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
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 experiment with the ball rolling down a slope is an instructive
one to make, because it brings clearly before the mind what is meant
by saying, in scientific language, that one thing “varies as the
square root” of another. We meet with so many instances of this mode
of variation in the study of physics, that the reader, especially the
young reader, should not be content until the idea conveyed by these
words has become quite clear to him or her.
Thus, for instance, the time of vibration of a simple clock pendulum
“varies as the square root of the length;” the velocity of a canal
wave “varies as the square root of the depth of the canal;” and the
velocity or speed acquired by a falling ball “varies as the square
root of the distance fallen through.” These phrases mean that if we
have pendulums whose lengths are in the ratio of 1 to 4 to 9, then the
respective times of their vibration are in the ratio of 1 to 2 to 3.
Also a similar relation connects the canal-depth and wave-velocity, or
the ball-velocity and height of fall.
Returning again to canal waves, it should be pointed out that the real
path of a particle of water in the canal, when long waves are passing
along it, is a very flat oval curve called an ellipse. In the extreme
cases, when the canal is very wide and deep, this ellipse will become
nearly a circle; and, on the other hand, when narrow and shallow, it
will be nearly a straight line. Hence, if long waves are created in
a canal which is shallow compared with the length of the wave, the
water-particles simply oscillate to and fro in a horizontal line. There
is, however, one important fact connected with wave-propagation in a
canal, which has a great bearing on the mode of formation of what is
called a “bore.”
As a wave travels along a canal, it can be shown, both experimentally
and theoretically, that the crest of the wave travels faster than the
hollow, and as a consequence the wave tends to become steeper on its
front side, and its shape then resembles a saw-tooth.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account