Geoscience Reference
In-Depth Information
ˆ
ˆ
ˆ
P
T B
R
B
Figure 2.13 Local coordinate system used to describe a curved magnetic field. The inset
gives the directions of the unit vectors at the point P . In a stretched magnetic field the
tension force T B is parallel to and inversely proportional to R .
b
normal to B (and antiparallel to the radius of curvature), and a unit vector
given by b
n
׈
s . We have just shown that J
×
B may be written in the form
of the magnetic force f B =
J
×
B ,or
B 2
μ 0
f B = (
1
0 )(
B
·∇ )
B
−∇
/
2
(2.61)
where
B
=
B
s
ˆ
n , and b ,
In terms of
ˆ
s ,
ˆ
B 2
(
B
·∇ )
B
=
B
(∂/∂
s
)(
B
ˆ
s
) =
B
(∂
B
/∂
s
) ˆ
s
+
(∂ ˆ
s
/∂
s
)
Now
ˆ
s
/∂
s
nd
θ/
Rd
θ
n
/
R
so
B 2
R
(
B
·∇ )
B
=
B
(∂
B
/∂
s
) ˆ
s
+
/
n
ˆ
Substituting into (2.61),
B 2
μ 0 R
B 2
μ 0
f B =
/
2
n
ˆ
+ (
B
0 )(∂
B
/∂
s
) ˆ
s
−∇
/
2
But
B 2
μ 0
(
1
0 )(
B
B
/∂
s
) =
/
2
/∂
s
 
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