Geoscience Reference
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Equations for Disturbances
Suppose that in the equilibrium state, the velocities
v
a
and electric field
E
vanish and the plasma is embedded into external magnetic field
B
0
. Unper-
turbed values of concentration denote as
N
0
=
N
e
0
=
N
i
0
,
N
n
0
, and pressure
P
α
0
. Denote small perturbations of magnetic and electric fields, particle num-
ber densities, velocities and pressure by
b
,
E
,n
α
,
v
(
α
)
and
p
α
.
Substituting into (1.23)-(1.27)
B
0
+
b
,
E
,N
α
0
+
n
α
,
v
(
α
)
,P
α
0
+
p
α
,
(1.42)
and neglecting all quadratic terms of the perturbations, we obtain linearized
equations of 3-fluid hydrodynamics. From now on, if it is not specified, we
drop
0
when there was no risk of ambiguity and write
N
α
instead of
N
α
0
,
for easy of notation. Linearized continuity equations (1.23)-(1.25) allow us to
find perturbations of concentrations of plasma components from divergencies
of mean velocities:
∂n
e
∂t
∂n
i
∂t
∂n
n
∂t
=
−
N
∇
·
v
e
,
=
−
N
∇
·
v
i
,
=
−
N
n
∇
·
v
n
.
(1.43)
From the momentum equations (1.26)-(1.27) we get
E
+
1
B
0
]
∂
v
e
∂t
e
m
e
−
∇
p
e
m
e
N
e
−
=
−
c
[
v
e
×
ν
ei
(
v
e
−
v
i
)
−
ν
en
(
v
e
−
v
n
)
,
(1.44)
E
+
1
B
0
]
∂
v
i
∂t
e
m
i
−
∇
m
i
N
i
+
m
e
p
i
=
c
[
v
i
×
m
i
ν
ei
(
v
e
−
v
i
)
−
ν
in
(
v
i
−
v
n
)
,
(1.45)
∂
v
n
∂t
−
∇
p
n
m
n
N
n
−
m
e
m
n
N
e
N
n
ν
en
(
v
n
−
m
i
m
n
N
i
N
n
ν
in
(
v
n
−
=
v
e
)
−
v
i
)
.
(1.46)
A linear approximation to (1.33)-(1.34) is given in Chapter 4, where wave
disturbances in the linear magnetohydrodynamics are considered.
1.3 Electromagnetic Field Equations
Let us introduce the electric induction vector
D
(
r
,t
)as
t
j
(
r
,t
)dt
D
(
r
,t
)=
E
(
r
,t
)+4
π
(1.47)
−∞
making it possible to combine density of induced charges and currents with
displacement currents in the field equations. Thus, Maxwell's equations (1.9)
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