The Economic Aspect of GeologyLeith, C. K. (Charles Kenneth)
Science
The Economic Aspect of Geology
Leith, C. K. (Charles Kenneth)
Geology, Economic
War-time development of the nitrogen industry in the United States for
munition purposes brought the domestic production almost up to the
pre-war requirements for fertilizers alone. With the increasing demand
for fertilizers and with the cheapness of the Chilean supply of natural
nitrates, it is likely that the United States will continue for a good
many years to import considerable amounts of Chilean nitrates. It may be
noted that, although this country normally consumes about one-fourth of
the Chilean product, American interests commercially control less than
one-twentieth of the output. Presumably, if for no other purpose than
future protection, effort will be made to develop the domestic industry
to a point where in a crisis the United States could be independent of
Chile. Particularly may an increase in the output of by-product ammonia
from coke manufacture be looked for (see also pp. 118-119), since
nitrogenous material thus produced need bear no fixed part of the cost
of production, and requires no protective tariff.
The reserves of Chilean nitrate are known to be sufficient for world
requirements for an indefinitely long future.
GEOLOGIC FEATURES
Mineral nitrates in general, and particularly those of soda and potash,
are readily soluble at ordinary temperatures. Mineral nitrate deposits
are therefore very rare, and are found only in arid regions or other
places where they are protected from rain and ground-water. The only
large deposits known are those of northern Chile and some extensions in
adjacent parts of Peru and Bolivia. These are located on high desert
plateaus, where there is almost a total absence of rain, and form
blankets of one to six feet in thickness near the surface. The most
important mineral, the sodium nitrate or Chile saltpeter, is mingled
with various other soluble salts, including common salt, borax minerals,
and potassium nitrate, and with loose clay, sand, and gravel. The
nitrate deposits occur largely around and just above slight basin-like
depressions in the desert which contain an abundance of common salt. The
highest grade material contains 40 to 50 per cent of sodium nitrate, and
material to be of shipping grade must run at least 12 to 15 per cent.
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