Waves and ripples in water, air, and æther : $b Being a course of Christmas lectures delivered at the Royal Institution of Great BritainFleming, J. A. (John Ambrose), Sir
Science
Waves and ripples in water, air, and æther : $b Being a course of Christmas lectures delivered at the Royal Institution of Great Britain
Fleming, J. A. (John Ambrose), Sir
Electric waves; Sound; Waves
The above calculation was made first by Newton; and he was unable
to explain how it was that the velocity of the air wave, calculated
in the above manner from the general formula for wave-speed, gave a
value for the velocity, viz. 912·6, which was so much less than the
observed velocity of sound, viz. 1090 feet per second at 0° C. The
true explanation of this difference was first given by the celebrated
French mathematician Laplace. He pointed out that in air, as in all
other gases, the elasticity, when it is compressed slowly, is less
than that when it is compressed quickly. A gas, when compressed, is
heated, and if we give this heat time to escape, the gas resists the
compression less than if the heat stays in it. Hence air is a little
more resilient to a very sudden compression than to a slow one. Laplace
showed that the ratio of the elasticity under sudden compression was
to that under slow compression in the same ratio as the quantities of
heat required to raise a unit mass of air 1° C. under constant pressure
and under constant volume. This ratio is called “the ratio of the two
specific heats,” and is a number close to 1·41. Hence the velocity, as
calculated above, must be corrected by multiplying the number 844,168
by the number 1·41, and then taking the square root of the product.
When this calculation is made, we obtain, as a result, the number 1091,
which is exactly the observed value of the velocity of sound in feet
per second at 0° C. and under atmospheric pressure. The velocity of
sound is much affected by wind or movement of the air. Sound travels
faster with the wind than against it. Hence the presence of wind
distorts the shape of the sound wave by making portions of it travel
faster or slower than the rest.
These two facts explain how it happens that loud sounds are sometimes
heard at great distances from the source, but not heard at places close
by.
[Illustration: FIG. 47 (reproduced by permission of proprietors of
_Knowledge_).—Map of South of England, showing places (black dots) at
which sound of funeral guns was heard, February 1, 1901.]
Public-domain text, read in full here on John Shaqi.
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