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How sound moves
Sound waves are compression waves. This means that the
disturbance of the particles is in the same direction as the propagation
of the wave. Imagine bunching up several loops of a stretched out slinky
and then releasing them. As the wave moves from one end of the slinky
to another, the loops of the slinky are seen to move along the length
of the slinky as well, not at right angles as is the case for transverse
waves. This is an excellent model of a compression wave, which is also
known as a longitudinal wave.
Sound travels through a medium from the source to the observer,
thus if there is no medium, you can't hear anything. To convince yourself
of this, see if you can get access to a bell jar. Put a continuous source
of sound in it, like a ringing bell and slowly pump out the air. The sound
will be fainter and fainter until eventually there will be no sound reaching
your ear at all. This occurs when there is no air in the jar, and thus
no medium for the sound to propagate through.
Like all waves, sound travels at different speeds depending
on the medium it is traveling through. The exact velocity for the speed
of the propagation of sound in a given medium can be found by using the
equation
This equation makes sense because the speed of a compression
wave is dependent on how far from their neutral positions the molecules
of a medium can be moved (its elasticity) and how close together these
molecules are (its density). As you can see, the greater the elasticity
and the lesser the density of the medium, the faster the sound travels
through it. The reason that sound travels faster in air (see table below)
is that the rising temperature decreases the density of the air without
really affecting the elasticity of the medium. While temperature affects
the speed of sound in ideal gases, pressure, interestingly enough, does
not. This is because a change in pressure affects both the elasticity
and the density of a gas in the same proportion, so the velocity of sound
remains unchanged.
Refer to the following table for the speed of sound in
various media.
|
Medium
|
Speed of sound (m/s) |
| Air (0º C) |
331 |
| Air (20º C) |
343 |
| Helium |
965 |
| Hydrogen |
1284 |
| Water (0º C) |
1402 |
| Water (20º C) |
1482 |
| Seawater |
1522 |
| Aluminum |
6420 |
| Steel |
5941 |
| Granite |
6000 |
Not only must a sound-producing body be in contact with
some medium that transmits the sound, but it must also be a vibrating
body. Remember that a sound wave is a compression wave. This name gives
a hint to how exactly sound is transmitted. When sound waves travel, they
produce alternating condensations and rarefactions. Although
sound is a longitudinal wave, a condensation is equivalent to a crest
in a transverse wave, and is an area of greater than normal pressure.
A rarefaction is equivalent to a trough in a transverse wave and is an
area of smaller than normal pressure. Picture a tuning fork. As the tines
vibrate, they bend back and forth. As they bend outwards, the air on either
side of the fork is compressed, increasing its pressure and causing it
to push against the air next to it which only has normal pressure. As
they bend back inwards, they create more space for the air, causing an
area of lower pressure to form. This motion sets up a wave of alternating
lower and higher pressure, which is propagated outward. In this manner,
compression waves like sound travel. See the illustration below.

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