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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