7.7 Inhomogeneous plasma 285
where v
T
=−
T
k
B
T
0
/m so that (7.67) becomes
v
n
+ v
T
+ 2 ¯v
B
/β = 0 (7.70)
Now let us examine the roles of these macroscopic drift velocities and compare
them with the microscopic v
B
which is velocity dependent and actually appears
in the orbit equations. Since the magnetic field gradient determines the current by
Amp
`
ere’s law, it follows that the main role of ¯v
B
is to determine the net drift ve-
locity between the ions and electrons. For simplicity let us treat the ions as a static
neutralizing background so that the current is carried entirely by the electrons. Then
Amp
`
ere’s law gives the drift velocity v
d
as
v
d
=−2 ¯v
B
/β = v
n
+ v
T
This can give rise to drift wave instabilities as we saw earlier when discussing ion
acoustic waves.
Whilst the sum of v
n
and v
T
is fixed by v
d
it turns out that v
T
is in general
more destabilizing than v
n
because, for a given v
d
, it produces a more distorted f
0
.
Within the approximation of weak gradients it is easily seen that a density gradient
moves the peak of f
0
(v
y
) only slightly away from v
y
= 0. On the other hand, the
v
3
y
dependence of the
T
term in (7.69) shifts the peak much further from v
y
= 0as
illustrated in Fig. 7.16.
An interesting example occurs in the physics of shock waves. In laminar, perpen-
dicular shocks, for which the magnetic field is at right angles to the shock normal,
all three gradients are in the same direction, along the normal, and the equilibrium
is maintained by an electric field opposing the combined magnetic and plasma
pressure. The macroscopic drifts now include the E × B drift, v
E
= E
0
/B
0
, and
obey the equation
v
d
= v
E
− (v
n
+ v
T
) = 2 ¯v
B
/β
Priest and Sanderson (1972) showed that in this case the density gradient has no
significant effect, merely increasing v
E
to maintain v
d
which is determined by the
magnetic field gradient through ¯v
B
. However, the distortion of f
0
introduced by
a temperature gradient moves the peak of f
0
from v
d
to v
d
+ 3v
T
/2, as shown
in Fig. 7.17, and can produce a very significant increase in instability. Allan and
Sanderson (1974) showed that this effect can drive the ion acoustic instability even
in the case of zero net drift velocity (v
d
= 0) and T
i
∼ T
e
. Note that although
v
E
is a microscopic drift, since it appears in the orbits, as well as a macroscopic
drift, because it is the same for all electrons, it is the net drift v
d
which matters.
The equilibrium equation must be obeyed and in the absence of a pressure gradient
v
E
= v
d
. Introduction of density and temperature gradients then increase v
E
but in
such a way as to maintain the same net drift velocity.