Environmental Engineering Reference
In-Depth Information
tions can be written as
μ m
lh 1
2
sin μ m x
l + ϕ m
)= μ m
lh 1 cos μ m x
sin μ m x
X m (
x
l +
l =
1
+
,
ϕ m = μ m
where tan
lh 1 .
Finally, we have eigenvalues
λ m and eigenfunctions X m (
x
)
μ m
l
2
Eigenvalues
λ m =
,
μ m are the positive zero points of f
(
x
)
in Eq. (6.44).
sin μ m x
l + ϕ m
ϕ m = μ m
Eigenfunctions X m (
x
)=
,
tan
lh 1 . Normal square of
eigenfunction set
l
sin 2 μ m x
l
m d x
2
X m
(
x
)
=(
X m
(
x
) ,
X m
(
x
)) =
+ ϕ
0
l
1
β m
sin 2
=
( β m x
+ ϕ m )
d
( β m x
+ ϕ m )
0
l
1
β m
1
cos2
( β m x
+ ϕ m )
=
d
( β m x
+ ϕ m )
2
0
1
2 ( β
l
1
β
1
4 sin2
=
m x
+ ϕ
)
( β
m x
+ ϕ
)
m
m
m
0
1
2 l
ϕ m
1
β m
1
4 sin2
1
4 sin2
=
β m
(
l
β m + ϕ m )+
1
l
2
1
=
μ m [
sin2
( μ m + ϕ m )
sin2
ϕ m ]
2
1
l
2
sin
μ m
=
cos
( μ m +
2
ϕ m )
.
(6.45)
μ
m
Remark 1 . Eigenvalues and eigenfunctions of the other eight combinations can also
be obtained using a similar approach. The results for all nine combinations are listed
in Table 2.1. Therefore we can use Table 2.1 to solve the mixed problems of dual-
phase-lagging heat-conduction equations subject to different boundary conditions.
Remark 2 . We can also apply integration by parts to prove that the eigenvalues
of Eq. (6.43) cannot be negative. Integrating the equation in Eq. (6.43) from x
=
0
yields l
0
) X (
) d x
=
(
)
to x
l after multiplying X
x
X
(
x
x
)+ λ
X
(
x
=
0, which be-
comes, by making use of integration by parts, to l
0
X (
X
(
x
)
x
)
d x ,
l
l
)
0 X (
) 2 d x
l
0 +
X 2
X (
λ
(
x
)
d x
=
X
(
x
)
x
x
.
0
It becomes, after applying the boundary conditions in Eq. (6.43),
l
l
X (
) 2 d x
X 2
h 1 X 2
h 2 X 2
λ
(
x
)
d x
=
(
0
)+
(
l
)+
x
,
0
0
 
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