Geoscience Reference
In-Depth Information
where s is a distance measured in the direction parallel to k . The perturbation
vector k is confined to the x - z plane, while
n is in the y direction. Because both
elements
σ P of the tensor conductivity are proportional to the density, it
follows that they will depend on s in a similar manner,
σ 0 and
) = σ 0 + δσ 0 e i ( ks ω t )
σ 0 (
s
,
t
) = σ P + δσ P e i ( ks ω t )
σ P (
s
,
t
Our goal is to determine the perturbation electric field
δ
E k that is parallel to
k , since we are dealing with an electrostatic wave,
E k e i ( ks ω t )
E k (
s
,
t
) = δ
We now solve for
δ
E k
in terms of the initial perturbation in
δ
n by setting
∇·
J
=
0. In the x - z plane,
J
= σ 0 E z ˆ
a z + σ P E x ˆ
a x
For now, we take the zero-order perpendicular electric field to be zero. Since
the zero-order parallel electric field is upward in the case illustrated by Fig. 10.15,
we have
)
)
(
(
σ 0 + δσ 0 e i
k x x
+
k z z
ω
t
e i
k x x
+
k z z
ω
t
J
=
E
|| + δ
E k sin
θ
a z
ˆ
)
)
(
(
σ p + δσ p e i
k x x
+
k z z
ω
t
e i
k x x
+
k z z
ω
t
+
δ
E k cos
θ
a x
ˆ
Evaluating
∇·
J , dropping second-order terms, and setting the result equal to
zero yields
θ e i
(
) =
k x x
+
k z z
ω
t
ik z δσ 0 E
|| +
ik z σ 0 δ
E k sin
θ +
ik x δσ p δ
E k cos
0
Substituting k z =
k sin
θ
and k x =
k cos
θ
and solving for
δ
E k ,
θ
σ 0 sin 2
θ + σ p cos 2
δ
E k =
E
|| δσ 0 sin
θ
which may be written
δσ 0
σ 0
sin
θ
δ
E k +
E
θ + σ p 0 cos 2
(10.7)
||
sin 2
θ
Our goal is not to carry out a full algebraic analysis of the process, which is
quite messy, but rather to gain some physical insight. To proceed, however, we
 
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