The Quarterly Journal of Science, Literature and the Arts, July-December, 1827Various
Science
The Quarterly Journal of Science, Literature and the Arts, July-December, 1827
Various
Arts -- Periodicals; Science -- Periodicals; Technology -- Periodicals
We have seen that each undulation produced by an oscillatory motion
was composed of two semiundulations, which [p124] occasioned in the
particles of the fluids velocities exactly equal in their intensity,
though opposite in the direction of the motions. Let us at first
suppose that two whole undulations, moving in the same line and in
the same direction, differ half an undulation in their progress:
they will then be superinduced on each other through one half of
their length, or of their breadth, as we should say in speaking
of the waves of a liquid: but I here use in preference the term
length as applied to the interval between the two points which are
similarly affected by the motions of two consecutive undulations.
In the supposed case of the coincidence of one half of each of the
undulations, the interference will only take place with respect to
the parts so coinciding: that is, to the latter half of the first
undulation, and the preceding half of the second: and if these two
semiundulations are of equal intensity, since they tend to give, to
the same points of the ether, impulses directly opposite, they will
wholly neutralise each other, and the motion will be destroyed in
this part of the fluid, while it will subsist without alteration in
the two other halves of the undulations. In such a case, therefore,
half of the motion only would be destroyed.
If now we suppose that each of these undulations, differing in their
progress by half the whole length of each, is preceded and followed
by a great number of other similar undulations; then, instead of
the interference of two detached undulations, we must consider the
interference of two systems of waves, which may be supposed equal
in their number and their intensity. Since, by the hypothesis, they
differ half an undulation in their progress, the semiundulations of
the one, which tend to cause in the particles of ether a motion in
one direction, coincide with the semiundulations of the other, which
urge them in the opposite direction, and these two forces hold each
other in equilibrium, so that the motion is wholly destroyed in the
whole extent of these two systems of waves, except the two extreme
semiundulations, which escape from the interference. But these
semiundulations will always constitute a very small part of the whole
series to be considered.
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