Meteorology: The Science of the AtmosphereTalman, Charles Fitzhugh
Science
Meteorology: The Science of the Atmosphere
Talman, Charles Fitzhugh
Meteorology
As we have stated on another page, lightning discharges cause nitrogen
and oxygen to combine in the atmosphere, and perhaps also combine
nitrogen and hydrogen to form ammonia. There is one other natural
process by which atmospheric nitrogen is fixed. Certain species of
bacteria are able to extract this gas from the atmosphere and combine
it with other materials. Some of these bacteria are independent
organisms, while others form colonies of parasites growing on the roots
of higher plants, chiefly members of the pea family. In the latter case
the bacteria use the nitrogen of the air and carbohydrates drawn from
the roots on which they grow to form nitrogenous compounds, which are,
in part, transmitted to the host plant.
Unfortunately these natural processes do not suffice to maintain
agricultural soils in a high state of fertility. Mineral deposits of
combined nitrogen are practically limited to the nitrate fields of
Chile, from which more than two million tons of nitrate of soda are
exported annually; but this supply cannot last more than a few decades.
Combined nitrogen in the form of ammonia is supplied on a large and
rapidly growing scale from by-product coke ovens, and another perennial
source of nitrogenous matter is found in animal and vegetable refuse of
all kinds, including fish scrap and slaughter-house refuse, garbage,
sewage, manure, etc. Since, however, the demands of agriculture and
the manufacturing industries greatly exceed the total amount of
combined nitrogen obtainable from all these sources, the ingenuity of
inventors has been spurred to the task of fixing atmospheric nitrogen
by artificial methods, and several such methods have now been put in
operation commercially. Their combined product at present constitutes
nearly one-third of the total nitrogen supply of the world.
Public-domain text, read in full here on John Shaqi.
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