Geoscience Reference
In-Depth Information
In low-pressure plasma,
c
s
c
2
A
β
=
<<
1
.
Therefore, neglecting all terms proportional to
β
, (4.33) and (4.34) reduce to
b
B
0
∂
2
∂t
2
1
c
2
A
2
∇
−
=0
,
(4.35)
∂
2
∂z
2
−
∂t
2
ξ
||
=
∂
2
b
B
0
.
1
c
s
∂
∂z
(4.36)
Equation (4.35) describes the FMS-waves. Medium elasticity in a FMS-
wave is created by magnetic pressure
P
m
=
B
0
/
8
π
. Basing on analogy with
adiabatic gas-dynamic sound velocity
c
s
=
γ
P
0
ρ
0
(
γ
is the adiabatic index) write the Alfven velocity as
B
0
4
πρ
0
=
γ
m
P
m
c
2
A
=
ρ
0
,
where
γ
m
= 2. The condition
γ
m
= 2 is linked to the field being frozen into the
plasma, owing to which the magnetic field at
ξ
||
= 0 is changed in proportion
to plasma density, while its pressure is proportional to plasma density squared.
The longitudinal displacement
ξ
||
is small in the FMS-wave in low
β
plasmas.
It follows from (4.36) that
b
propagating at Alfven velocity produces
ξ
proportional to
β
, since perturbations
b
move with Alfven velocity
c
A
c
s
.
Perturbations with
b
=0
and
∇
⊥
·
ξ
⊥
=0
are described by the uniform equation (4.36). These are ion sound waves
propagating at velocity
c
s
along the magnetic field. Plasma perturbations
occur only along the magnetic field.
Dispersion Equation
Three hydromagnetic wave modes can propagate in homogeneous plasma:
1. Alfven waves: plasma density is undisturbed and field-lines are twisted due
to plasma transverse displacements.
2. Fast magnetosonic (FMS) waves: compressions and rarefactions of field-
lines accompanied by plasma density variations. For low-temperature
plasma, when
β<<
1, longitudinal displacements of plasma in FMS-waves
are small,
ξ
∝
β
.
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