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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