Environmental Engineering Reference
In-Depth Information
6.10.1 Thermal Waves
Without loss of generality, Xu and Wang (2002) consider the one-dimensional
initial-boundary value problem of dual-phase-lagging heat conduction
⎧
⎨
∂
k
F
t
2
T
∂
2
T
3
T
1
α
T
t
+
τ
0
∂
=
∂
x
2
+
τ
T
∂
1
+
τ
0
∂
F
∂
x
2
+
,
(
0
,
l
)
×
(
0
,
+
∞
)
,
∂
t
2
∂
∂
t
∂
T
(
0
,
t
)=
T
(
l
,
t
)=
0
,
⎩
T
(
x
,
0
)=
φ
(
x
)
,
T
t
(
x
,
0
)=
ψ
(
x
)
,
(6.209)
whose solution represents the temperature distribution in an infinitely-wide slab of
thickness
l
.Here
t
is the time,
T
is the temperature,
α
is the thermal diffusivity
of the medium,
F
is the volumetric heat source,
φ
and
ψ
are two given functions,
and
τ
0
are the phase-lags of the temperature gradient and heat flux vector,
respectively.
For a free thermal oscillation,
F
τ
T
and
=
0. By taking the boundary conditions into
account, let
∞
m
=
1
Γ
m
(
t
)
sin β
m
x
,
T
(
x
,
t
)=
(6.210)
where
m
l
.
β
m
=
Using the Fourier sine series to express
φ
and
ψ
as
∞
m
=
1
φ
m
sin β
m
x
,
φ
(
x
)=
(6.211)
and
∞
m
=
1
ψ
m
sin β
m
x
,
ψ
(
x
)=
(6.212)
where
l
0
φ
(
ξ
)
2
l
φ
m
=
sin
β
m
ξ
d
ξ
,
and
l
0
ψ
(
ξ
)
2
l
=
ξ
.
ψ
sin
β
ξ
d
m
m
A substitution of Eqs. (6.210)-(6.212) into (6.209) yields, by making use of the
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