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 consider, in the first place, the effect of sending out into
the air two sets of air waves of slightly different wave lengths.
These waves both travel at the same rate, hence we shall not affect
the combined effects of the waves upon the air if we consider both
sets of waves to stand still. For the sake of simplicity, we will
consider that the wave-length of one train is 20 inches, and that
of the other is 21. Moreover, let the two wave-trains be so placed
relatively to one another that they both start from one point in the
same phase of movement; that is, let their zero points, or their humps
or hollows, coincide. Then if we draw two wavy lines (see Fig. 56)
to represent these two trains, it will be evident that, since the
wave-length of one is 1 inch longer than that of the other—that is, a
distance equal to twenty wave-lengths—one wave-train will have gained
a whole wave-length upon the other, and in a distance equal to ten
wave-lengths, one wave train will have gained half a wave-length upon
the other. If we therefore imagine the two wave-trains superimposed,
we shall find, on looking along the line of propagation, an alternate
doubling or destruction of wave-effect at regular intervals. In other
words, the effect of superimposing two trains of waves of slightly
different wave-lengths is to produce a resultant wave-train in which
the wave-amplitude increases up to a certain point, and then dies away
again nearly to nothing, as shown in the lowest of the three wave-lines
in Fig. 56.
[Illustration: FIG. 56.—The formation of beats by two wave-trains.]
We must, then, determine how far apart these points of maximum
wave-amplitude or points of no wave effect lie. If the wave-length of
one train is, as stated, 20 inches, then a length of ten wave-lengths
is 200 inches, and this must be, therefore, the distance from a
place of maximum combined wave-effect to a place of zero wave-effect.
Accordingly, the distance between two places where the two wave trains
help one another must be 400 inches, and this must also be the distance
between two adjacent places of wave-destruction. If, therefore, we look
along the wavy line representing the resultant wave, every 400 inches
we shall find a maximum wave-amplitude, and every 400 inches a place
where the waves have destroyed each other. We may call this distance
_a wave-train length_, and it is obviously equal to the product of
the constituent wave-lengths divided by the difference of the two
constituent wave-lengths.
Public-domain text, read in full here on John Shaqi.
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