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.
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.
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.
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.
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.
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....
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.
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?
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 |
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 | f1
- f2|/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...).
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?
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.
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.