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Widtsoe, John Andreas, 1872-1952

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


The column headed "Insoluble Residue" shows the average proportions
of arid and humid soils which remain undissolved by acids. It is
evident at once that the humid soils are much less soluble in acids
than arid soils, the difference being 84 to 69. Since the only
plant-food in soils that may be used for plant production is that
which is soluble, it follows that it is safe to assume that arid
soils are generally more fertile than humid soils. This is borne out
by a study of the constituents of the soil. For instance, potash,
one of the essential plant foods ordinarily present in sufficient
amount, is found in humid soils to the extent of 0.21 per cent,
while in arid soils the quantity present is 0.67 per cent, or over
three times as much. Phosphoric acid, another of the very important
plant-foods, is present in arid soils in only slightly higher
quantities than in humid soils. This explains the somewhat
well-known fact that the first fertilizer ordinarily required by
arid soils is some form of phosphorus:
The difference in the chemical composition of arid and humid soils
is perhaps shown nowhere better than in the lime content.


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