Environmental Engineering Reference
In-Depth Information
Generalized Fourier Expansion of u
=
W Ψ (
r
, θ , ϕ ,
t
)
a 0 ,the T
With k nl = μ (
1
2
)
n +
(
t
)
-equation becomes
l
T
nl
nl T nl =
+ ω
0
,
a
a 0 2
1
2 )
(
n
+
2
nl
where
ω
=
μ
. Its general solution reads
l
c ( 1 )
c ( 2 )
T nl (
t
)=
nl cos
ω nl t
+
nl sin
ω nl t
.
Therefore
u
=
1 { (
a mnl cos
ω nl t
+
b mnl sin
ω nl t
)
cos m
ϕ
m
,
n
=
0
,
l
=
μ (
2
)
n
+
P n (
l
+(
c mnl cos
ω nl t
+
d mnl sin
ω nl t
)
sin m
ϕ }
cos
θ )
j n
r
a 0
satisfies the wave equation and the boundary conditions of PDS (2.54).
Rewriting Eqs. (2.56) and (2.58) in the form of Eq. (2.48) shows that the eigen-
function sets are orthogonal with respect to weight functions r 2 and sin
θ
, respec-
tively.
Applying the initial condition u
(
r
, θ , ϕ ,
0
)=
0 leads to a mnl =
c mnl =
0 . To satisfy
the initial condition u t (
r
, θ , ϕ ,
0
)= Ψ (
r
, θ , ϕ )
, b mnl and d mnl must be determined
such that
μ (
1
2
)
n
+
.
P n (
l
Ψ (
r
, θ , ϕ )=
1 (
b mnl ω nl cos m
ϕ +
d mnl ω nl sin m
ϕ )
cos
θ )
j n
r
a 0
m
,
n
=
0
,
l
=
 
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