Drift Equations
The drift equations take the form:
and
If we assume that
then the dominant term in the electron energy conservation equation
(4.202) yields
|
(4.206) |
which implies that
|
(4.207) |
In other words, in the drift approximation, the parallel electron heat conductivity is usually sufficiently large that it
forces the electron temperature to be constant on magnetic field-lines.
The dominant term in the ion energy conservation equation
(4.205) yields
|
(4.208) |
which implies that
|
(4.209) |
In other words, in the drift approximation, the parallel ion heat conductivity is usually sufficiently large that it
forces the ion temperature to be constant on magnetic field-lines.
The dominant terms in the electron and ion momentum conservation equations, (4.201) and (4.204),
yield
The sum of the preceding two equations gives
|
(4.212) |
where . In other words, in the drift approximation, to lowest order, the plasma exists in an equilibrium state in which
the magnetic force density balances the total scalar pressure force density. It follows from the previous equation that
|
(4.213) |
In other words, in the drift approximation, the total plasma pressure is constant along magnetic field-lines.
Given that
, and making use of Equations (4.207) and (4.209), we deduce that
|
(4.214) |
In other words, in the drift approximation, the electron number density is constant along magnetic field-lines.
It follows that the electron and ion pressures,
and
, are also constant along magnetic
field-lines. Hence, Equation (4.210) yields
|
(4.215) |
In other words, in the drift approximation, to lowest order, the parallel electric field is zero.
Equations (4.210)–(4.211) can be inverted to give
Here,
is the
velocity, whereas
|
(4.218) |
and
|
(4.219) |
are termed the electron diamagnetic velocity and the ion diamagnetic
velocity, respectively.
According to Equations (4.216)–(4.217), in the drift approximation, the velocity of the electron
fluid perpendicular to the magnetic field is the sum of the
velocity and the electron diamagnetic velocity. A similar statement can be made for the ion fluid.
By contrast, in the MHD approximation the perpendicular velocities of the
two fluids consist of the
velocity alone, and are,
therefore, identical to lowest order. The main difference between the
two orderings lies in the assumed magnitude of the electric field. In the
MHD limit
|
(4.220) |
whereas in the drift limit
|
(4.221) |
Thus, the MHD ordering can be regarded as a strong electric field
ordering, whereas the drift ordering corresponds to a weak electric
field ordering.
The diamagnetic velocities are so named because the diamagnetic
current,
|
(4.222) |
generally acts to reduce the magnitude of the magnetic field inside
the plasma.
The electron diamagnetic velocity can be written
|
(4.223) |
In order to account for this velocity, let us consider a simplified
case in which the electron temperature is uniform, there is a
uniform density gradient running along the -direction, and the magnetic
field is parallel to the -axis. (See Figure 4.3.)
The electrons gyrate in the - plane in circles of radius
. At a given point, coordinate , say, on the -axis,
the electrons that come from the right and the left have traversed distances
of approximate magnitude . Thus, the electrons from the right originate from
regions where the particle density is approximately
greater than the regions from which the electrons from the left originate.
It follows that the -directed particle flux
is unbalanced, with slightly more particles moving in the -direction
than in the -direction. Thus, there is a net particle flux
in the -direction: that is, in the direction of
.
The magnitude of this flux is
|
(4.224) |
There is no unbalanced particle flux in the -direction, because the
-directed fluxes are associated with electrons that originate from regions
where . We have now accounted for the first term on the
right-hand side of Equation (4.223).
We can account for the second term using similar arguments.
The ion diamagnetic velocity is similar in magnitude to the electron
diamagnetic velocity, but is oppositely directed, because ions gyrate
in the opposite direction to electrons.
Figure 4.3:
Origin of the diamagnetic velocity in a magnetized plasma.
|
The most curious aspect of diamagnetic flows is that they represent fluid flows
for which there is no corresponding motion of the particle guiding
centers. Nevertheless, the diamagnetic velocities are real fluid
velocities, and the associated diamagnetic current is a real current.
For instance, the diamagnetic current contributes to force balance inside the plasma,
and also gives rise to ohmic heating.