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 author had an instance of this before him not long ago. He was at
a place where very large masts were being erected. One of these masts,
about 50 feet long, was resting on two great blocks of wood placed
under each end. This mast was a fine beam of timber, square in section,
and each side about 2 feet wide. The mast, therefore, lay like a bridge
on its terminal supports. Standing or jumping on the middle of this
great beam produced hardly any visible deflection. The writer, however,
placed his hand on the centre of the log and pressed it gently.
Repeating this pressure at intervals, discovery was soon made of the
natural time-period of vibration, and by repeating the pressures at the
right moment it was found that large oscillations could be accumulated.
If he had ventured to proceed far with this operation, it is certain
that, with properly timed impulses, it would have been possible, by
merely applying the pressure of one hand, to break in half this great
wooden mast.
We have constant occasion in mechanical work to notice that whereas one
pull or push of great vigour will not create some desired displacement
of an object, a number of very small hits, or properly timed pushes
or pulls, will achieve the requisite result. We might summarize the
foregoing facts by saying that it is a maxim in dealing with bodies
capable of any kind of free vibration that impulses, however small,
will create oscillations of any required magnitude, if only applied at
intervals equal to the natural free period of vibration of the body in
question.
We can illustrate these principles by a few experiments which have
special reference to musical instruments. If we fasten one end of a
rope to a fixed support, we find we can produce a wave or pulse in the
rope by jerking the free end up and down with the hand. The speed with
which a pulse or wave travels along a rope depends upon its weight per
unit of length, or, say, on the number of pounds it weighs per yard,
and on the tension or pull on the rope. The tighter the rope, the
quicker it travels; and for the same tension the heavier the rope, the
slower it travels.
It is not difficult to show that the speed with which the pulse
travels is measured by the square root of the quotient of the tension
of the rope by its weight per unit of length, or, as it may be called,
the density of the rope.
Public-domain text, read in full here on John Shaqi.
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