Environmental Engineering Reference
In-Depth Information
Therefore, Eqs. (7.160') and (7.163') are transpose equations of each other. Equa-
tions (7.161') and (7.162') are also transpose equations of each other.
Remark 2
.ByTheorem3inSection7.8,thekernel
K
(
M
,
P
)
satisfies
≤
cos
(
PM
,
n
)
c
r
2
−
δ
|
K
(
M
,
P
)
|
=
PM
,
0
<
δ
<
1
.
r
PM
2
π
is weakly singular, and the four integral equations all have
a weakly-singular kernel.
Thus the kernel
K
(
M
,
P
)
7.9.3 Boundary-Value Problems of Poisson Equations
In studying steady heat conduction or steady electric fields in domains with an in-
ternal source or sink, we arrive at the Poisson equations
Δ
u
=
F
(
M
)
,
M
∈
Ω
.
(7.164)
The key for seeking solutions of boundary-value problems of Eq. (7.164) is to find a
particular solution
u
∗
of Eq. (7.164). Once
u
∗
is available, a function transformation
of
u
u
∗
will transform the boundary-value problems of Poisson equations into
Laplace equations. For example, Dirichlet problems of the Poisson equation
=
ω
+
Δ
u
=
F
(
M
)
,
M
∈
Ω
,
(7.165)
u
|
S
=
f
(
M
)
.
will be transformed into
Δω
=
0
,
M
∈
Ω
,
(7.166)
u
∗
|
S
ω
|
S
=
(
)
−
f
M
u
∗
.
By the third Green formula (Eq. (7.65)), the solution of a Poisson equation satis-
fies
by a function transformation of
u
=
ω
+
u
1
r
PM
d
S
1
4
)
∂
∂
r
PM
∂
1
u
(
P
)
1
4
F
(
P
)
u
(
M
)=
−
(
P
−
−
d
Ω
.
π
n
∂
n
π
r
PM
S
Ω
(7.167)
The two surface integrals in the right-hand side are the single-layer potential and the
double-layer potential, respectively. They satisfy the Laplace equation. The volume
integral in the right-hand side thus must be a particular solution of the Poisson equa-
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