Dry-Farming : A System of Agriculture for Countries under a Low RainfallWidtsoe, John Andreas
Science
Dry-Farming : A System of Agriculture for Countries under a Low Rainfall
Widtsoe, John Andreas
Dry farming
the cultivated soils, though the direct evaporation was no smaller,
the number of pounds of water for each pound of dry substance was as
low as 265.
One of the chief values of fallowing lies in the liberation of the
plant-food during the fallow year, which reduces the quantity of
water required the next year for the full growth of crops. The Utah
experiments to which reference has already been made show the effect
of the previous soil treatment upon the water requirements of crops.
One half of the three types of soil had been cropped for three
successive years, while the other half had been left bare. During
the fourth year both halves were planted to corn. For the sandy loam
it was found that, on the part that had been cropped previously, 659
pounds of water were required for each pound of dry matter produced,
while on the part that had been bare only 573 pounds were required.
For the clay loam 889 pounds on the cropped part and 550 on the
previously bare part were required for each pound of dry matter. For
the clay 7466 pounds on the cropped part and 1739 pounds on the
previously bare part were required for each pound of dry matter.
These results teach clearly and emphatically that the fertile
condition of the soil induced by fallowing makes it possible to
produce dry matter with a smaller amount of water than can be done
on soils that are cropped continuously. The beneficial effects of
fallowing are therefore clearly twofold: to store the moisture of
two seasons for the use of one crop; and to set free fertility to
enable the plant to grow with the least amount of water. It is not
yet fully understood what changes occur in fallowing to give the
soil the fertility which reduces the water needs of the plant. The
researches of Atkinson in Montana, Stewart and Graves in Utah, and
Jensen in South Dakota make it seem probable that the formation of
nitrates plays an important part in the whole process. If a soil is
of such a nature that neither careful, deep plowing at the right
time nor constant crust cultivation are sufficient to set free an
abundance of plant-food, it may be necessary to apply manures or
commercial fertilizers to the soil. While the question of restoring
soil fertility has not yet come to be a leading one in dry-farming,
yet in view of what has been said in this chapter it is not
impossible that the time will come when the farmers must give
primary attention to soil fertility in addition to the storing and
conservation of soil-moisture. The fertilizing of lands with proper
plant-foods, as shown in the last sections, tends to check
transpiration and makes possible the production of dry matter at the
lowest water-cost.
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