
which impl ies
b
nv
l
; n 1; 2; 3; ...: 10:53
Note that n cannot be equal to zero, because it would make b 0, which in turn
would mak e u 0.
Substituting Eq. (10.53) into Eq. (10.51) we have
u
n
x; tsin
nx
l
C
n
sin
nvt
l
D
n
cos
nvt
l
; n 1 ; 2; 3; ...: 10:54
We see that there is an in®nite set of discrete values of b and that to each value of
b there corresponds a particular solution. Any linear combination of these parti-
cular solutions is also a solution:
u
n
x; t
X
1
n1
sin
nx
l
C
n
sin
nvt
l
D
n
cos
nvt
l
: 10:55
The constants C
n
and D
n
are ®xed by the boundary conditions (10.45) and
(10.46).
Application of boundary condition (10.45) yields
f x
X
1
n1
D
n
sin
nx
l
: 10:56
Similarly, application of boundary condition (10.46) gives
gx
v
l
X
1
n1
nC
n
sin
nx
l
: 10:57
The coecients C
n
and D
n
may then be determined by the Fourier series method:
D
n
2
l
Z
l
0
f xsin
nx
l
dx; C
n
2
nv
Z
l
0
gxsin
nx
l
dx: 10:58
We can use the method of separation of varia ble to solve the heat conduction
equation. W e shall leave this as a home work problem.
In the following sections, we shall consider two more methods for the solution
of linear partial diÿerential equations: the method of Green's functions, and the
method of the Laplace transformation which was used in Chapter 9 for the
solution of ordinary linear diÿerential equations with constant coecients.
Solution of Poisson's equation. Green's functions
The Green's function approach to boundary-value problems is a very powerful
technique. The ®eld at a point caused by a source can be considered to be the total
eÿect due to each ``unit'' (or elementary portion) of the source. If Gx; x
0
is the
404
PARTIAL DIFFERENTIAL EQUATIONS