
276 Basics of Magnetostatics
,
(5.43)
. (5.44)
One might as well integrate from through . vanishes because of the odd
integrand, does not, however. We will, once again, demonstrate the necessity of
starting from Cartesian coordinates when using eq. (5.15). Had we tried to
calculate and directly from (5.15), the result would not have been (5.44),
but an incorrect one. This would have been the integral without the factor
in the numerator of the integrand. To find an analytic solution for
of (5.44) is not possible. However, the integral is related to the total elliptic
integrals. To see this, one has to resort to some mathematical tricks. First, we
introduce the variable
or
.
This makes
.
Furthermore, define the parameter
.
(5.45)
Then, obtain
.
Obviously, this is independent of because integration is always over a whole
period of . Also the symmetry of the problem does not allow a -
dependency of . This allows one to pick a convenient value, for example,
. The integration is then from through :
A
r
µ
0
Ir
0
4π
-------------
ϕϕ'–()sin ϕ'd
r
2
r
0
2
z
2
2rr
0
ϕϕ'–()cos–++
-----------------------------------------------------------------------------
0
2π
∫
0==
A
ϕ
µ
0
Ir
0
4π
-------------
ϕϕ'–()cos ϕ'd
r
2
r
0
2
z
2
2rr
0
ϕϕ'–()cos–++
-----------------------------------------------------------------------------
0
2π
∫
=
π–+π A
r
A
ϕ
A
ϕ
g
ϕ
ϕϕ'–()cos A
ϕ
ψ
πϕϕ'–()–
2
----------------------------=
ϕϕ'– π 2ψ–=
ϕϕ'–()cos 2 ψsin
2
1–=
k
2
4rr
0
rr
0
+()
2
z
2
+
--------------------------------=
A
ϕ
µ
0
Ir
0
4π rr
0
+()
2
z
2
+
-------------------------------------------
2 ψsin
2
1–
1 k
2
ψsin
2
–
---------------------------------
2 ψd
π 2⁄ϕ2⁄–
3π 2⁄ϕ2⁄–
∫
=
ϕ
ψsin
2
ϕ
A
ϕ
ϕ 2π= ψπ2⁄–= ψ +π 2⁄=
A
ϕ
µ
0
Ir
0
2π rr
0
+()
2
z
2
+
-------------------------------------------
2 ψsin
2
1–
1 k
2
ψsin
2
–
---------------------------------
ψd
π 2⁄–
π 2⁄
∫
=
µ
0
Ir
0
π rr
0
+()
2
z
2
+
----------------------------------------
2 ψsin
2
1–
1 k
2
ψsin
2
–
---------------------------------
ψd
0
π 2⁄
∫
=