Environmental Engineering Reference
In-Depth Information
and the formula for calculating internal energy in thermodynamics, the first law of
thermodynamics yields
c
∂
T
(
r
,
t
)
ρ
t
+
∇
·
q
−
F
(
r
,
t
)=
0
,
(1.72)
∂
where
and
c
are the density and the specific heat of the material, and
F
is the rate
of internal energy generation per unit volume. Equation (1.72) is called the
energy
equation
, and it contains two unknowns
T
and
q
. By usinga constitutive relation of
heat flux density, we may eliminate
q
from Eq. (1.72) to obtain an equation of tem-
perature
T
. Since both the Fourier law (1.23) and the CV constitutive relation (1.25)
are the special cases of the dual-phase-lagging constitutive relation (1.35), we use
Eq. (1.35) to derive the heat-conduction equations.
Assuming constant material properties, the divergence of Eq. (1.35) yields
ρ
+
τ
0
∂
∂
τ
T
∂
∂
∇
·
q
t
[
∇
·
q
]=
−
k
Δ
T
−
k
t
[
Δ
T
]
.
(1.73)
Substituting the expression of
∇
·
q
from Eq. (1.72)
c
∂
T
∂
∇
·
q
=
F
−
ρ
t
into Eq. (1.73) and introducing the thermal diffusivity
α
=
k
/
(
ρ
c
)
leads to
F
2
T
∂
1
α
∂
T
∂
t
+
τ
0
∂
T
∂
∂
1
k
0
∂
F
∂
t
2
=
Δ
T
+
τ
t
(
Δ
T
)+
+
τ
.
(1.74)
α
t
This is called the
dual-phase-lagging heat-conduction equation
.When
τ
T
=
0, it
reduces to the
hyperbolic heat-conduction equation
F
2
T
∂
1
α
∂
T
t
+
τ
0
∂
1
k
+
τ
0
∂
F
∂
t
2
=
Δ
T
+
.
(1.75)
∂
α
t
In the absence of two phase lags, i. e. when
τ
0
=
τ
T
=
0 , it reduces to the
classical
parabolic heat-conduction equation
1
α
∂
T
∂
1
k
F
t
=
Δ
T
+
.
(1.76)
For steady-state heat conduction, both the first and the second derivatives of
T
with
respect to
t
are zero. All three kinds of heat-conduction equations reduce to
potential
equations
.
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