Environmental Engineering Reference
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so
π
2
a n
4 T 0
a n n 3
n
b n
=
T 0
θ ( π θ )
sin n
θ
d
θ =
π [
1
(
1
)
] .
π
0
Thus
n = 1
4 T 0
a n n 3
n
r n sin n
u
(
r
, θ )=
π [
1
(
1
)
]
θ .
Example 2 . Consider heat conduction in a sphere
Ω
of center O and radius a .Its
boundary is denoted by
. There is no heat source/sink inside the sphere. The
temperature on S 1 and S 2 is T 0 (constant) and 0, respectively. Here S 1 is the part of
∂Ω
∂Ω
inside a cone of vertex O and vertex angle 2
α
,and S 2 is the part of
∂Ω
outside
the cone. Find the steady temperature distribution in
Ω
.
Solution. Take the center of the sphere (also the cone vertex) as the origin of the
coordinate system. Let u be the temperature; it must satisfy
x 2
y 2
z 2
a 2
Δ
u
=
0
,
+
+
<
,
T 0 , (
x
,
y
,
z
)
S 1 ,
(7.20)
u
=
0
, (
x
,
y
,
z
)
S 2 .
Without loss of generality, take the positive Oz -axis as the axis of the cone. In a
spherical coordinate system
(
r
, θ , ϕ )
, u is independent of
ϕ
basedonasymmetryof
the boundary conditions. Therefore, u satisfies
r 2
sin
=
u
1
sin
∂θ
θ
u
∂θ
Δ
u
+
=
0
,
0
<
r
<
a
,
0
< θ < π ,
r
r
θ
T 0 ,
0
θ α ,
u
(
a
, θ )=
0
, α < θ π .
(7.21)
Assume u
=
R
(
r
) Θ ( θ )
. Substituting it into the equation in PDS (7.21) yields
r 2 R (
)
θ )
( Θ ( θ )
r
1
sin
sin
=
= λ ,
R
(
r
)
θ
Θ ( θ )
where
λ
is the separation constant. Thus we have
1
sin
θ ) + λΘ ( θ )=
θ ( Θ ( θ )
sin
0
,
0
< θ < π ,
(7.22)
| Θ (
0
) | < , θ (
0
, π ) .
and
r 2 R (
2 rR (
r
)+
r
) λ
R
(
r
)=
0
,
|
R
(
0
) | < .
(7.23)
 
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