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
The mixed mineral mass, called “Caliche,” when taken out
of the ground is dissolved in water; and the solution
boiled down, during which process the common salt is first
deposited and is raked out of the pans; the nitrate is
afterward farther purified by crystallization. As brought
into commerce for agricultural purposes it constitutes a
moist gray saline mass, somewhat resembling common salt,
of which substance it usually contains a few per cent;
occasionally also a small amount of sodic perchlorate (which
acts injuriously on vegetation). Aside from its use as a
fertilizer, Chile saltpeter serves for the manufacture
of nitric acid; and either directly, or after previous
transformation into potassic nitrate, for that of gunpowder.
The Chilean locality is the only one from which the
commercial article is derived; the deposits elsewhere are
too limited in extent to compete commercially with the South
American product. Caliche ranging as high as 80% of nitrate
of soda has been sent to the writer from the Colorado
Desert in Southern California, but the exact locality of
occurrence has not been divulged. Extended areas of clay
hills impregnated with nitrates exist in the Death Valley
region of California, but in the absence or extreme scarcity
of water in that region, it is doubtful whether these
impregnations can be made practically available. Another
locality is that near White Plains, Nevada, where Caliche
averaging about 50% purity is found in cavities and crevices
of a reddish volcanic rock. The rainfall in this region is
so slight that the greater part of the dust or sand blown
about by the wind consists of Glauber’s salt. Here also,
as in Chile, the niter deposits appear to be restricted to
within a short distance from the surface, and the total
amount thus far observed appears to be insufficient to
encourage large-scale exploitation.
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