Environmental Engineering Reference
In-Depth Information
3.4.2 Fundamental Solution of the One-Dimensional
Heat-Conduction Equation
+
∞
Rewrite Eq. (3.27) into
u
=
ϕ
(
ξ
)
V
(
x
,
ξ
,
t
)
d
ξ
,where
−
∞
t
e
−
(
x
−
ξ
)
2
1
2
a
√
π
V
(
x
,
ξ
,
t
)=
,
t
>
0
.
(3.29)
4
a
2
t
Consider a unit point source at
t
=
0and
x
=
x
0
such that
ϕ
(
x
)=
δ
(
x
−
x
0
)
and
Eq. (3.27) becomes
+
∞
u
=
δ
(
ξ
−
x
0
)
V
(
x
,
ξ
,
t
)
d
ξ
=
V
(
x
,
x
0
,
t
)
,
−
∞
which is the temperature distribution due to the initial unit point source at
x
=
x
0
.
Therefore,
V
(
x
,
ξ
,
t
)
in Eq. (3.29) must satisfy
V
t
=
a
2
V
xx
, −
∞
<
x
<
+
∞
,
0
<
t
,
(3.30)
V
|
t
=
0
=
δ
(
x
−
ξ
)
,
and is the temperature distribution due to
ϕ
(
x
)=
δ
(
x
−
ξ
)
, an initial unit point
source at
x
=
ξ
.
defined by Eq. (3.29) is called the
fundamental solution of the one-
dimensional heat-conduction equation
.Byusing
V
, we may rewrite the solution of
PDS (3.25) by
The
V
(
x
,
ξ
,
t
)
+
∞
t
+
∞
=
u
ϕ
(
ξ
)
V
(
x
,
ξ
,
t
)
d
ξ
+
d
τ
f
(
ξ
,
τ
)
V
(
x
,
ξ
,
t
−
τ
)
d
ξ
.
(3.31)
−
∞
0
−
∞
Therefore,
V
(
x
,
ξ
,
t
)
in Eq. (3.29) can also be regarded as the fundamental solution
of PDS (3.25). Here
e
−
(
x
−
ξ
)
2
1
2
a
π
(
V
(
x
,
ξ
,
t
−
τ
)=
4
a
2
,
t
>
τ
(3.32)
(
t
−
τ
)
t
−
τ
)
satisfies
V
t
=
a
2
V
xx
, −
∞
<
x
<
+
∞
,
0
<
τ
<
t
<
+
∞
,
(3.33)
V
|
t
=
τ
=
δ
(
x
−
ξ
)
or
V
t
a
2
V
xx
=
+
δ
(
x
−
ξ
,
t
−
τ
)
, −
∞
<
x
<
+
∞
,
0
<
τ
<
t
<
+
∞
,
(3.34)
|
t
=
τ
=
.
V
0
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