Geology Reference
In-Depth Information
The following theorem, known as the Green ' s
third identity , is probably the most important
result for potential functions, in particular for
harmonic fields.
Green's Third Identity
Let § D §( r ) be a scalar field , defined in a closed
region R with boundary S ( R ), and let P be a fixed
point in R . If r is the distance of any other point
Q 2 R from P , then :
Fig. 4.20 Geometry of problem for Green's third identity
Z
I
1
1
r r
1
1
r
@n dS
2 §dV C
§.P/ D
element versor n is directed inwards , because
the sphere itself belongs to the complement of
E . Therefore, for any scalar field f defined on
the surface of †, the directional derivative in
the direction n is the opposite of a directional
derivative in the direction of Q , so that it results:
R
S . R /
1
r
dS
I
1
§ @
@n
S. R /
(4.68)
Proof Let us consider the scalar field ¥ D 1/ r .
In this instance, the Green's second identity as-
sumes the form:
I
@f
@r
Furthermore, when we integrate over the sur-
face of †, the points Q have a fixed distance r D
R from P , R being the radius of †, and the spatial
average of § over the surface of this sphere is:
@f
@n D
1
r
1
r
dS
@n § @
@n
S. R /
1
r r
2 1
r
dV
Z
I
2 § § r
D
1
4 R 2
h § i D
§dS
R
2 (1/ r ) D 0 for any point
Q ¤ P . Therefore, let us consider a small sphere,
†, about P (Fig. 4.20 )andtheset E D R †.
In E , the previous identity can be rewritten as
follows:
Z
We
know
that r
Clearly, if we take the limit as R ! 0of
this expression, we obtain simply §( P ). At the
same time, the integral at left-hand side of ( 4.69 )
will be extended to the whole region R .Thelast
integral at the right-hand side of ( 4.69 ) can be
evaluated as follows:
I
1
r
1
r
dS
I
1
r r
@n § @
2 §dV D
1
r
1
r
dS
@n
@n § @
E
S . E /
I
1
r
1
r
dS
@n
@n § @
D
I
1
r
dS D
@n
1
r
@r C § @
D
S. R /
@r
I
1
r
1
r
dS
@n § @
C
I
r 2 § dS D
@n
1
r
@r
1
D
(4.69)
I
1
R
@r dS
In evaluating the integral over the surface of
†, we must take into account that any surface
D h § i
 
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