26.7 Physical Examples 631
26.7 Physical Examples
The most common physical problems involving Laplace’s equation are those
from electrostatics in empty space, and steady-state heat transfer. In each
case, a surface is held at some (not necessarily uniform) potential or tem-
perature and the potential or temperature is sought in regions away from
the surface. In the present context, these surfaces are typically (portions of)
spheres.
Example 26.7.1.
Two solid heat-conducting hemispheres of radius a, separated
by a very small insulating gap, form a sphere. The two halves of the sphere are two solid
heat-conducting
hemispheres held
at temperatures
T
0
and −T
0
in contact—on the outside—with two (infinite) heat baths at temperatures T
0
and
−T
0
[Figure 26.1(a)]. We want to find the temperature distribution T (r, θ, ϕ)inside
the sphere. We choose a spherical coordinate system in which the origin coincides
with the center of the sphere and the polar axis is perpendicular to the equatorial
plane. The hemisphere with temperature T
0
is assumed to constitute the northern
hemisphere.
Since the problem has azimuthal symmetry, T is independent of ϕ,andwecan
immediately write the general solution from Equation (26.29). However, since the
origin is in the region of interest, we need to exclude all negative powers of r.This
is accomplished by setting all the B coefficients equal to zero. Thus, we have
T (r, θ)=
∞
n=0
A
n
r
n
P
n
(cos θ). (26.50)
It remains to calculate the constants A
n
. This is done by noting that
T (a, θ)=
⎧
⎪
⎨
⎪
⎩
T
0
if 0 ≤ θ<
π
2
,
−T
0
if
π
2
<θ≤ π.
In terms of u =cosθ, this is written as
T (a, u)=
⎧
⎨
⎩
−T
0
if − 1 ≤ u<0,
T
0
if 0 <u≤ 1.
Substituting this in Equation (26.50), we obtain
T (a, θ)=
⎧
⎨
⎩
−T
0
if − 1 ≤ u<0
T
0
if 0 <u≤ 1
=
∞
n=0
A
n
a
n
≡c
n
P
n
(u), (26.51)
which—except for using u instead of x—is entirely equivalent to the expansion of
Example 26.6.1, where we found that even coefficients are absent and
c
2k+1
≡ A
2k+1
a
2k+1
=
(−1)
k
(4k + 3)(2k)!
2
2k+1
k!(k +1)!
T
0
.
Finding A
2k+1
from this equation and inserting the result in (26.50) yields
T (r, θ)=T
0
∞
k=0
(−1)
k
(4k + 3)(2k)!
2
2k+1
k!(k +1)!
r
a
2k+1
P
2k+1
(cos θ), (26.52)
where we have substituted cos θ for u.