The Atlantic Monthly, Volume 06, No. 33, July, 1860: A Magazine Of Literature, Art, And PoliticsVarious
Science
The Atlantic Monthly, Volume 06, No. 33, July, 1860: A Magazine Of Literature, Art, And Politics
Various
American periodicals
However it may be compressed, air returns, on liberation, to its
original volume, and while thus perfectly elastic it is also the most
compressible of bodies. This elasticity arises from the repulsive
force of its particles, and is always equal to the compressive force
which it balances. A glass vessel full of air, placed under a receiver
and then exhausted by the air-pump, will burst into atoms. Water, on
the other hand, is almost the reverse. Twenty cubic inches, introduced
into a cannon whose sides are three inches thick, cannot be compressed
into nineteen inches without bursting it. This non-elastic property of
water, with another, that of communicating, when under the action of
any force, an equal pressure in all directions, led to the invention
of the hydraulic press.
The elasticity of the air enables fishes to rise and sink in water,
through the action of the air-bladder.
The sudden compression of air liberates its latent heat, and produces
fire. On this principle the pneumatic tinder-box is constructed.
Brockhaus says that air has as yet been compressed only into
one-eighth of its original bulk.
For every degree of heat between the freezing-point and the boiling-point,
32° and 212°, the expansion of air is about 1/490th part, so that
any invention which seeks to use rarefied air as a motive power
must employ a very intense degree of heat, enough to fuse many kinds
of metals.
To the celebrated Mr. Boyle and to Henry Cavendish, both of Great
Britain, we are indebted for most of what we know of this particular
property of the air.
* * * * *
Density, or closeness, is another quality of the atmosphere. It has
been found to be 770 times less than that of water, and 770 cubic
inches of air weigh as much as a cubic inch of water. It is in direct
ratio with its elasticity, and there are tables by which it may be
determined at different altitudes. At the surface of the earth, this
density is indicated as 1; at 2-1/2 miles, as 1/2; at 5 miles, as 1/4;
and so on, the difference being in a geometrical progression.
As we proceed in the consideration of our general subject, we shall
find, under the appropriate heads, that density is not without
material influence on reflection and refraction, on transparency and
the transmission of light, the presence or absence of moisture, and
the amount of heat at the earth's surface,--and we might add, on
health, and the increase or diminution of the vital energies.
* * * * *
Temperature is another branch of our subject, and one involving a
series of subordinate topics on which volumes have been written, and
to which are still devoted the labors of the most learned men of our
day. In this place, merely an out-line can be attempted.
Public-domain text, read in full here on John Shaqi.
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