Geoscience Reference
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Ohm's law and the first equation of (15.7) lead to
σ P E x + σ H E z = j x ,
σ H E x + σ P E z =0 ,
(15.8)
where
v z
c B 0
and E x is the electric field in the stationary coordinate system. Let us elimi-
nate E z from (15.8). The result is
E x = E x
z = σ H
j x = σ C E x ,
σ P E x
(15.9)
where the Cowling conductivity σ C is
σ C = σ P + σ 2 H
σ P .
Substituting (1.93) for Pedersen σ P and (1.94) for Hall σ H conductivities, we
obtain
ω pe
4 πν e .
σ C = σ 0 1+ β i e
1+ β e β i
,
0 =
( m e /m i ) 1 / 2 , we rewrite the last equation in the
Omitting the term β i e
form
σ 0
1+ β e β i .
σ C =
(15.10)
It follows from projections of the equations onto the coordinate axis, that
the system supports two uncoupled propagating modes. For the first mode
variables v z ,j x ,b y, E x ,E z
=0and
2 v z
∂z 2
2 v z
∂t 2
1
c s
1
H
∂v z
∂z
B 0
cc s N n m n
∂j x
∂t
=
,
∂b y
∂z
4 π
c
∂E x
∂z
1
c
∂b y
∂t
=
j x ,
=
,
j x = σ C E x
v z .
B 0
c
(15.11)
E z -component of this mode is
σ H
σ P σ C j x =
β e
σ 0
1
β i e
1+ β i e j x .
E z =
( m e /m i ) 1 / 2 , we obtain
And again, if to omit terms
β e
σ 0
E z =
j x .
 
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