
EXPANSIONS
WITH
EIGENFUNCTIONS
433
@
=1
@=-I
@
=1
@=-1
@
=1
a
/
@=-1
@
=I
@=-1
@
=1
@=-1
--bp
~-
Figure
11.7
Conversion
to
a
Periodic
Problem
in
the
x-Direction
sides
of
the shaded region to have
@
=
0.
Looking back on the previous example,
it is pretty easy to see that these requirements are met with the potential distribution
shown in Figure 1
1.7.
The solution inside the box is therefore identical to the solution
to the previous example with the x-periodicity equal to
26.
The only difference is, of
course, that this solution is only valid inside the region of the original
a
X
b
box of
Figure 11.5.
We successfully made this problem periodic
in
the x-direction. Could we have
done the same thing in the y-direction? Figure 11.8 shows what this would look like.
Again, we need to apply periodic potentials to the areas where the
?
marks occur in
the figure,
to
try
to force the horizontal sides of the shaded region to have
@
=
2
1.
It’s pretty obvious this cannot work. In
this
case, the x-direction must
be
chosen as
the periodic one.
An interesting twist is added
to
this problem if we modify the boundary conditions,
as
shown in Figure
1
1.9. In a case llke this, you will find it is impossible to simply
make either the
x-
or
y-direction periodic. Instead, the problem must be broken up
into two parts,
as
shown in Figure 11.10, Because Laplace’s Equation
is
linear, the
solution can be written as the
sum
of two solutions,
@I
(x,
y) and
@*(x,
y),
which
each satisfy modified boundary conditions shown
for
the two boxes on the right. The
function
@~(x,
y)
satisfies Laplace’s equation and has boundary conditions which are
amenable
to
periodic extension in the x-direction. The function
@(x,
y) also satisfies
Laplace’s equation, but with conditions which can be extended in the y-direction.
The combination
Q1(x,
y)
+
Q2(x,
y)
=
@(x,
y) satisfies Laplace’s equation inside
the box and satisfies the original boundary conditions of Figure 1
1.9.
11.2
EXPANSIONS WITH ELGENFUNCTIONS
Before looking at solutions to Laplace’s equation in other coordinate systems, we need
to establish some general techniques for expanding functions with linear summations
of
orthogonal functions. In the Cartesian problems we have discussed
so
far, we found
that we could evaluate the individual amplitude constants in the general solution by
using Fourier series type orthogonality conditions.
This
worked because the terms in
our sums
of
the general solution contained sine and cosine functions. In this section,
we will generalize this technique for other problems. We will begin by reviewing the