*Michael Fowler 3/23/07*

We’ll begin by considering sound traveling down a hollow pipe, to avoid unnecessary mathematical complications. Sound is a longitudinal wave—as the wave passes through, the air moves backwards and forwards in the pipe, this oscillatory movement is in the same direction the wave is traveling.

To visualize what’s happening, imagine mentally dividing the air in the pipe, which is at rest if there is no sound, into a stack of thin slices. Think about one of these slices. In equilibrium, it feels equal and opposite pressure from the gas on its two sides. (This is analogous to the little bit of string at rest feeling equal and opposite tension on its two sides, but of course the gas pressure is inward). As the sound wave goes through, the pressure wave generates slight differences in pressure on the two sides of our thin slice of air, and this imbalance of forces causes the slice to accelerate.

To analyze this quantitatively—to apply _{} to the thin slice of
air—we must begin by defining *displacement*,
the quantity corresponding to the string’s transverse movement _{}. We shall use _{} to denote the *horizontal* (along the pipe) displacement
of the thin slice of air which rests at position *x* when no sound is present.

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**An animated version of this diagram is available here!**

If the pipe has radius *a*,
and hence cross-sectional area _{}, a slice of air of thickness _{} has volume _{}, so writing the density of air _{} (1.29 kg/m^{3}),
the mass of the slice of air is _{}. Clearly, its
acceleration is _{}, so we already have the right-hand side of _{}. To find the left
hand side—the force on the thin slice of air—we must find the pressure
imbalance between the two sides.

The pressure change as
the sound wave moves down the tube is directly tied to the local
compression or expansion of the gas.
It’s like a spring: as the gas is compressed into a smaller volume, its
pressure rises, and as the gas expands the pressure drops. And, exactly as for a spring, the changes in
pressure and volume are linearly related.
The coefficient of proportionality is called the ** bulk modulus**, usually
written

_{}

*Note the sign*! As the volume decreases, the pressure
increases. Since the ratio of volumes is
dimensionless, the units for the bulk modulus are the same as for pressure:
Pascals. For air at standard temperature
and pressure, the bulk modulus *B* = 10^{5}

Now, we are tracking the motion of the gas as the sound wave
passes through by following the parameter_{}the displacement along the tube at time *t* of gas having equilibrium position *x*. Obviously, if _{} does not depend on *x*, all the gas is shifted by the same amount,
and no compression or expansion has taken place. Local change in volume *only* happens if there is local *variation*
in _{}.

To make this quantitative, consider a slice of gas having
thickness _{}(when at rest): if, at some instant when the sound wave is
passing through, the right-hand end is displaced by_{}, and the left-hand end by a greater amount_{}, say,

the thickness of the slice has evidently been changed from _{} to

_{}

Since the volume of air in the slice is directly
proportional to its thickness, the sound wave has at this instant changed the* volume* of the air initially in the
segment _{}near the point *x*
by a fraction

_{}

the differential being exact in the limit of a thin slice.

Therefore, *the local
extra pressure is directly proportional to minus the gradient of *_{}:

_{}.

Having
found how the local pressure variation relates to_{}, we’re ready to derive the wave equation from *F* = *ma*
for a thin slice of gas. Recall that for
such a slice_{}, and of course _{}.

The net force *F* on
the slice is the difference between the pressure at *x* and that at _{}:

_{}.

Putting this into *F*
= *ma*:

_{}

This is exactly the wave equation we found for the string,
with now the longitudinal displacement *s *replacing
the transverse displacement *y*, and the
bulk modulus playing the role of the string tension, both being measures of
stored potential energy arising from local variations in displacement. The densities, of course, play the same role
in the two cases, measuring how much *kinetic*
energy is stored for given local displacement velocities.

Since the new wave equation is identical in form to that for waves on a string, our discussion of traveling waves, standing waves, etc., for a string can be carried over with the appropriate changes of notation and applied here.

For example, a standing wave in a pipe has the form _{}, this would be for a pipe *closed* at *x* = 0, so that
the air doesn’t move at *x* = 0.

The boundary condition for a closed end of a pipe is:

_{}

What about an *open*
end? In that case, the air is free to
move—the boundary condition won’t be _{} However, the pressure
is *not* free to vary: it’s atmospheric
pressure, the pipe being open to the atmosphere.

So at an open end _{}

Remembering that _{} the boundary condition
is:

_{}

Consider now a standing harmonic wave in a pipe of length *L*, *closed
*at *x* = 0 but *open* at *x* = *L*.

From the *x* = 0
boundary condition, the wave must have the form
_{}.

The *x* = *L* open end boundary condition requires
that the slope _{}

That is, _{}

*Exercise*: Prove that the longest wavelength
standing wave possible in the pipe has wavelength 4*L*, and sketch the wave.

*Exercise*: what is the *next* longest wavelength of a possible standing wave in the
pipe? Draw a picture.

Another solution to the wave equation is

_{}

where _{}, just as for
string. This is a wave traveling down
the pipe. It could be generated by an oscillating
plate at the closed end: in other words,
a speaker.

How much **power** is this
speaker putting out? It’s moving and
pushing against the pressure:

**Power = P = rate of
working = force **

How fast is it moving?
At time *t*, the plate is at

_{}

so it is moving at velocity

_{}

The pressure at the plate is_{}where

_{}

at *x* = 0.

So the rate of working at time *t*, the power *P*(*t*)
= velocity x
force:

_{}

*The standard
definition of power for any kind of wave generator is the average power over a complete cycle. *

Since the average value of cos^{2}*x* = ½,

_{}.

Using _{} and _{}, this can be written

_{}

** This also tells us how much energy there is in the
wave as it travels**:

_{} per meter.

The *intensity** *of the wave is ** average power per square meter of cross
sectional area**, so here

_{}

and *I* is measures in *watts per square meter*.

The factor *v*, the
velocity, in the above expression comes about because in one second, the energy
delivered by a steady sound wave to one square meter of area perpendicular to
the direction of the wave’s motion is the energy in *v* cubic meters of wave: taking the speed of sound to be 330 meters
per second, 330 cubic meters of sound energy will plough into one square meter
each second.