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
It is undoubtedly true that the thorough tillage involved in
dry-farming exposes to the action of the elements the organic matter
of the soil and thereby favors rapid oxidation. For that reason the
different ways in which organic matter may be supplied regularly to
dry-farms are pointed out in Chapter XIV. It may also be observed
that the header harvesting system employed over a large part of the
dry-farm territory leaves the large header stubble to be plowed
under, and it is probable that under such methods more organic
matter is added to the soil during the year of cropping than is lost
during the year of fallowing. It may, moreover, be observed that
thorough tillage of a crop like corn or potatoes tends to cause a
loss of the organic matter of the soil to a degree nearly as large
as is the case when a fallow field is well cultivated. The thorough
stirring of the soil under an arid or semiarid climate, which is an
essential feature of dry-farming, will always result in a decrease
in organic matter. It matters little whether the soil is fallow or
in crop during the process of cultivation, so far as the result is
concerned.
A serious matter connected with fallowing in the Great Plains area
is the blowing of the loose well-tilled soil of the fallow fields,
which results from the heavy winds that blow so steadily over a
large part of the western slope of the Mississippi Valley. This is
largely avoided when crops are grown on the land, even when it is
well tilled.
The theory, recently proposed, that in the Great Plains area, where
the rains come chicfly in summer, the growing of hoed crops may take
the place of the summer fallow, is said to be based on experimental
data not yet published. Careful and conscientious experimenters, as
Chilcott and his co-laborers, indicate in their statements that in
many cases the yields of wheat, after a hoed crop, have been larger
than after a fallow year. The doctrine has, therefore, been rather
widely disseminated that fallowing has no place in the dry-farming
of the Great Plains area and should be replaced by the growing of
hoed crops. Chilcott, who is the chief exponent of this doctrine,
declares, however, that it is only with spring-grown crops and for a
succession of normal years that fallowing may be omitted, and that
fallowing must be resorted to as a safeguard or temporary expedient
to guard against total loss of crop where extreme drouth is
anticipated; that is, where the rainfall falls below the average. He
further explains that continuous grain cropping, even with careful
plowing and spring and fall tillage, is unsuccessful; but holds that
certain rotations of crops, including grain and a hoed crop every
other year, are often more profitable than grain alternating with
clean summer fallow. He further believes that the fallow year every
third or fourth year is sufficient for Great Plains conditions.
Jardine explains that whenever fall grain is grown in the Great
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