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
=ˆ
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
/μ
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
=ˆ
nd
θ/
Rd
θ
=ˆ
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
/μ
0
)(∂
B
/∂
s
)
ˆ
s
−∇
/
2
But
B
2
μ
0
(
1
/μ
0
)(
B
∂
B
/∂
s
)
=
∂
/
2
/∂
s
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