The wave equation is
  | 
(1) | 
 
where 
 is the Laplacian.
The 1-D wave equation is
  | 
(2) | 
 
In order to specify a wave, the equation is subject to boundary conditions
  | 
(3) | 
 
 
  | 
(4) | 
 
and initial conditions
The wave equation can be solved using the so-called d'Alembert's solution, a  Fourier Transform method, or
Separation of Variables.
d'Alembert 
 devised his solution in 1746, and Euler 
 subsequently expanded the method in 1748.  Let
  | 
(7) | 
 
  | 
(8) | 
 
By the Chain Rule,
  | 
(9) | 
 
  | 
(10) | 
 
The wave equation then becomes
  | 
(11) | 
 
Any solution of this equation is of the form
  | 
(12) | 
 
where 
 and 
 are any functions.  They represent two waveforms traveling in opposite directions, 
 in the
Negative 
 direction and 
 in the Positive 
 direction.
The 1-D wave equation can also be solved by applying a Fourier Transform to each side,
  | 
(13) | 
 
which is given, with the help of the Fourier Transform Derivative identity, by
  | 
(14) | 
 
where
![\begin{displaymath}
\Psi(k,t) \equiv {\mathcal F}[\psi(x,t)] = \int_{-\infty}^\infty \psi(x,t)e^{-2\pi ikx}\,dx.
\end{displaymath}](w_165.gif)  | 
(15) | 
 
This has solution
  | 
(16) | 
 
Taking the inverse Fourier Transform gives
where
![\begin{displaymath}
f_1(u)\equiv {\mathcal F}[A(k)] = \int_{-\infty}^\infty A(k)e^{-2\pi iku}\,dk
\end{displaymath}](w_172.gif)  | 
(18) | 
 
![\begin{displaymath}
f_2(u)\equiv {\mathcal F}[B(k)] = \int_{-\infty}^\infty B(k)e^{-2\pi iku}\,dk.
\end{displaymath}](w_173.gif)  | 
(19) | 
 
This solution is still subject to all other initial and boundary conditions.
The 1-D wave equation can be solved by Separation of Variables using a trial solution
  | 
(20) | 
 
This gives
  | 
(21) | 
 
 
  | 
(22) | 
 
So the solution for 
 is
  | 
(23) | 
 
Rewriting (22) gives
  | 
(24) | 
 
so the solution for 
 is
  | 
(25) | 
 
where 
.  Applying the boundary conditions 
 to (23) gives
  | 
(26) | 
 
where 
 is an Integer. Plugging (23), (25) and (26) back in for 
 in (21) gives, for a
particular value of 
,
The initial condition 
 then gives 
, so (27) becomes
  | 
(28) | 
 
The general solution is a sum over all possible values of 
, so
  | 
(29) | 
 
Using Orthogonality of sines again,
  | 
(30) | 
 
where 
 is the Kronecker Delta defined by
  | 
(31) | 
 
gives 
so we have
  | 
(33) | 
 
The computation of 
s for specific initial distortions is derived in the Fourier Sine Series section.  We already have found
that 
, so the equation of motion for the string (29), with
  | 
(34) | 
 
is
  | 
(35) | 
 
where the 
 Coefficients are given by (33).
A damped 1-D wave
  | 
(36) | 
 
given boundary conditions
initial conditions
and the additional constraint
  | 
(41) | 
 
can also be solved as a Fourier Series.
![\begin{displaymath}
\psi(x,t) = \sum_{n=1}^\infty \sin\left({n\pi x\over L}\right)e^{-v^2bt/2} [a_n\sin(\mu_nt)+b_n\cos(\mu_nt)],
\end{displaymath}](w_211.gif)  | 
(42) | 
 
where
To find the motion of a rectangular membrane with sides of length 
 and 
 (in the absence of 
gravity 
), use the 2-D wave equation
  | 
(46) | 
 
where 
 is the vertical displacement of a point on the membrane at position (
) and time 
.  Use 
Separation of Variables to look for solutions of the form
  | 
(47) | 
 
Plugging (47) into (46) gives
  | 
(48) | 
 
where the partial derivatives have now become complete derivatives.  Multiplying (48) by 
 gives
  | 
(49) | 
 
The left and right sides must both be equal to a constant, so we can separate the equation by writing the right side as
  | 
(50) | 
 
This has solution
  | 
(51) | 
 
Plugging (50) back into (49),
  | 
(52) | 
 
which we can rewrite as
  | 
(53) | 
 
since the left and right sides again must both be equal to a constant. We can now separate out the 
 equation
  | 
(54) | 
 
where we have defined a new constant 
 satisfying
  | 
(55) | 
 
Equations (53) and (54) have solutions
  | 
(56) | 
 
 
  | 
(57) | 
 
We now apply the boundary conditions to (56) and (57).  The conditions 
 and 
 mean that
  | 
(58) | 
 
Similarly, the conditions 
 and 
 give 
 and 
, so 
and 
, where 
 and 
 are Integers.  Solving for the allowed values of 
 and 
 then gives
  | 
(59) | 
 
Plugging (52), (56), (57), (58), and (59) back into (22) gives the solution for particular
values of 
 and 
,
![\begin{displaymath}
z_{pq}(x,y,t) = [C_\omega\cos(\omega t)+D_\omega\sin(\omega ...
...)}\right]\left[{H_q\sin\left({q\pi y\over L_y}\right)}\right].
\end{displaymath}](w_251.gif)  | 
(60) | 
 
Lumping the constants together by writing 
 (we can do this since 
 is a function of
 and 
, so 
 can be written as 
) and 
, we obtain
  | 
(61) | 
 
Plots of the spatial part for modes (1, 1), (1, 2), (2, 1), and (2, 2) follow.
The general solution is a sum over all possible values of 
 and 
, so the final solution is
  | 
(62) | 
 
where 
 is defined by combining (55) and (59) to yield
  | 
(63) | 
 
Given the initial conditions 
 and 
, we can compute the 
s and
s explicitly.  To accomplish this, we make use of the orthogonality of the Sine function in the form
  | 
(64) | 
 
where 
 is the Kronecker Delta.
This can be demonstrated by direct Integration.  Let 
 so 
 in (64), then
  | 
(65) | 
 
Now use the trigonometric identity
![\begin{displaymath}
\sin\alpha\sin\beta ={\textstyle{1\over 2}}[\cos(\alpha-\beta)-\cos(\alpha+\beta)]
\end{displaymath}](w_270.gif)  | 
(66) | 
 
to write
![\begin{displaymath}
I = {L\over 2\pi} \int_0^\pi \cos[(m-n)u]\,du+\int_0^\pi \cos [(m+n)u]\,du.
\end{displaymath}](w_271.gif)  | 
(67) | 
 
Note that for an Integer 
, the following Integral vanishes
since 
 when 
 is an Integer.  Therefore, 
 when 
.  However, 
 does not
vanish when 
, since
  | 
(69) | 
 
We therefore have that 
, so we have derived (64).  Now we multiply 
 by two sine
terms and integrate between 0 and 
 and between 0 and 
,
![\begin{displaymath}
I=\int_0^{L_y}\left[{\int_0^{L_x} z(x,y,0)\sin\left({p\pi x\...
...L_x}\right)\,dx}\right]\sin\left({q\pi y\over L_y}\right)\,dy.
\end{displaymath}](w_284.gif)  | 
(70) | 
 
Now plug in 
, set 
, and prime the indices to distinguish them from the 
 and 
 in (70),
Making use of (64) in (71),
  | 
(72) | 
 
so the sums over 
 and 
 collapse to a single term
  | 
(73) | 
 
Equating (72) and (73) and solving for 
 then gives
![\begin{displaymath}
A_{pq} = {4\over L_xL_y} \int_0^{L_y}\left[{\int_0^{L_x} z(x...
...L_x}\right)\,dx}\right]\sin\left({q\pi y\over L_y}\right)\,dy.
\end{displaymath}](w_294.gif)  | 
(74) | 
 
An analogous derivation gives the 
s as
![\begin{displaymath}
B_{pq} = {4\over \omega_{pq}L_xL_y} \int_0^{L_y}\left[{\int_...
...L_x}\right)\,dx}\right]\sin\left({q\pi y\over L_y}\right)\,dy.
\end{displaymath}](w_295.gif)  | 
(75) | 
 
The equation of motion for a membrane shaped as a Right Isosceles Triangle of length
 on a side and with the sides oriented along the Positive 
 and 
 axes is given by
 
 | 
 | 
 
 | 
 | 
| 
 
  | 
(76) | 
where
  | 
(77) | 
 
and 
, 
 Integers with 
.  This solution can be obtained by subtracting two wave solutions for a
square membrane with the indices reversed.  Since points on the diagonal which are equidistant from the center must have the
same wave equation solution (by symmetry), this procedure gives a wavefunction which will vanish along the diagonal as
long as 
 and 
 are both Even or Odd.  We must further restrict the modes since those with 
 give
wavefunctions which are just the Negative of 
 and 
 give an identically zero wavefunction. The following
plots show (3, 1), (4, 2), (5, 1), and (5,3).
References
Abramowitz, M. and Stegun, C. A. (Eds.).  ``Wave Equation in Prolate and Oblate Spheroidal Coordinates.''  §21.5 in
  Handbook of Mathematical Functions with Formulas, Graphs, and Mathematical Tables, 9th printing.
  New York: Dover, pp. 752-753, 1972.
Morse, P. M. and Feshbach, H.  Methods of Theoretical Physics, Part I.  New York: McGraw-Hill, pp. 124-125, 1953.
© 1996-9 Eric W. Weisstein 
1999-05-26