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 ).
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