Therefore
YES, f (x, y ) is harmonic
on all of ![]() |
Release from rest
Þ
q (x)
º 0.
The dAlembert solution
is therefore
A = 1 ,
B = –6 ,
C = 8
Þ
D = 36 - 4(8) = 4 > 0
Therefore
the PDE is hyperbolic. |
This is a homogeneous second order linear PDE with constant
coefficients, for which the d’Alembert method may be
used to find a general solution.
Applying the additional information:
The complete solution is therefore
A = 4 ,
B = 12 ,
C = 9
Þ
D = 144 - 4(4)(9) = 0
Therefore
the PDE is parabolic. |
where h(x, y) is any
non-trivial linear function of x and y that is
not a multiple of
A simple choice, such as
h(x, y) = x , will do.
Therefore one form of the complementary function is
The right side function is a constant (78), while the left
hand side involves only second partial derivatives.
The particular solution must therefore be some function
of x and y of second order only, so we try
The second partial derivatives of this trial particular solution
are
Substituting into the PDE we obtain
There is only one condition on the three constants.
We therefore have a free choice for two of the constants.
Choose b = 0 and c = a
26a = 78
a = 3
The particular solution is therefore
and the general solution is
In order to find the complete solution, we employ the
additional information:
The complete solution to the PDE is therefore
t is playing the role of y.
A = 4 ,
B = 0 ,
C = 0
Þ
D = 0 - 4(4)(0) = 0
This is also the PDE for heat diffusion. Therefore
the PDE is parabolic. |
From page 4.28 of the lecture notes (Example 4.5.1), the
complete solution of the heat equation (with the boundary
conditions of constant temperatures T1
and T2 at the ends
In this case k = 4, L = 100,
T1 = 0, T2 = 100
and f (x) = 2x –
(x/10)2.
The coefficients in the Fourier sine series become![]() ![]() ![]() ![]() | Integration by parts: |
The Fourier series for x converges rapidly.
The steady state solution is
Two snapshots of u (x, t):
[The Maple file used to generate these diagrams is available here.]
A = 4 ,
B = 4 ,
C = 1
Þ
D = 16 - 4(4) = 0
Therefore
the PDE is parabolic. |
Assume a complementary function of the form
where h(x, y) is any
non-trivial linear function of x and y that is
not a multiple of
A simple choice, such as
h(x, y) = x , will do.
Therefore one form of the general solution is
The functional forms of f and
g remain arbitrary in the absence of
any further information (such as boundary conditions).
Several alternatives are possible, such as
.
A = 1 ,
B = 0 ,
C = 1
Þ
D = 0 - 4(1) =
-4 < 0
Therefore
the PDE is elliptic. |
Assuming a complementary function of the form
uC = f
(ax+by) + g(ax+by),
Þ
uC(x, y) =
f (y - jx) +
g(y+jx)
Many possibilities exist for the particular integral.
Among them is:
Try uP(x, y)
=
c (x3 + y3)
Therefore the P.I. is uP(x, y)
= x3 + y3
and the general solution is
u(x, y) = f (y - jx) + g(y+jx) + x3 + y3 |
The functional forms of f and g remain arbitrary in the absence of any further information (such as boundary conditions).