Geoscience Reference
In-Depth Information
In the text we need to develop the boundary condition (
4.12
) as a series in Legendre
polynomials. For that one should use the following representation of the delta-
function
X
ı./
sin
D
C
n
P
n
.cos /:
(4.59)
nD0
In order to obtain the undetermined coefficients C
n
, one should multiply Eq. (
4.59
)
by sin P
m
.cos / and then integrate both sides of this equation between zero and .
On account of Eqs. (
4.57
) and (
4.58
) one can find
n
C
P
n
.1/
D
n
C
1
2
1
2
:
C
n
D
(4.60)
In the course of this text, we also need the following sum
n
.
n
C
1
/
P
n
.cos /
D
ln
sin
2
X
.2n
C
1/
1:
(4.61)
2
nD1
Rearrangement of Solution
Before rearranging Eq. (
4.33
), it should be noted that this equation contains the
delta-function of because the source function, that is, the current density j
s
includes the same factor, i.e., ı./. In order to eliminate the delta-function, one
should rearrange the sum in Eq. (
4.33
). Taking the notice of
!
n
!
n
!
2
D
!
2
!
n
!
2
C
1
(4.62)
and accounting of Eqs. (
4.59
) and (
4.60
), we obtain
X
X
!
n
.2n
C
1/
!
2
.2n
C
1/
!
n
!
2
2ı./
sin
: (4.63)
!
n
!
2
P
n
.cos /
D
P
n
.cos /
C
n
D
0
n
D
0
If the delta-function is omitted and !
2
in the sums is replaced by the !
2
C
ic!Z.!/=d,Eq.(
4.33
) is reduced to (
4.38
).
Search WWH ::
Custom Search