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
Let us apply these rules to calculate the speed of a long wave in a
canal having water 8 feet deep in it. The half-depth of the canal is
therefore 4 feet. The square root of 4 is 2; hence the speed of the
wave is that of a body which has fallen from a height of 4 feet, and is
therefore 16 feet per second, or nearly 11 miles an hour. When we come
to consider the question of waves made by ships, in the next chapter,
a story will be related of a scientific discovery made by a horse
employed in dragging canal-boats, which depended on the fact that the
speed of long waves in this canal was nearly the same as the trotting
speed of the horse.
[Illustration: FIG. 15.]
It may be well, as a little digression, to point out how the law
connecting height fallen through and velocity acquired by the falling
body may be experimentally illustrated for teaching purposes.
The apparatus is shown in Fig. 15. It consists of a long board placed
in a horizontal position and held with the face vertical. This board
is about 16 feet long. Attached to this board is a grooved railway,
part of which is on a slope and part is horizontal. A smooth iron
ball, A, about 2 inches in diameter, can run down this railway, and is
stopped by a movable buffer or bell, B, which can be clamped at various
positions on the horizontal rail. At the bottom of the inclined plane
is a light lever, T, which is touched by the ball on reaching the
bottom of the hill. The trigger releases a pendulum, P, which is held
engaged on one side, and, when released, it takes one swing and strikes
a bell, G. The pendulum occupies half a second in making its swing. An
experiment is then performed in the following manner: The iron ball is
placed at a distance, say, of 1 foot up the hill and released. It rolls
down, detaches the pendulum at the moment it arrives at the bottom of
the hill, and then expends its momentum in running along the flat part
of the railway. The buffer must be so placed by trial that the iron
ball hits it at the instant when the pendulum strikes the bell. The
distance which the buffer has to be placed from the bottom of the hill
is a measure of the velocity acquired by the iron ball in falling down
the set distance along the hill. The experiment is then repeated with
the iron ball placed respectively four times and nine times higher up
the hill, and it will be found that the distances which the ball runs
along the flat part in one half-second are in the ratio of 1, 2, and 3,
when the heights fallen through down the hill are in the ratio of 1, 4,
and 9.
The inference we make from this experiment is that the velocity
acquired by a body in falling through any distance is proportional to
the square root of the height. The same law holds good, no matter how
steep the hill, and therefore it holds good when the body, such as a
stone or ball, falls freely through the air.
Public-domain text, read in full here on John Shaqi.
Waves and ripples in water, air, and æther : $b Being a course of Christmas lectures delivered at the Royal Institution of Great Britain — John Shaqi
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