The new air world : $b The science of meteorology simplified — John Shaqi
The new air world : $b The science of meteorology simplifiedMoore, Willis L. (Willis Luther)
Science
The new air world : $b The science of meteorology simplified
Moore, Willis L. (Willis Luther)
Meteorology
It is important that this mixture of gases that constitutes our air
be maintained in the right proportion. Only a slight difference in
relative amounts might be disastrous to life. An increase in the
oxygen would stimulate mental and physical activities and hold the
human faculties at a higher tension. Man would accomplish more in a
given time, but his span of life would be shortened; and too great an
increase in the proportion of this stimulating element would quickly
terminate life. Conversely an increase in the nitrogen would render
all life more lethargic and man would be slower to act and to think;
and too great an increase would smother every living thing.
In addition to the gases named, the air contains small amounts of
many other substances,—argon, nitric acid, ammonia, ozone, xenon,
krypton, and neon; as well as organic matter, germs, and dust in
suspension. Over the land it contains sulphates in minute quantities,
and over the sea and near the seashore salt left from the evaporated
spray.
The proportion of each component of the atmosphere by volume of the
total atmosphere is different from its proportion by weight. The
percentages for the more abundant gases are as follows:
===============+=============+===========
| BY VOLUME | BY WEIGHT
---------------+-------------+-----------
Nitrogen | 78.04 | 75.46
Oxygen | 20.99 | 23.19
Argon | 0.94 | 1.30
Carbon dioxide | 0.03 | 0.05
+-------------+-----------
| 100.00 | 100.00
===============+=============+===========
=Nitrogen.= Its principal functions are to dilute the oxygen and to
furnish food to vegetation. It is inert and does not manifest many
marked chemical affinities. Its lack of activity is shown by the fact
that it will neither support combustion nor burn.
=Oxygen.= Oxygen, unlike nitrogen, is an active element that readily
enters into chemical combination with many other elements, and it
is second in quantity to nitrogen. With hydrogen it constitutes
eight ninths, by weight, of water; combined with other elements it
constitutes forty to fifty per cent. of the crust of the earth. It
burns so readily that were it not greatly diluted by an inert gas
like nitrogen it would be difficult if not impossible to stop a
conflagration when once started. It is the vitalizing principle in
all forms of life. By its chemical union with carbon in the tissues
of plants and animals it develops the energy manifested in their
movements.
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