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Widtsoe, John Andreas, 1872-1952

"Dry-Farming : a System of Agriculture for Countries under a Low Rainfall"





CHAPTER V
DRY-FARM SOILS


Important as is the rainfall in making dry-farming successful, it is
not more so than the soils of the dry-farms. On a shallow soil, or
on one penetrated with gravel streaks, crop failures are probable
even under a large rainfall; but a deep soil of uniform texture,
unbroken by gravel or hardpan, in which much water may be stored,
and which furnishes also an abundance of feeding space for the
roots, will yield large crops even under a very small rainfall.
Likewise, an infertile soil, though it be deep, and under a large
precipitation, cannot be depended on for good crops; but a fertile
soil, though not quite so deep, nor under so large a rainfall, will
almost invariably bring large crops to maturity.
A correct understanding of the soil, from the surface to a depth of
ten feet, is almost indispensable before a safe Judgment can be
pronounced upon the full dry-farm possibilities of a district.
Especially is it necessary to know (a) the depth, (b) the uniformity
of structure, and (c) the relative fertility of the soil, in order
to plan an intelligent system of farming that will be rationally
adapted to the rainfall and other climatic factors.


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