Environmental Engineering Reference
In-Depth Information
and (6.220), Xu andWang (2002) obtain an expression of
λ 1 , 2 in terms of
ζ m and
ω m ,
λ 1 , 2 = ω m
1
ζ m ±
ζ
m
.
(6.221)
Underdamped Oscillation
<
For the case
ζ
1, there are two complex conjugates
λ
1 and
λ
2 ,
m
λ 1 , 2 = ω m
i 1
ζ m ±
ζ
m
.
(6.222)
Therefore
e ζ m ω m t a m cos
ω m t 1
ω m t 1
m
m
Γ m (
t
)=
ζ
+
b m sin
ζ
.
(6.223)
After the determination of integration constants a m and b m by the initial conditions
[Eq. (6.214)], Xu and Wang (2002) obtain
e ζ m ω m t
ω m t 1
ω m t 1
+ ψ m + ζ m ω m φ m
m
ω m 1
m
Γ m (
t
)=
φ m cos
ζ
sin
ζ
m
ζ
(6.224)
which may be rewritten as
A m e ζ m ω m t sin
Γ m (
t
)=
( ω dm t
+ ϕ dm ) .
(6.225)
Here,
ψ m + ζ m ω m φ m
ω dm
2
m
A m =
φ
+
,
(6.226)
ω dm = ω m 1
ζ
m
,
(6.227)
tan 1
φ m ω dm
ψ m + ζ m ω m φ m
ϕ dm =
.
(6.228)
Therefore, the system is oscillating with frequency
ω dm and an exponentially decay-
ing amplitude A m e ζ m ω m t
[Eq. (6.215)]. Fig. 6.1 typifies the oscillatory pattern, for
ζ m =
0. The wave behavior is still observed in
dual-phase-lagging heat conduction. However, the amplitude decays exponentially
due to the damping of thermal diffusion. This differs enormously from classical heat
conduction.
0
.
1,
ω m =
1
.
0,
φ m =
1
.
0and
ψ m =
0
.
1 forms the condition for thermal oscillation of this kind.
Figure 6.2 illustrates the variation of
ζ m <
Γ m (
t
)
with the time t when
ψ m is changed
to 1
.
0 from 0.
Γ m is observed sometimes to be capable of surpassing
φ m . This phe-
 
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