Soils, their formation, properties, composition, and relations to climate and plant growth in the humid and arid regionsHilgard, Eugene W. (Eugene Woldemar)
Science
Soils, their formation, properties, composition, and relations to climate and plant growth in the humid and arid regions
Hilgard, Eugene W. (Eugene Woldemar)
Soils
[Illustration: FIG. 8.—Illustration of Results of Hydraulic
Elutriation, showing extremes of soil texture, and intermediate loam.]
[Illustration: FIG. 9.—Illustration of Results of Hydraulic
Elutriation, showing Alluvial Silts and Pine-Woods Soil.]
_Physical composition corresponding to popular designations of Soil
quality._—The subjoined table illustrates the physical composition
of a number of soils from the State of Mississippi, selected for
their representative character, in order to deduce therefrom
approximate definitions of physical character corresponding to popular
designations. This table, published in 1873 in accordance with results
obtained during the two preceding years, does not require any material
modification on account of subsequent investigations. It lacks,
however, a characteristic representative of the predominant soils of
the arid region, viz., the silty soils so prevalent in dry climates,
only approximately represented by No. 165 of the table; hence two such,
from California, exemplifying respectively the valley deposits of the
Sacramento and Colorado rivers, have been added to the list.
It must not, however, be understood that these typical soils
necessarily represent correctly the physical constitution of all
soils falling under the same popular designation; for we are far from
being able as yet to predict accurately in every case the tilling
qualities of a soil material from its physical composition. To do this
it would be necessary not only to know with some degree of precision
the several physical coefficients of each of the several grain-sizes,
and perhaps of many more intermediate ones; but we would also have to
construct a formula according to which each could be given its proper
weight when present in varying proportions, and of varying shapes,
surface condition, and material. For this our present knowledge is
wholly inadequate, if indeed the problem is not beyond the limits of
mathematical computation. We must for the present at least be satisfied
with the empirical approximations afforded us by the constantly
increasing number of such analyses, correlated with farming experience.
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