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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