Let us now examine the magnetized limit,
|
(4.95) |
in which the electron and ion gyroradii are much smaller than the
corresponding mean-free-paths. In this limit, the two-Laguerre-polynomial
Chapman-Enskog closure scheme yields
Here, the parallel electrical conductivity,
, is given by Equation (4.84),
whereas the perpendicular electrical conductivity,
, takes the form
|
(4.99) |
Note that
denotes a
gradient parallel to the magnetic field, whereas
denotes a gradient perpendicular to the magnetic
field. Likewise,
represents the component of the plasma current density flowing parallel to the
magnetic field, whereas
represents the perpendicular component of the plasma current density.
We expect the presence of a strong magnetic field to give rise to a
marked anisotropy in plasma properties between directions parallel
and perpendicular to , because of the completely different motions
of the constituent ions and electrons parallel and perpendicular to the field.
Thus, not surprisingly, we find that the electrical conductivity perpendicular
to the field is approximately half that parallel to the field [see Equations (4.96)
and (4.99)]. The thermal force is unchanged (relative to the unmagnetized case)
in the parallel direction, but is radically modified in the
perpendicular direction. In order to understand the origin
of the last term in Equation (4.96), let us consider a situation in
which there is a strong magnetic field along the -axis, and an electron
temperature gradient along the -axis. (See Figure 4.1.) 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
electron temperature is approximately
greater than
the regions from which the electrons from the left originate. Because the
friction force is proportional to , an unbalanced friction force
arises, directed along the -axis. (See Figure 4.1.) This direction
corresponds to the direction of
.
There is
no friction force along the -axis, because the -directed fluxes are associated with electrons that originate from regions where .
By analogy with Equation (4.85), the magnitude of the perpendicular
thermal force is
|
(4.100) |
The effect of a strong magnetic field on the perpendicular
component of the thermal force is directly analogous to a well-known
phenomenon in metals called the Nernst effect (Rowe 2006).
Figure 4.1:
Origin of the perpendicular thermal force in a magnetized plasma.
|
In the magnetized limit, the electron and ion heat flux densities become
respectively. Here, the parallel thermal conductivities are
given by Equations (4.89)–(4.90), and
the perpendicular thermal conductivities take the form
Finally, the cross thermal conductivities are written
The first two terms on the right-hand sides of Equations (4.101) and (4.102)
correspond to diffusive heat transport by the electron and ion
fluids, respectively. According to the first terms, the diffusive transport in
the direction parallel to the magnetic field is exactly the same as that in the
unmagnetized case: that is, it corresponds to
collision-induced random-walk diffusion
of the ions and electrons, with
frequency , and step-length . According to the
second terms, the diffusive transport in the direction perpendicular to the
magnetic field is far smaller than that in the parallel direction.
To be more exact, it is smaller by a factor
, where is the
gyroradius, and the mean-free-path. In fact, the perpendicular
heat transport also corresponds to collision-induced random-walk diffusion
of charged particles,
but with frequency , and
step-length . Thus, it is the greatly reduced step-length in the
perpendicular direction, relative to the parallel direction, that ultimately
gives rise to the strong reduction in the perpendicular heat transport.
If
then the ion perpendicular heat diffusivity actually
exceeds that of the electrons by the square root of a mass ratio: that is,
.
The third terms on the right-hand sides of Equations (4.101) and (4.102)
correspond to heat fluxes that are perpendicular to both the magnetic field
and the direction of the temperature gradient. In order to understand the
origin of these terms, let us consider the ion flux. Suppose that there
is a strong magnetic field along the -axis, and an ion temperature gradient
along the -axis. (See Figure 4.2.) The ions gyrate in the - plane
in circles of radius
, where is the
ion thermal velocity. At a given point, coordinate , say, on the -axis,
the ions that come from the right and the left have traversed distances of
approximate magnitude . The ions from the right are clearly somewhat hotter than those
from the left. If the unidirectional particle fluxes, of approximate magnitude , are
balanced, then the unidirectional heat fluxes, of approximate magnitude
, will
have an unbalanced component of relative magnitude
. As a result, there is a net heat flux in the -direction
(i.e., the direction of
). The magnitude of
this flux is
|
(4.107) |
There is an analogous expression for the electron flux, except that the electron
flux is in the opposite direction
to the ion flux (because the electrons gyrate in the opposite
direction to the ions). Both the ion and electron fluxes transport
heat along isotherms, and do not, therefore, give rise to
any change in plasma temperature.
Figure 4.2:
Origin of the convective perpendicular heat flux in a magnetized plasma.
|
The fourth and fifth terms on the right-hand side of Equation (4.101) correspond to
the convective component of the electron heat flux density, driven by
motion of the electrons relative to the ions. It is clear from the
fourth term that the convective flux parallel to the magnetic field is exactly the
same as in the unmagnetized case [see Equation (4.87)]. However, according to the fifth term, the
convective flux is radically modified in the perpendicular direction.
Probably the easiest method of explaining the fifth
term is via an examination
of Equations (4.81), (4.87), (4.96), and (4.101). There is clearly a very close
connection between the electron thermal force and the convective heat flux.
In fact, starting from general principles of the thermodynamics of irreversible
processes—the so-called Onsager principles (Reif 1965)—it is possible to
demonstrate that an electron frictional force of the form
necessarily gives rise to an electron heat flux
of the form
, where the
subscript corresponds to a general Cartesian component, and
is a unit vector. Thus, the fifth term on the right-hand side of Equation (4.101)
follows by Onsager symmetry from the third term on the right-hand
side of Equation (4.96). This is one of many Onsager symmetries that
occur in plasma transport theory.
In order to describe the viscosity tensor in a magnetized plasma, it is
helpful to define the rate-of-strain tensor
|
(4.108) |
Obviously, there is a separate rate-of-strain tensor for the electron and ion
fluids. It is easily demonstrated that this tensor is zero if the plasma
translates, or rotates as a rigid body, or if it undergoes isotropic
compression. Thus, the rate-of-strain tensor measures the deformation of
plasma volume elements.
In a magnetized plasma, the viscosity tensor is best described as the
sum of five component tensors,
where
|
(4.110) |
with
|
(4.111) |
and
|
(4.112) |
plus
|
(4.113) |
and
|
(4.114) |
Here, is the identity tensor, and
. The previous
expressions are valid for both electrons and ions.
The tensor
describes what is known as parallel viscosity.
This is a viscosity that controls the variation along magnetic field-lines of the
velocity component parallel to field-lines.
The parallel
viscosity coefficients, and , are specified in Equations (4.93)–(4.94).
The parallel viscosity is unchanged from the unmagnetized case,
and is caused by the collision-induced random-walk diffusion of particles,
with frequency , and step-length .
The tensors
and
describe what is known
as perpendicular viscosity. This is a viscosity
that controls the variation perpendicular to magnetic field-lines
of the velocity components perpendicular to field-lines. The perpendicular
viscosity coefficients are given by
The perpendicular viscosity is far smaller than the parallel
viscosity. In fact, it is smaller by a factor
. The
perpendicular viscosity corresponds to collision-induced random-walk diffusion
of particles, with frequency , and step-length . Thus, it
is the greatly reduced step-length in the perpendicular direction, relative
to the parallel direction, that accounts for the smallness of the
perpendicular viscosity compared to the parallel viscosity.
Finally, the tensors
and
describe what is known
as gyroviscosity. This is not really viscosity at all, because the
associated viscous stresses are always perpendicular to the velocity, implying that
there is no dissipation (i.e., viscous heating) associated with
this effect. The gyroviscosity coefficients are given by
The origin of gyroviscosity is very similar to the origin of the
cross thermal conductivity terms in Equations (4.101)–(4.102). Both
cross thermal conductivity and gyroviscosity are independent
of the collision frequency.