Section 1-11 - Waves and Sound

Speed of Mechanical Waves
Reflections of Pulses
Sinusoidal Waves
Properties of a Wave
Standing Waves
Non-Sinusoidal Waves
Intensity
Beats
Doppler Effect
Notes: Sound in Solids, Trig Identity
Correlation to your Textbook

Speed of Mechanical Waves

We covered single oscillators in Section 1-10.  For the specific example of a mass/spring system, we saw that there is a natural frequency at which the system would 'like' to oscillate, given by wo = [k/m]1/2, or rather, the period T = 2p[m/k]1/2.  Now, let's consider a chain of such oscillators, identical masses connected by identical springs:

If we apply a disturbing impulse to the end oscillator, it will move to the right, applying its own force on the next mass, et c.  The speed of this disturbance as it moves down the chain of oscillators should depend inversely on the period of oscillation of each mass, i.e., be proportional to the natural frequency [k/m]1/2.   We can guess, then, that the speed of any mechanical wave in a material should be proportional to [elastic property of material/inertial property of material]1/2.  For example, the speed of a sound pulse in a solid is found experimentally to be v = [Y/r]1/2, where Y is the Young's modulus, a measure of the springiness of the material, and r is the mass density of the material (inertial property).  See below for a more mathematical justification of this relationship.  The speed of sound in a fluid (like air) also follows this form: v = [B/r]1/2, where B is the bulk modulus, a measure of the elastic properties of a fluid.

Derivation for the specific case of a chain of oscillators:

Let x be the equilibrium position of each mass.  The masses are separated at equilibrium by distance D.  Let y(x, t) be the displacement of each mass from its proper position.
Consider Newton's Second Law for the mass at position x + D.
Fx+D = max+D = m d2y/dt2|x+D

NB Here I use delta to indicate a partial derivative.

The force is due to the springs on either side of the mass (Hooke's Law), but the amount each spring is stretched or compressed depends on the locations of both of the masses:
Fx+D = k[y(x+2D, t) - y(x+D, t)] - k[y(x+D, t) - y(x, t)]

Combine these expressions, divide each side by m, factor the k, and multiply the right side by D2/D2:

d2y/dt2|x+D = [D2 k/m]  [[y(x+2D, t) - y(x+D, t)]/D - [y(x+D, t) - y(x, t)]/D]/D
Now, let's define some new quantities:
KEFF = k/N is the effective spring constant for N of the oscillators.
L = ND is the length of the chain of N oscillators.
M = Nm is the mass of N oscillators.
So,
d2y/dt2|x+D = [KEFFL2/M]  [[y(x+2D, t) - y(x+D, t)]/D - [y(x+D, t) - y(x, t)]/D]/D

Now, let's smooth the system out by taking a limit D-> 0 by letting N go to infinity while D and m go to zero:

lim D-> 0 d2y/dt2|x+D = [KEFFL2/M]  lim D-> 0 [[y(x+2D, t) - y(x+D, t)]/D - [y(x+D, t) - y(x, t)]/D]/D

The expression in red then becomes the derivative of y wrt x, evaluated at x+D, and the blue expression is the derivative of y at x.  The left side simply becomes the second derivative at x.
d2y/dt2|x = [KEFFL2/M]  lim D-> 0 [dy/dx|x+D - dy/dx|x]/D

The limit that remains is the derivative wrt x of the derivative of y, or in other words, the second derivative of y wrt x evaluated at x:

d2y/dt2|x = [KEFFL2/M]  d2y/dx|2x

This then results in a version of the wave equation:
d2y/dx2 = [M/KEFFL2] d2y/dt2.

We'll come back to this result in a while.


Properties of a Wave

Let's consider a disturbance that repeats itself at regular intervals.  Instead of pulses, the driving force at the end of the medium in which the disturbance travels is periodic, i.e., it repeats its motion in a given amount of time, T.  Now, the wave which is produced will have the same frequency as the driving force, even though the speed of propagation will be determined by the natural frequency of the individual oscillations (yet to be proven).  Mechanical waves in general are often classified as longitudinal or transverse.  Waves in which the individual pieces of the medium move along the same line as the direction of propagation of the wave are referred to as longitudinal, while waves in which each piece of material moves along a line perpendicular to the direction of propagation, such as on a taut string, are called transverse.  We demonstrated each of these with the slinky.


We describe waves using several quantities:


There is a relationship among  f, l, and v, which we can deduce from the 'railcar analogy.'

Suppose that a train with cars of length L passes you at speed v.  You count N cars in time t.  The distance traveled by the train in that time is NL.  The speed of the train is v = d/t = (NL)/t = (N/t)L.  We recognize (N/t) as the frequency f and L as the analog of l, so v = fl.

Sinusoidal Waves

Let's consider a special case in which the driving force is sinusoidal.  

Although we won't prove it, sinusoidal waves are described mathematically by the expression:
y(x,t) = A sin(2px/l -/+ 2pf t + f),
where f is a phase angle which allows us to change the function to cosine or to some combination of sine and cosine.  This is sometimes written this way:
y(x,t) = A sin(kx -/+ wt + f).
The quantity k above is the magnitude of the wave vector, which is then 2p/l. In both cases, the negative sign indicates a wave moving the the right (positive x) and the plus sign indicates that the wave is moving toward the left.

Let's check this out.  If we choose a particular time, then the function looks like this (here, I'm combining the now constant time term with the phase angle and renaming the combination as a new phase angle):
y(x) = Asin(2px/l + f'),
that is, a snap shot of the wave at that instant.  We see that the wave has a sinusoidal shape with regard to position, x, and that as x increases by one wavelength, the function advances by one cycle.
On the other hand, if we look at what's happening at a particular location x (again, I'll include the now constant spatial term into a new phase angle), the function looks like this:
y(t) = Asin(wt +f"),
that is, that piece of the medium at that particular location undergoes simple harmonic motion.  These results are at least consistent with our notions about the wave.

We see that the wave has a combined spatial and temporal dependence, since both x and t occur in the argument of the sine function.  How does this correspond to a moving wave?  The crest (for example) of the wave will occur when the argument of the sine function equals p/2 radians (or p/2 + 2np, n an interger, depending on exactly which peak we want to consider):
kx - wt + f = p/2.
The position x at which this peak occurs is then given by
x = [p/2 - f]/k+ [w/k]t,
so that, as time progresses, the location x of the crest must become more positive, that is, the crest moves to the right.  If the sign between the two terms had been positive instead, then the value for x would have to become more negative as t increases, so that the crest moves to the left.

NOTE: Even though we are using transverse waves on a string as our model for wave behaviour, these properties can be ascribed to just about any type of mechanical wave.  We just let the displacement from equilibrium represent, for example, the deviations from atmospheric pressure (for sound) or angular displacement (for torsional waves).  We can even talk about variations in the strengths of electric and magnetic fields in this way.

Now, let's see if our sinusoidal wave function is a solution to the wave equation:

 y(x,t) = A sin(2px/l -/+ 2pf t + f),

dy/dx = [A2p/l] cos(2px/l -/+ 2pf t + f)
d2y/dx2 = -A[2p/l]2 sin(2px/l -/+ 2pf t + f)
l2 d2y/dx2 = -A[2p]2 sin(2px/l -/+ 2pf t + f)

dy/dt = -/+ [A 2pf] cos(2px/l -/+ 2pf t + f)
d2y/dt2 = -A[2pf]2 sin(2px/l -/+ 2pf t + f)
f  -2 d2y/dt2 = -A[2p]2 sin(2px/l -/+ 2pf t + f)

Equating the last two results:
l2 d2y/dx2 = f  -2 d2y/dt2
d2y/dx2 = [lf]  -2 d2y/dt2
You may remember that lf is the wave's velocity, so our wave equation becomes:
d2y/dx2 = [v] -2 d2y/dt2
So, the constant of proportionality is the square of the wave's velocity.  This will be true for any type of wave we study.  Is it restricted to waves that are sine or cosine functions?  No.  We will make use of a technique called Fourier decomposition and argue that any well behaved wave shape can be written as a sum of sine and cosine terms, each of which independently solves this wave equation.

Non-Sinusoidal Waves

We've been concentrating on sinusoidal waves.  What about waves that are not sinusoidal?  Most wave shapes can be approximated by adding up different amplitudes of many sinusoidal waves of different frequencies (Fourier decomposition):
Y(t) ~ Sn An sin(nwt)   with n = 1, 2, 3, ...
We can represent these amplitudes An graphically with a figure like this one, similar to what was shown on the screen of the spectrum analyzer).
For example, a 'ramp' wave is composed of waves with the form An sin(nwt) with n = 1, 2, 3, ... and the amplitude An decreasing as 1/n.


Or, a square wave is the sum of waves of the form An sin(nwt) with n = 1, 3, 5, ... and the amplitude An decreasing as 1/n.

Or, a triangular wave is the sum of waves of the form An sin(nwt) with n = 1, 3, 5, ... and the amplitude An decreasing as 1/n2.
Go to the Excel workbook again and try some combinations of harmonics to see if you can duplicate these waveforms on the Fourier Demo worksheet.  Enter the amplitudes of the various harmonics and observe the resulting wave shape.

To wrap it all up, the functions describing waves, in one dimension at least, generally are solutions to the wave equation:
d2y/dx2 = [v] -2 d2y/dt2.


Special case - tranverse waves on a string

Consider a small length Dx of string a distance x from the end on which a transverse wave is traveling.

The mass of this small piece of string is m.  The forces acting on m are shown in the figure above.  Each end of m is pulled by the adjacent piece of string along a line tangent to the string at the end (T1 and T2).  Each of these forces can be broken up into components; since we do not expect any motion in the horizontal direction, those components (T) should cancel, and individually should be equal to the tension in the string.  The vertical components will act to accelerate m.  Let's find them:
T1y / T = tanq1     T2y / T = tanq2
Let's remember that the tangents of these angles are the slopes of the curves at those points, so
T1y / T = dy/dx|x     T2y / T = dy/dx|x+Dx
Use NII:
Si Fyi  = may
T2y - T1y = T [dy/dx|x+Dx - dy/dx|x] = m d2y/dt2
Divide both sides by T Dx.
[dy/dx|x+Dx - dy/dx|x]/Dx = [m/TDx] d2y/dt2       Note that m/Dx is the linear mass density, l.  To avoid confusion in this section, however, we will use m = m/Dx.
Take the limit of Dx -> 0.  We've already seen an example of this; the left side becomes the second derivative of y wrt x.
d2y/dx2 = [m/T]   d2y/dt2
Comparison with previous results then indicates that the speed of this wave along the string is
v = [T/m]1/2.



Reflections

We next looked at reflections of pulses in a string.  We noted that a pulse traveling down the string is reflected with the same orientation if the end of the string is free to move, and reflected with an inverted orientation if the end of the string is fixed.  Although this could be proven mathematically, we based our assertion on experiment.  We can visualize what's happening, however, by imagining that the string continues beyond its actual end, and that an imaginary wave is traveling back down the string towards the end from the imaginary side.  We invoke the principle of superposition, the notion that the total displacement of the medium is the sum of the individual displacements due to each pulse; in this way, we know that the reflected pulse for a fixed end must be inverted, since this is the only way the total displacement at the end of the string can always be zero, and then clearly, the wave and its reflection must add together in the case of a free end.

I have no animation for this yet, but download this Excel workbook, go to the 'reflection demo', choose 'Enable Macros,' and press 'Ctrl Z' to advance the simulations.  The dark line represents the actual string, the coloured lines the real and imaginary pulses on it.  Reset the demo by pressing 'Esc' and typing '0' in the black box.

Now, instead of considering the two extreme cases (completely fixed or completely free ends), think about what would happen if the string were tied to another string.  In all cases, we would expect that some of the wave would continue down the second string with the same orientation (and frequency) as the original wave; this is called the transmitted wave.  We also notice that there is a reflected wave, the orientation (and size) of which depends on whether (and by how much) the second string is 'heavier' or 'lighter' than the first.  The quantity used to measure the difficulty of a wave in passing through some medium is called the impedance, Z.  If Z2>Z1, the reflected wave is inverted; if Z2<Z1, the reflected wave is upright.  This is a general result, even though the exact values of the impedances are calculated in different ways for different media.  In the specific example of transverse waves on a string, we have that (asserted without proof)
Z = [Tm]1/2.
In that case, we see that our original examples correspond to Z = 0 (end of string loose, so m2 = 0) and Z = infinity (end of string tied to wall, so m2 = infinity).

What would happen if the two media had the same impedance?

The impedances also tell us how much energy is reflected and how much is transmitted:
Some other day....


Standing Waves

The principle of superposition states that, if more than one wave is passing through a givien point, the total displacement is the linear sum of the displacements due to each individual wave.
Suppose that we set up two sinusoidal waves in a (one dimensional) medium which are identical in every way except their directions.  An example would be two waves moving along a very long string, each end being jiggled at the same amplitude and frequency.  What happens when these waves meet?  (In class, we made use of a wave I generated in the string, and that wave's reflection.
We use the principle of superposition to find the result by adding the two individual waves.  We saw that the resulting wave did not appear to travel at all; this type of wave is called a standing wave.  Let's examine this more mathematically:
y1  = A sin(kx - wt) and y2  = A sin(kx + wt).
ytotal = y1 + y2 = A sin(kx - wt) + A sin(kx + wt).
ytotal = A [sin(kx) cos(wt) - cos(kx) sin(wt)] + A [sin(kx)cos(wt) + cos(kx) sin(wt)],
where we have used the trig identity sin(a + b) = sin(a) cos(b) + cos(a) sin(b).
Re-arranging results in
ytotal = 2A sin(kx) cos(wt).
Here, we see that, in contrast to the original waves which had mixed spatial and temporal components, this wave has separate spatial and temporal components.  Each piece of the medium undergoes SHM, but with an amplitude which depends on its position.
y = [2A sin(kx)] cos(wt).
We can see that there are spots which never oscillate (nodes) and spots which have maximum oscillation (anti-nodes).  Each type of location is separated from its adjacent neighbour by one-half of the wavelength.

In our class demonstration, we used reflected waves as the second wave.  But in systems with finite length, there will be many reflections from each end which will have to be added to determine the overall shape of the string.  We started with a string fixed at each end, and we excited the waves with different frequencies.  In some cases, we noted that the waves all added up to a random pattern, eventually canceling out.  In other cases, we saw that the intial and reflected waved added to produce a standing wave.  What conditions need to be met to do this?  We could do a very mathematical derivation of this, but it is just as correct to base our investigation on the experimental data.

String fixed both ends:
We saw a series of patterns like those shown below as we increased the frequency at which the system was excited.  The lines indicate the limits of the oscillations of the string (the envelope).

We noticed that in each case, the length of the string L was a positive integer multiple of half of the wavelength,
L = nl/2, n = 1, 2, 3, ....
We can convert that to frequency by remembering that f = v/l, so that
f n = nv/2L.
We do the demonstration again with one end free, and find patterns like these:

such that L = nl/4, n = 1, 3, 5, ..., which then becomes f n = nv/4L.
Lastly, we image what might happen if we could have a string free at each end. This might seem impossible, but remember that we can use the concept for a number of other systems which do meet this criterion, for example, sound waves in a tube open at each end where the air is free to vibrate back and forth.

We see that the results here are identical to the case of fixed both ends, just with the positions of the nodes and anti-nodes exchanged.

We see that, unlike for a single oscillator with a single natural frequency, we here have a system with many natural frequencies:

Remember that, even though we derived these results for transverse waves on a string, the results are valid for other system.  For example, consider a stopped organ pipe, which means that it is open at one end and closed off at the other.  At the open end, air is free to vibrate, while at the closed end, no vibration is possible because of the stopper.  This pipe will support standing waves of the form f n = nv/4L, n  = 1, 3, 5, ....  How are these frequencies produced?  In an organ , air is pumped into the pipe against a sharp edge, which produces all frequencies.  However, those frequencies which do not correspond to the favoured frequencies reflect back and forth in the pipe and, on average, cancel themselves.  But the few special frequencies re-inforce one another and produce standing waves.  These frequencies are often referred to as the harmonics of the system.  On occasion, they are referred to as the fundamental (n = 1) and the overtones (n > 1).

Now here's a question.  How can a listener distinguish different musical instruments which are playing the same note?  For example, an oboe and a clarinet are both essentially cylindrical tubes, closed at one end and open at the other, and so they produce the same sequence of harmonics, fn = nv/4L.  The answer is that they each put slightly different amounts of energy into the different harmonics, and it is that distribution that your brain remembers and labels as one instrument or the other (see below).
FIGURE

Also, it is possible to suppress certain harmonics.  For example, we managed to suppress all odd harmonics on a string fixed at both ends simply by grabbing the middle of the string, thus forcing a node to form there; any harmonics which do not have a node there do not form.  We also investigated the suppression of harmonics in an aluminum rod; by grasping the rod at different points, we could make the sound the rod makes when struck different.  This technique is used in the forked fingerings of woodwinds, and in the 'nodal vents' used in some reproduction natural trumpets.

Intensity

A wave can be defined as a transfer of energy without a net movement of matter.  For sound (and later, light), we measure the rate of energy transfer per unit area as the intensity, I, with the corresponding units of watts/m2.  Consider a fire siren which broadcasts isotropically P joules of sound energy per second.  Draw an imaginary sphere of radius R with the centre at the siren; all the energy must pass through that sphere, and the intensity will be
I = P/4pR2.
We see that if we make the sphere larger, the energy will be distributed over a larger area, and the intensity will be reduced (that is, each square metre of area will receive less energy).  This 1/r2 dependence is fairly common, and we shall see it again.

An alternate way of expressing intensity is in units of decibels.  The decibel scale is is logarithmic, and thus follows more closely the actual size of the signal sent from human ear to human brain.  The bel is named for Alexander Graham Bell, who was not, as one might suppose, American, but rather a Scot-born Canadian working in Boston.  A reference intensity Io is defined as 10-12 wts/m2, which corresponds roughly to the quietest sound a normal human can hear.  The intensity to be converted is compared to this standard, and the log base ten is taken of the ratio.  This gives the number of bels, so the number of decibels (dB) must be ten times more:
b = 10 log10[I/Io].
Let's try some examples:
Suppose that the sound that one professor produces (at a given distance) has an intensity of 10-7 wts/m2.  How many dB does this correspond to?


Now, how many decibels would ten professors produce? What about one hundred?

So, note that this is not a linear relationship.  A multiplicative factor of ten in intensity is an additive increase of ten in decibels.

Note: we assume that we can simply add the intensities of individual waves.  This works so  long as those individual waves are incoherent.  When waves are coherent, a more difficult approach is necessary (which we'll investigate in the second semestre).  Please, no comments about how professors are always incoherent.

Here are the intensity levels of some common situations:
Situation Intensity Intensity level
Threshold of Hearing 10-12 W/m2 0 dB
Library Reading Room 10-9 W/m2 30 dB
Conversation 10-6 W/m2 60 dB
Vacuum Cleaner 10-3 W/m2 90 dB
Rock Concert 10-1 W/m2 110 dB
Thunder 10 W/m2 130 dB
Of course, these values depend on the distance between source and listener.  Prolonged exposure to sounds above 90dB will cause permanent damage, and exposure to sounds over 110dB will be painful.  Here are some helpful hints: ALWAYS wear ear protection in noisy situations, such as lawn mowing or vacuuming and on up.  If you must wear headphones to listen to music, place them just in front of your ears, not right over them.


Beats

Suppose that we have two nearly identical waves passing through a spot in space, so that the time dependences (we'll ignore the spatial dependence for now) are given by:
Y1 = Ao sin(2pf1t)
Y2 = Ao sin(2p f2 t).
Using the principle of superposition, we get that total 'displacement' from equilibrium is then the sum of these two expressions:
Ytotal = Y1 + Y2 = Ao sin(2pf1t) + Ao sin(2pf2 t).

Now, we'll make use of a trig identity, (which we'll prove below):
sin a + sin b = 2 sin[(a+b)/2] cos[(a-b)/2],
so that
Ytotal =  2 Ao cos(2p[(f1- f2)/2]t) sin(2p[(f1+ f2)/2]t).
From this we see that the frequency of oscillation is the average of the two original frequencies, but also that the amplitude of the oscillation is modulated by an envelope with a frequency of | f1f2|/2.  What will be heard, though is a pulsing or beating in the amplitude with twice that frequency; this is known in fact as the beat frequency:
 fBeat =  | f1 - f2|.

This can be (and often is) used as a method for tuning pianos and other such instruments.  Once a 'C' string is tuned to the correct pitch, it and the 'G' a fifth above it above are struck simultaneously.  The third harmonic of the C and the second harmonic of the G are the same note, and so the G string's tension is adjusted until no beats are heard between those two harmonics (or in other tuning schemes, a certain number of beats per second should be heard, but that's a whole 'nother story...).


Doppler Effect

You're probably familiar with this effect: a car or train paasses you while blowing its horn, so that the pitch of the sound rises while the vehicle is moving toward you, but sounds lower when the vehicle is moving away from you.  We shall look at a couple of special cases, and then integrate the results for all such cases into a single relationship.  Note, however, that the results will only be true if there is no wind, that is, the medium (usually air or water) is stationary.  Also, our derivations will be done for a one dimensional universe.

Consider a source moving at speed vSource toward (approaching) a stationary observer (or listener, if you insist).  Instead of having the source emit a sinusoidal wave, let's assume that it emits pulses; we can later correlate these pulses to the peaks of a sinusoidal wave, if necessary.  Let the frequency of the pulse emitted by the source be fo, and the time between the emission of pulses be To = 1/ fo.
Here at t = 0, the source releases a pulse, which then travels to the right at speed vSound.

Now, let's look at the locations of everything a time t = To later:

Here, at a time To later, Pulse 1 has traveled a distance
dSound = vSound To,
while the source has traveled a distance
dSource = vSource To,
at which point it emits Pulse 2.
Now, the wavelength that the observer will measure is the distance between the two pulses:
l' = dSound - d Source
l' = vSound To vSource To.
Now we remember that, in general,  f  = 1/T and that fl = vwave, and so this last expression can be re-written as
vSound/ f ' = vSound/fo - vSource/ fo,
which get re-arranged to be
 f ' =  f o [vSound/(vSound - vSource)].
Now, if the source had instead been moving the other way (receding), those two distances would have had to have been added, changing the red minus sign to a plus sign:
 f ' =  f o [vSound/(vSound + vSource)].

Now, suppose instead that it were the observer moving toward (approaching) the stationary source at speed vObserver.  Once again, let the source emit pulses at an interval of To.  Let t = 0 when Pulse 1 arrives at the observer:

The second pulse arrives at the observer at time T', during which interval the pulse has traveled distance (to the right)
dSound = vSound T'
and the observer has traveled distance (to the left)
dObserver = vObserver T'.
T' is now the time between pulses, as heard by the observer.
The sum of these distances is the old wavelength, lo:
lo = dSound + dObserver = vSound T' + vObserver T'.
Once again remembering that, in general,  f  = 1/T and that  f l = vwave, we substiute to obtain
vSound/ f o  = vSound/ f ' + vObserver/ f '.
This, we re-arrange to obtain
 f ' =  f o [vSound + vObserver]/vSound.
Once again, if the observer had been receding from the source, there would have been a sign reversal (blue) to
 f ' =  f o [vSound - vObserver]/vSound.

Now, we can combine all these relationships, if we're careful.  First, we need to define better the terms 'approach' and 'recede.' 'Approach' is to head in the direction of the other object, regardless of whether the distance between the objects is becoming smaller or not, and 'recede' means to head in the opposite direction of the other object, whether the distance between is increasing or not.  Then
f' = fo [vSound +/- vObserver]/[vSound -/+ vSource],
where the upper sign is used if that object is approaching and the lower sign if that object is receding.

What exactly would one do if there were wind?


NOTE: For light, the result is very different.

What happens if the source travels more quickly than sound?  Consider these diagrams:

The upper left figure shows the locations of the crests of three waves emitted by a source such as a jet while it is stationary.  The upper right figure shows the the same when the source is moving to the right at about 0.5 the speed of sound; note that the wavelengths will be shorter for listeners in the path of the source, but longer for listeners from which the source is receding.  When the source reaches the speed of the wave in that medium, a bow shock wave is generated; this is most easily seen when generated by a boat, but recent photos of jets breaking the 'sound barrier' have caught these shock waves as they condensed water vapour in the air.  Once the speed of the source exceeds the speed of the wave in that medium, the crests of all waves co-incide to produce a giant shock wave (red line); for jets, this results in the familiar sonic boom.

Some random notes:
1) The reason the Concorde was so quiet (to the passengers anyway, not to those living on the flight path) during supersonic flight is that the the noise from the engines could not keep up with the cabin; one could hear only the noise transmitted through the body of the plane.
2) The apex angle (2q) of the cone formed by the shockwave depends on the speed of the source:

The wave shown was generated at the instant that the source was at its centre.  In time interval t, the source moved a distance vsourcet and the sound moved outward a distance vsoundt.  Consider the right triangle formed in the diagram.  We see that
sinq = vsoundt/vsourcet = vsound/vsource.
The inverse of this ratio is referred to as the Mach number.  The official speed record of any jet aircraft is about Mach 3, set by a Soviet fighter.  There are rumours however that the US's SR-71 has hit Mach 5.  The Space Shuttle enters earth's atmosphere at about Mach 25.



We would like to justify the contention that the speed of a disturbance propagates with a speed that is related to the natural frequency of the individual oscillators.

Consider a rectangular block of a solid, length L and cross-sectional area A.  The material can be modelled by small balls of mass m (representing the atoms) connected by bonds represented by springs with stiffness k, and relaxed length lo.  We can justify this last statement by examining the typical potential energy curve of these bonds:

The atoms would 'like' to arrange themselves so that the potential energy is a minimum, at r = lo.  At that point, the shape of the curve is approximately parabolic, and so the system follows Hooke's law,
F1 = - 2k(r-lo) = - 2k Dl,
where F1 approximately represents the x-component of the force on one atom from two adjacent atoms (the problem is actually more complicated than this, even, since the amount of stretching or compression of any spring depends on the positions of both of the masses to which it's connected.).  Now, we remember that the Young's modulus is given experimentally and macroscopically by
Y = -(F/A)/(DL/L),
where F/A is the pressure exerted on each end of the material, and DL/L is the resulting fractional change in length.  We assert that DL/L = Dl/lo, since we assume that any change of the dimensions (during equilibrium compression or stretching ) is evenly divided among all of the bonds.  Also, the pressure F/A is the same for the whole face of the metal as for the area corresponding to one atom, F1/lo2.  So,
Y = -(F/A)/(DL/L) = -(F1/lo2)/(Dl/lo) = -(F1/Dl)/lo = +2k/lo.
In the same way, the density can be found with the mass of one atom and the volume that atom occupies on average:
r = m/lo3.
We know also from macroscopic experimentation that the speed of sound in a solid is given by
v = [Y/r]1/2
So, we then show that
v = [Y/r]1/2 = [2k/lo/m/lo3]1/2 = [2]1/2 lo [k/m]1/2
So, as asserted, the speed of propagation is proportional to the frequency of the individual oscillators:
v ~ wo.
Does this make sense?  In general, v = d/t = lo/(0.11T).  Yes, the disturbance travels one spring length in an appreciable fraction of the mass's oscillation period.


Trig Identity

We want to find sin a + sin b.
Let a = [a + b]/2 and b = [a - b]/2.
Then, a + b = (a/2 + b/2) + (a/2  - b/2) = a
and  a - b = (a/2 + b/2) - (a/2  - b/2) = b.
So, sin a = sin(a + b) = sina cosb + sinb cosa
and
sin b = sin (a - b) = sina cosb - sinb cosa.
So, sin a + sin b = sina cosb + sinb cosa + sina cosb - sinb cosa = 2 sina cosb = 2 sin([a + b]/2) cos([a - b]/2)




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D Baum 2000