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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