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
[Illustration: FIG. 23.—Interfering ripples on a mercury surface,
showing interference along hyperbolic lines (Vincent).]
All along each hyperbola the disturbance due to the combined effect of
the waves is either doubled or annulled when compared with that due
to each wave-train separately. With the apparatus described, we can
arrange to create and adjust two sets of similar water ripples from
origins not far apart, and on looking at the complicated shadow-pattern
due to the interference of the waves, we shall be able to trace out
certain white lines along which the waves are annulled, these lines
being hyperbolic curves (see Fig. 23). With the same appliances
another characteristic of wave-motion, which is equally important, can
be well shown.
[Illustration: FIG. 24.]
We make one half of the circular tank in which the ripples are
generated much more shallow than the other half, by placing in it
a thick semicircular plate of glass. It has already been explained
that the speed with which long waves travel in a canal increases with
the depth of the water in the canal. The same is true, with certain
restrictions, of ripples produced in a confined space or tank, one part
of which is much shallower than the rest. If waves are made by dropping
water on to the water-surface in the deeper part of the tank, they will
travel more quickly in this deeper part than in the shallower portion.
We can then adjust the water-dropping jet in such a position that it
creates circular ripples which originate in deep water, but at certain
places pass over a boundary into a region of shallower water (see Fig.
24). The left-hand side of the circular tank represented in the diagram
is more shallow than the right-hand side.
When this is done, we notice two interesting facts, viz. that the
wave-lines are bent, or _refracted_, where they pass over the boundary,
and that the waves are shorter or nearer together in the shallower
region. This bending, or refraction, of a wave-front in passing the
boundary line between two districts in which the wave has different
velocities is an exceedingly important characteristic of wave-motion,
and we shall have brought before us the analogous facts in speaking of
waves in air and waves in æther.
[Illustration: FIG. 25.]
Public-domain text, read in full here on John Shaqi.
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