Environmental Engineering Reference
In-Depth Information
we have
t
t
2
t
t
t
2
1
τ
0
∂
∂
τ
+
∂
B
2
∂
∂
A
2
W
f
τ
d
W
f
τ
d
τ
−
Δ
W
f
τ
d
τ
−
t
Δ
W
f
τ
d
τ
t
∂
0
0
0
0
1
d
t
2
W
f
τ
∂
τ
0
∂
W
f
τ
∂
t
+
∂
B
2
∂
∂
A
2
=
−
Δ
W
f
τ
−
t
Δ
W
f
τ
τ
+
f
(
r
,
θ
,
ϕ
,
t
)
t
2
0
=
f
(
r
,
θ
,
ϕ
,
t
)
.
Therefore, the
u
(
r
,
θ
,
ϕ
,
t
)
in Eq. (6.153) is indeed the solution of PDS (6.152).
Remark 1.
Let
u
be the solution of PDS (6.141) (Eq. (6.146)). The
solution of PDS (6.140) is, by the principle of superposition,
=
W
ψ
(
r
,
θ
,
ϕ
,
t
)
1
W
Φ
(
τ
0
+
∂
B
2
W
k
nl
Φ
(
u
=
r
,
θ
,
ϕ
,
t
)+
r
,
θ
,
ϕ
,
t
)
∂
t
t
+
W
ψ
(
r
,
θ
,
ϕ
,
t
)+
W
f
τ
(
r
,
θ
,
ϕ
,
t
−
τ
)
d
τ
,
(6.155)
0
1
2
)
1
2
)
(
n
+
(
n
+
where
f
τ
=
f
(
r
,
θ
,
ϕ
,
τ
)
,
k
nl
=
μ
/
a
.The
μ
are available in Section 2.6.2.
l
l
Remark 2.
All results for the hyperbolic heat-conduction equations are recovered
as the special case of dual-phase-lagging heat-conduction equations at
B
=
0.
Remark 3.
By using the structure of
W
ψ
in Eq. (6.146), we obtain the
u
(
r
,
θ
,
ϕ
,
t
)
in
Eq. (6.153).
t
=
W
f
τ
(
,
θ
,
ϕ
,
−
τ
)
u
r
t
d
τ
0
t
r
;
θ
,
θ
;
ϕ
,
ϕ
;
t
r
,
θ
,
ϕ
,
τ
)
=
G
(
r
,
−
τ
)
f
(
d
Ω
d
τ
.
0
r
≤
a
This is called the
integral expression
of the solution of PDS (6.152). The triple series
G
r
;
θ
,
θ
;
ϕ
,
ϕ
;
t
(
,
−
τ
)
is called the
Green function of dual-phase-lagging heat-
conduction equations in a spherical domain
.When
f
r
(
r
,
θ
,
ϕ
,
t
)=
δ
(
r
−
r
0
,
t
−
t
0
)
,
in particular, the solution of PDS (6.152) reduces
u
=
G
(
r
,
r
0
;
θ
,
θ
0
;
ϕ
,
ϕ
0
;
t
−
t
0
)
.
where
r
=(
r
,
θ
,
ϕ
)
,
r
0
=(
r
0
,
θ
0
,
ϕ
0
)
. Thus the Green function
G
(
r
,
r
0
;
θ
,
θ
0
;
ϕ
,
ϕ
0
;
t
,
t
0
)
is the solution due to a source term
δ
(
r
−
r
0
,
t
−
t
0
)
.
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