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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