Sound is a mechanical wave that
results from the back and forth vibration of the particles of the medium
through which the sound wave is moving. If a sound wave is moving from left to
right through air, then particles of air will be displaced both rightward and
leftward as the energy of the sound wave passes through it. The motion of the
particles is parallel (and anti-parallel) to the direction of the energy
transport. This is what characterizes sound waves in air as longitudinal waves.
A vibrating tuning fork is capable of creating such a
longitudinal wave. As the tines of the fork vibrate back and forth, they push
on neighboring air particles. The forward
motion of a tine pushes air molecules horizontally to the right and the
backward retraction of the tine creates a low-pressure area allowing the air
particles to move back to the left.
Because of the longitudinal motion of the air particles,
there are regions in the air where the air particles are compressed together
and other regions where the air particles are spread apart. These regions are
known as compressions and rarefactions respectively.
The compressions are regions of high air pressure while the rarefactions are
regions of low air pressure. The diagram below depicts a sound wave created by
a tuning fork and propagated through the air in an open tube. The compressions
and rarefactions are labeled.
The wavelength of a wave
is merely the distance that a disturbance travels along the medium in one
complete wave cycle. Since a wave repeats its pattern once every wave cycle,
the wavelength is sometimes referred to as the length of the repeating patterns
- the length of one complete wave. For a transverse wave, this length is
commonly measured from one wave crest to the next adjacent wave crest or from
one wave trough to the next adjacent wave trough. Since a longitudinal wave
does not contain crests and troughs, its wavelength must be measured
differently. A longitudinal wave consists of a repeating pattern of
compressions and rarefactions. Thus, the wavelength is commonly measured as the
distance from one compression to the next adjacent compression or the distance
from one rarefaction to the next adjacent rarefaction.
Since a sound wave consists of a repeating pattern of
high-pressure and low-pressure regions moving through a medium, it is sometimes
referred to as a pressure wave. If a
detector, whether it is the human ear or a man-made instrument, were used to
detect a sound wave, it would detect fluctuations in pressure as the sound wave
impinges upon the detecting device. At one instant in time, the detector would
detect a high pressure; this would correspond to the arrival of a compression
at the detector site. At the next instant in time, the detector might detect
normal pressure. And then finally a low pressure would be detected,
corresponding to the arrival of a rarefaction at the detector site. The
fluctuations in pressure as detected by the detector occur at periodic and
regular time intervals. In fact, a plot of pressure versus time would appear as
a sine curve. The peak points of the sine curve correspond to compressions; the
low points correspond to rarefactions; and the "zero points"
correspond to the pressure that the air would have if there were no disturbance
moving through it. The diagram below depicts the correspondence between the
longitudinal nature of a sound wave in air and the pressure-time fluctuations
that it creates at a fixed detector location.
The above diagram can be somewhat misleading if you are not
careful. The representation of sound by a sine wave is merely an attempt to
illustrate the sinusoidal nature of the pressure-time fluctuations. Do not
conclude that sound is a transverse wave that has crests and troughs. Sound
waves traveling through air are indeed longitudinal waves with compressions and
rarefactions. As sound passes through air (or any fluid medium), the particles
of air do not vibrate in a transverse manner. Do not be misled - sound waves
traveling through air are longitudinal waves.
1. A sound wave is a pressure wave; regions of high
(compressions) and low pressure (rarefactions) are established as the result of
the vibrations of the sound source. These compressions and rarefactions result
because sound
a. is more dense
than air and thus has more inertia, causing the bunching up of sound.
b. waves have a
speed that is dependent only upon the properties of the medium.
c. is like all
waves; it is able to bend into the regions of space behind obstacles.
d. is able to
reflect off fixed ends and interfere with incident waves
e. vibrates
longitudinally; the longitudinal movement of air produces pressure fluctuations.
Answer: E
Since the
particles of the medium vibrate in a longitudinal fashion, compressions and
rarefactions are created. Study the tuning fork animation provided on the
Tutorial page.