Environmental Engineering Reference
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whichtendto2
π
u
(
M 0 )
and zero, respectively, as
ε
0. because as
ε
0,
M ξ
M 0 .
u
u
d
ω
2
π ,
u
(
M ξ )
u
(
M 0 ) ,
r
r
M 0
ε
∂Ω
Equation (7.65) becomes
u
1
r
d S
1
2
1
r
u
1
2
Δ
u
r
u
(
M 0 )=
d
Ω .
(7.73)
π
n
n
π
∂Ω
Ω
Equations (7.68), (7.69) and (7.73) can be summarized as
4
π
u
(
M 0
) ,
M 0
Ω ,
u
1
r
d S
)
1
r
u
(
M
)
Δ
u
r
(
M
d
Ω =
2
π
u
(
M 0 ) ,
M 0 ∂Ω ,
n
n
¯
∂Ω
Ω
0
,
M 0
Ω .
(7.74)
= (
where r
=
M 0 M
x
x 0 )
2
+(
y
y 0 )
2
+(
z
z 0 )
2 .If u satisfies
Δ
u
=
0, in par-
ticular, the triple integral on the left-hand side of Eq. (7.74) vanishes.
The counterpart of Eq. (7.74) in a two-dimensional case reads
2
π
u
(
M 0 ) ,
M 0
D
,
u
ln 1
r
ln 1
r
d S
u
Δ
u
r
(
) ,
,
(
M
)
d
σ =
π
u
M 0
M 0
D
n
n
D
D
0
,
M 0
.
(7.75)
D
This can be obtained by following a simi lar approach to that used in developing
Eq. (7.74), simply replacing
Ω
,
∂Ω
, M 0 M and the solid angle 4
π
of a sphere by a
plane
domain
D ,
the
piecewise
smooth
boundary
curve
2
2 and the central angle 2
of a circle, and using the
two-dimensional fundamental solution ln r .When u satisfies
D , r
=
(
x
x 0 )
+(
y
y 0 )
π
=
Δ
u
0, the double
integral in the left-hand side of Eq. (7.75) reduces to zero.
Remark. For a fixed point M 0
R 3 and a variable point M
R 3 ,
(
x 0
,
y 0
,
z 0
)
(
x
,
y
,
z
)
1
r
satisfies the harmonic equation in R 3 except at the point M 0
the function v
(
M
)=
so
1
r =
Δ
0
,
r
=
0
.
Thus
1
r
d
1
r
d
1
r
1
r 3 r
Δ
Ω =
Δ
Ω =
Δ
·
n d S
=
·
n d S
r
ε
r = ε
r = ε
R 3
 
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