On Molecular and Microscopic Science, Volume 1 (of 2)Somerville, Mary
History
On Molecular and Microscopic Science, Volume 1 (of 2)
Somerville, Mary
Matter -- Constitution; Microscopy; Natural history
Natural plumbago or graphite has little or no porosity and cannot be
used in these experiments, but the pores of artificial graphite of which
pencils are made, appear to be so minute that only isolated molecules of
gas are able to pass, without however being at all impeded by friction;
for the smallest pores that we can suppose to exist in the graphite must
be real tunnels compared with the minuteness of the ultimate atoms or
molecules of a gaseous body. The cause of motion appears to reside
solely in that internal movement of molecules which is now generally
admitted as an essential condition of matter in a gaseous state. The
molecules and atoms are assumed to be perfectly elastic and to move in
all directions with different velocities according to the nature of the
gas. Enclosed in a porous vessel the moving atoms constantly strike
against its walls and against one another, but in consequence of their
perfect elasticity, no loss of movement results from the collision. When
the gases inside and outside of the tube are of the same density and
molecular movement, an exchange takes place without any perceptible
change of volume; but when the two gases are of different densities and
molecular velocities, then the reciprocal penetration ceases to be equal
on the two sides. Reciprocal diffusion of gases is accelerated by heat
and retarded by cold; the tension of the gases is increased in the first
case, and diminished in the second.
In Mr. Graham’s experiments relating to effusion, a gas under a constant
pressure was on one side of a minute opening in a very thin plate, and a
vacuum on the other. The rapidity with which air or gases enter the
vacuum depends upon their specific gravity. A gas rushes into a vacuum
with the speed acquired by a heavy body in falling from the height of an
atmosphere of the gas in question supposed to be everywhere of the same
density. The height of this uniform atmosphere will be in an inverse
ratio to the density of the gas. An atmosphere of hydrogen, for example,
will be 16 times higher than one of oxygen. But the velocity acquired by
a heavy body not being in direct proportion to the height, but to the
square root of the height, it follows that the rate of flow of different
gases into a vacuum will be in an inverse ratio to the square root of
their respective densities. The rate of flow of oxygen being represented
by 1, that of hydrogen will be represented by 4 the square root of 16.
This law has been verified by experiment, and is quite analogous to that
which regulates molecular diffusion, but the phenomena are essentially
different. It is the gas _en masse_ which partakes of the movements of
effusion, whilst only the molecules or atoms of a gas are affected by
the movements of diffusion. For that reason the swiftness of the
effusion of a gas is many thousand times greater than that of diffusion.
The swiftness of the efflux of atmospheric air is as rapid as the
velocity of sound.
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