, 
 
 pot 2. 
 
UNIV. CALIF. FUBL. AGR. SCI. VOL, 
 
 [ PENDLETON ] PLATE 50 
 
 Altamont Clay Loam — Second Crop 
 Pots of same and different representatives of a given soil type compared. 
 Cowpeas B, following barley. Left to right — Soil 3, pot 1 ; soil 3, pot- 
 soil 4, pot 1; soil 4, pot 3; soil 7, pot 1; soil 7, pot 3. 
 
UNiV. CALIF. PUBL. AGR. SCI. VOL. 3 
 
 [PENDLETON] PLATE 51 
 
 Altamont Clay Loam — Second Crop 
 Pots of same and different representatives of a given soil type compared. 
 Fig. 1. Soy beans A, following oats. Left to right — Soil 3, pot 1; soil 3, 
 pot 2; soil 4, pot 2; soil 4, pot 3; soil 7, pot 2; soil 7, pot 3. 
 
 Altamont Clay Loam — Second Crop 
 Pots of same and different representatives of a given soil type compared. 
 Fig. 2. Soy beans B, following Phaseolus. Left to right — Soil 3, pot 2 
 soil 3, pot 3; soil 4, pot 1; soil 4, pot 2; soil 7, pot 1; soil 7, pot 2. 
 
UNIV. CALIF. PUBL. AGR. SCI. VOL. 
 
 [ PENDLETON ] PLATE 52 
 
 Altamont Clay Loam — Second Crop 
 Pots of same and different representatives of a given soil type compared. 
 Fig. 1. Dwarf milo A, following wheat. Left to right — Soil 3, pot 2 ; soil 3, 
 pot 3; soil 4, pot 1; soil 4, pot 3; soil 7, pot 1; soil 7, pot 3. 
 
 Altamont Clay Loam — Second Crop 
 Pots of same and different representatives of a given soil type compared. 
 Fig. 2. Dwarf milo A, following bur clover. Left to right — Soil 3, pot 1 ; 
 soil 3, pot 2; soil 4, pot 1; soil 4, pot 3; soil 7, pot 1 ; soil 7, pot 3. 
 
UNIV. CALIF. PUBL. AGR. SCI. VOL. 3 
 
 [PENDLETON] PLATE 53 
 
 Haxford Fine Sandy Loam — First Crop 
 Pots of same and different representatives of a given soil type compared. 
 Fig. 1. Dwarf milo A. Left to right — Soil 14, pot 2; soil 15, pot 2; soil 16, 
 
 pot 3 ; soil 19, pot 3 ; soil 20, pot 2 ; soil 22, pot 2 ; soil 23, pot 1 ; soil 21, pot 2 ; 
 
 soil 2.1, pot 1. 
 
 Hanford Fine Sandy Loam — First Crop 
 Pots of same and different representatives of a given soil type compared. 
 Fig. 2. Dwarf milo A. Left to right— Soil 15, pot 1; soil 15, pot 2; soil 15, 
 
 pot 3; soil 20, pot 1; soil 20, pot 2; soil 20, pot 3; soil 23, pot 1; soil 23, pot 2; 
 
 soil 23, pot 3. 
 
1 
 
UNIV. CALIF. PUBL. AGR. SCI. VOL. 3 
 
 [ PENDLETON ] PLATE 54 
 
 I 
 
 Haxford Fixe Sandy Loam — First Crop 
 Pota of same and different representatives of a given soil type compared. 
 Fig. 1. Dwarf milo B. Left to right — Soil 14, pot 3; soil 15, pot 2; soil lb', 
 
 pot 1 : soil H», pot 3; soil 20, pot 2; soil 22, pot 3; soil 23, pot 3; soil 24, pot 2; 
 
 soil 25, pot •">. 
 
 
 :i 
 
 Haxford Fine Sandy Loam — First Crop 
 Pots of same and different representatives of a given soil type compared. 
 Fig. 2. Dwarf milo B. Left to right— Soil 14, pot 1; soil 14, pot 2; soil 14, 
 
 pot 3; soil 22, pot 1; soil 22, pot 2; soil 22, pot 3; soil 23, pot 1; soil 23, pot 2; 
 
 soil 23, pot 3. 
 
i 
 
UNIV. CALIF. PUBL. AGR. SCI. VOL. 3 
 
 [PENDLETON] PLATE 55 
 
 Haxford Fixe Sandy Loam — First (jrop 
 Pots of same and different representatives of a given soil type compared. 
 Fig. 1. Soy beans. Left to right — Soil 14, pot 1; soil 15, pot 1; soil 16, 
 
 pot 2; soil L9, pot 2; soil 20, pot 3: soil 22, pot 1; soil 23, pot 3; soil 24, pot 1; 
 
 soil 2.", pot 3. 
 
 Haxford Fine Sandy. Loam — First Crop 
 Pots of same and different representatives of a given soil type compared. 
 Fig. 2. Soy beans. Left to right— Soil 14, pot 1; soil 14, pot 2; soil 14, 
 
 pot 3; soil 16, pot 1; soil 16, pot 2; soil 16, pot 3; soil 23, pot 1; soil 23, pot 2; 
 
 soil 23, pot 3. 
 
UNIV. CALIF. PUBL. AGR. SCI. VOL. 3 
 
 [ PENDLETON ] PLATE 56 
 
 Haxford Fine Sandy Loam — First Crop 
 Pots of same and different representatives of a given soil type compared. 
 Fig. 1. Cowpeas B. Left to right— Soil 14, pot 1; soil 14, pot 2; soil 14, 
 pot 3; soil 22, pot 1 ; soil 22, pot 2; soil 22, pot 3; soil 23, pot 1; soil 23, pot 2; 
 
 soil 2:;, pot :;. 
 
 *; 
 
 Mi ' ££& 
 
 A I A ii^A A A* A 
 
 Hanford Fine Sandy Loam — First Crop 
 Pots of same and different representatives of a given soil type compared. 
 Fig. 2. Cowpeas B. Left to right — Soil 14, pot 3; soil 15, pot 2; soil 16, 
 
 pot 2; soil 19, pot 2; soil 20, pot 2; soil 22, pot 2; soil 23, pot 2; soil 24, pot 1; 
 
 soil 25, pot 3. 
 
UNIV. CALIF. PUBL. AGR. SCI. VOL. 3 
 
 [ PENDLETON ] PLATE 57 
 
 
 
 
 
 
 1 
 
 
 
 
 
 
 
 
 
 
 
 i 
 
 
 
 
 
 
 
 
 
 
 
 
 
 / 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 'J^ 
 
 tf ?*iLBgMi 
 
 g^agfe 
 
 i 
 
 £gi 
 
 
 ^ "f 
 
 £** 
 
 * 
 
 gMflpfc 
 
 &t$m 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 \ 
 
 
 
 
 
 
 
 Hanford Fixe Sandy Loam — Second Crop 
 Pots of same and different representatives of a given soil type compared. 
 Fig. 1. Barley, following soy beans. Left to right — Soil 14, pot 2; soil 15, 
 
 pot I ; soil 16, pot 3; soil 19, pot 3; soil 20, pot 1; soil 22, pot 2; soil 23, pot 3; 
 
 soil 24, pot •"> : soil 2-"), pot 1. 
 
 Hanford Fine Sandy Loam — Second Crop 
 Pots of same and different representatives of a given soil type compared. 
 Fig. 2. Barley, following soy beans. Left to right — Soil 14, pot 1; soil 14, 
 
 pot 2; soil 14, pot 3; soil 19, pot 1; soil 19, pot 2; soil 19, pot 2; soil 19, pot 3; 
 
 soil 23, pot 1; soil 23, pot 2; soil 23, pot 3. 
 
UNIV. CALIF. PUBL. AGR. SCI. VOL. 3 
 
 [PENDLETON] PLATE 58 
 
 |M | t J 
 
 ] 
 
 If I 
 
 V:' 
 
 ;«l» v !ii Es&sJLJL'U 
 
 MM 
 
 ?-<*izm? 
 
 i**&m&>m«T^a& ! '* v&n "•itfafiK^vss. 
 
 
 IIaxford Fine Sandy Loam — Second Crop 
 Pots of same and different representatives of a given soil type compared. 
 Wheat, following millet. Left to right — Soil 14, pot 1; soil 15, pot 1; soil 16, 
 pot 1; soil 19, pot 3; soil 20, pot 1; soil 22, pot 1; soil 23, pot 1; soil 24, pot 1; 
 
 soil 25, pot 3. 
 
UNIV. CALIF. PUBL. AGR. SCI. VOL. 3 
 
 [PENDLETON] PLATE 59 
 
 . 
 
 Hanford Fine Sandy Loam — Second Crop 
 Pots of same ami different representatives of a given soil type compared. 
 Wheat, folio-wing millet. Left to right — Soil 16, pot 1 ; soil 16, pot 2 ; soil 16, 
 
 pot 3; soil 22, pot 1 ; soil 22, pot 2; soil 22, pot 3; soil 24, pot 1; soil 24, pot 2; 
 
 soil 24, pot 3. 
 
UNIV. CALIF. PUBL. AGR. SCI. VOL. 3 
 
 [PENDLETON] PLATE 60 
 
 Hanford Fixe Sandy Loam — Second Crop 
 Pots of same and different representatives of a given soil type compared. 
 Fig. 1. Barley, following cowpeas. Left to right — Soil 14, pot 2; soil 15, 
 
 pot ::; soil 16, pot 2; soil ]9, pot 2; soil 20, pot 1; soil 22, pot 3; soil 23, pot 3; 
 
 soil 24, pot :'» ; soil 2.1, pot 1. 
 
 '. 
 
 Haxford Fine Sandy Loam — Second Chop 
 Pots of same and different representatives of a given soil type compared. 
 Fig. 2. Barley, following cowpeas. Left to right — Soil 19, pot 1; soil ]9, 
 
 pot 2; soil j 9, pot 3; soil 20, pot 1; soil 20, pot 2; soil 20, pot 3; soil 23, pot 1; 
 
 soil 23, pot 2 ; soil 23, pot 3. 
 
UNIV. CALIF. PUBL. AGR. SCI. VOL. 3 
 
 [PENDLETON] PLATE 61 
 
 Hanford Fine Sandy Loam — Second Crop 
 Pots of same and different representatives of a given soil type compared. 
 Fig. 1. Oats, following milo. Left to right — Soil 14, pot 3; soil 15, pot 2; 
 
 soil 16, pot 2; soil 19, pot 1; soil 20, pot 2; soil 22, pot 1; soil 23, pot 3; soil 24, 
 
 pot 1 ; soil 25, pot 1. 
 
 
 
 i 
 
 
 **$* / " ;' .-^ 
 
 " ' 'f '"BUiiiT ' ' i 1 """^ £ 
 
 1 
 
 j 
 
 1 1 ! 
 
 ^> i 
 
 | ! ! 
 
 
 r 
 
 ■ 
 
 i" 
 
 
 
 
 tej 
 
 « — — — -^ 
 
 
 
 = ■ - — ■; 
 
 
 
 
 
 
 
 
 ■ _ 
 
 
 
 
 Hanford Fine Sandy Loam — Second Crop 
 Pots of same and different representatives of a given soil type compared. 
 Fig. 2. Oats, following milo. Left to right — Soil 14, pot 1 ; soil 14, pot 2 ; 
 
 soil 14, pot 3; soil 15, pot 1; soil 15, pot 2; soil 15, pot 3; soil 24, pot 1; soil 24, 
 
 pot 2; soil 24, pot 3. 
 
UNIV. CALIF. PUBL. AGR. SCI. VOL. 3 
 
 [ PENDLETON ] PLATE 62 
 
 Hanford Fine Sandy Loam — Second Crop 
 Pots of same and different representatives of a given soil type compared. 
 
 Melilotus indica, following eowpeas. Left to right — Soil 14, Pot 1; Soil 15, 
 Pot 3; Soil 16, Pot 2; Soil 19, Pot 2; Soil 20, Pot 1. 
 
UNIV. CALIF. PUBL. AGR. SCI. VOL. 3 
 
 [PENDLETON] PLATE 63 
 
 
 
 
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 "1 
 
 
 
 
 
 
 
 T 
 
 {/ : 
 
 . 
 
 
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 - ,/X 
 
 
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 9W& 
 
 
 Hanford Fine Sandy Loam — Second Crop 
 Pots of same and different representatives of a given soil type compared. 
 Melilotus indica, following eowpeas. Left to right — Soil 22, Pot 2; Soil 23, 
 Pot ] ; Soil 24, Pot 1; Soil 25, Pot 1. 
 
UNIV. CALIF. PUBL. AGR. SCI. VOL. 3 
 
 [ PENDLETON ] PLATE 64 
 
 
 Hanford Fine Sandy Loam — Second Chop 
 Pots of same and different representatives of a given soil type compared. 
 Melilotus indica, following cowpeas. Left to right — Soil 15, Pot 1; Soil 15, 
 Pot 2; Soil 15, Pot 3; Soil 23, Pot 1. 
 
UNIV. CALIF. PUBL. AGR. SCI. VOL. 3 
 
 [ PENDLETON ] PLATE 65 
 
 IIanf-ord Fine Sandy Loam — Second Crop 
 Pots of same and different representatives of a given soil type compared. 
 
 Melilotus indica, following cowpeas. Left to right— Soil 23, Pot 2; Soil 23, 
 Pot 3; Soil 25, Pot 1 ; Soil 25, Pot 2; Soil 25, Pot 3. 
 
UNIV. CALIF. PUBL. AGR. SCI. VOL. 3 
 
 [ PENDLETON ] PLATE 66 
 
 
 
 • 
 
 
 
 
 
 V 
 
 ^ ngjjj^— 
 
 
 ■^HHBte^^P^^ 
 
 -^■P\. — 
 
 -- 
 
 
 
 
 
 
 
 Haxford Fixe Sandy Loam — Second Crop 
 Pots of same and different representatives of a given soil type compared. 
 Bur clover, following milo. Left to right — Boil 14, Pot 1 ; Soil 15, Pot 1; 
 Soil 16, Pot 2; Soil 19, Pot 1: Soil 20, Pot 1. 
 
 Haxford Fixe Saxdy Loam — Secoxd Crop 
 Pots of same and different representatives of a given soil type compared. 
 
 Bur clover following milo. Left to right— Soil 22, Pot 1 ; Soil 23, Pot 1 
 Soil 24, Pot 1; Soil 2o, Pot 1. 
 
UNIV. CALIF. PUBL. AGR. SCI. VOL. 3 
 
 [ PENDLETON ] PLATE 67 
 
 Haxford Fine Sandy Loam — Second Crop 
 Pots of same and different representatives of a given soil type compared. 
 Bur clover, following milo. Left to right— Soil 19, Pot 1; Soil 19, Pot 2; 
 Soil 19, Pot 3; Soil 23, Pot 1; Soil 23, Pot 2. 
 
 *5k t^tit 
 
 Hanford Fine Sandy Loam — Second Crop 
 Pots of same and different representatives of a given soil type compared. 
 Bur clover, following milo. Left to right— Soil 23, Pot 3; Soil 25, Pot 1 
 Soil 23, Pot 2: Soil 23, Pot 3. 
 
UNIV. CALIF. PUBL. AGR. SCI. VOL. 3 
 
 [PENDLETON] PLATE 68 
 
 San Joaquin Sandy Loam 
 Pots of same and different representatives of a given soil type compared. 
 Eye. Left to right— Soil 10, pot 2; soil 11, pot 1; soil 12, pot 2; soil 13, 
 pot 3; soil 17, pot 3; soil 18, pot 1; soil 21, pot 1; soil 26, pot 1. 
 
UNIV. CALIF. FUBL. AGR. SCI. VOL. 
 
 r PENDLETON ] PLATE 69 
 
 San Joaquin Sandy Loam 
 Pots of same and different representatives of a given soil type compared. 
 Fig. 1. Melilotus indica. Left to right— Soil 10, pot 1; soil 11, pot 3; soil 12, 
 pot 2; soil 13, pot 1; soil 17, pot 3; soil 18, pot 3; soil 21, pot 2; soil 28, pot 1. 
 
 
 
 
 
 
 [■ ' 
 
 
 Lti 
 
 
 
 _ 
 
 '- ' : '■■ 
 
 
 •• 1 
 
 
 \ 
 
 -' 
 
 
 1 
 
 
 Iff 
 
 ■I: 
 mm 
 
 w 
 
 
 
 
 
 Br ^ 
 
 ■ - 
 
 
 - '- " -;-> 
 
 L___' 
 
 - 
 
 
 
 San Joaquin Sandy Loam 
 
 Pots of same and different representatives of a given soil type compared. 
 
 Fig. 2. Melilotus indica. Left to right — Soil 13, pot 1; soil 13, pot 2; soil 13, 
 pot 3; soil 17, pot 1; soil 17, pot 2; soil 17, pot 3; soil 26, pot 1; soil 28, pot 2; 
 soil 26, pot 3. 
 
UNIV. CALIF. PUBL. AGR. SCI. VOL. 3 
 
 [PENDLETON] PLATE 70 
 
 San Joaquin - Sandy Loam 
 Pots of same and different representatives of a given soil type compared. 
 Eye. Left to right — Soil 10, pot 1; soil 10, pot 2; soil 10, pot 3; soil 18, 
 pot 1; soil 18, pot 2; soil 18, pot 3; soil 26, pot 1; soil 26, pot 2; soil 26, pot 3. 
 
UNIV. CALIF. PUBL. AGR. SCI. VOL, 3 
 
 [PENDLETON] PLATE 71 
 
 San Joaquin Sandy Loam 
 Pots of same and different representatives of a given soil type compared. 
 Fig. 1. Barley. Left to right— Soil 10, pot 3; soil 11, pot 2; soil 12, pot 3; 
 soil 13, pot 1; soil 17, pot 3; soil 18, pot 2; soil 21, pot 3; soil 26, pot 1. 
 
 
 San Joaquin Sandy Loam 
 
 Pots of same and different representatives of a given soil type compared. 
 
 Fig. 2. Barley. Left to right— Soil 10, pot 1 ; soil 10, pot 2 ; soil 10, pot 3 ; 
 soil 18, pot 1; soil 18, pot 2; soil 18, pot 3; soil 26, pot 1; soil 26, pot 2; soil 23, 
 pot 3. 
 
UNIV. CALIF. PUBL. AGR. SCI. VOL. 3 
 
 [PENDLETON] PLATE 72 
 
 Jf^fe^WjES! 
 
 San Joaquin Sandy Loam 
 Pots of same and different representatives of a given soil type compared. 
 Fig. 1. Oats. Left to right — Soil 10, pot 1; soil 11, pot 1; soil 12, pot 2; 
 soil 13, pot 1; soil 17, pot 2; soil 18, pot 3; soil 21, pot 1; soil 28, pot 3. 
 
 San Joaquin Sandy Loam 
 
 Pots of same and different representatives of a given soil type compared. 
 
 Fig. 2. Oats. Left to right— Soil 11, pot 1; soil 11, pot 2; soil 11, pot 3; 
 soil 17, pot 1; soil 17, pot 2; soil 17, pot 3; soil 21, pot 1; soil 21, pot 2; soil 21. 
 pot 3. 
 
UNIV. CALIF, PUBL. AGR. SCI. VOL. 3 
 
 [PENDLETON] PLATE 73 
 
 i > 
 
 San Joaquin Sandy Loam 
 Pots of same and different representatives of a given soil type compared. 
 Fig. 1. Wheat. Left to right— Soil 10, pot 1. ; soil 11, pot 3; soil 12, pot 1; 
 soil 13, pot ] ; soil 17, pot 1; soil 18, pot 2; soil 21, pot 1; soil 26, pot 3. 
 
 San Joaquin Sandy Loam 
 
 Pots of same and different representatives of a given soil type compared. 
 
 Fig. 2. Wheat. Left to right— Soil 10, pot 1; soil 10, pot 2; soil 10, pot 3; 
 soil 13, pot 1; soil 13, pot 2; soil 13, pot 3; soil 17, pot 1; soil 17, pot 2; soil 17, 
 pot 3. 
 
UNIV. CALIF. PUBL. AGR. SCI. VOL. 3 
 
 [ PENDLETON ] PLATE 74 
 
 
 fc'- 
 
 IV.vi 
 
 i 
 
 San Joaquin Sandy Loam 
 Pots of same and different representatives of a given soil type compared. 
 Fig. 1. Bur clover. Left to right— Soil 10, pot 2; soil 11, pot 2; soil 12, 
 pot 3; soil 13, pot 1; soil 17, pot 3; soil 18, pot 2; soil 21, pot 1; soil 26, pot 3. 
 
 San Joaquin Sandy Loam 
 
 Pots of same and different representatives of a given soil type compared. 
 
 Fig. 2. Bur clover. Left to right— Soil 10, pot 1; soil 10, pot 2; soil 10, 
 pot 3; soil 18, pot 1; soil 18, pot 2; soil 18, pot 3; soil 26, pot 1; soil 26, pot 2; 
 soil 26, pot 3.