The fixed boundary equilibrium problem (also called the ``inverse equilibrium
problem'' by some authors) refers to the case where the shape of a magnetic
surface is given and one is asked to solve the equilibrium within this
magnetic surface. To make it convenient to deal with the shape of the
boundary, one usually use a general coordinates system which has one
coordinate surface coinciding with the given magnetic surface. This makes it
trivial to deal with the irregular boundary. To obtain the equilibrium, one
needs to solve the GS equation in the general coordinate system. Next we
derive the form of the GS equation in a general coordinate system. The main
task is to derive the form of the toroidal elliptic operator in the general
coordinate system. The toroidal elliptic operator takes the form
|
(414) |
For an arbitrary general coordinate system
(the
coordinate system here is an arbitrary general coordinate
system except that
is perpendicular to both
and
), the toroidal elliptic operator is written
|
(415) |
where the subscripts denotes partial derivatives,
is the
Jacobian of the coordinate system
. [Next, we provide
the proof of Eq. (415). The gradient of is written as (note
that is independent of )
|
(416) |
which is in the covariant form. To calculate the divergence of
,
it is convenient to express
in terms of the contravariant basis
vectors. Using the metric matrix, we obtain
|
(417) |
and
|
(418) |
Using these, Eq. (416) is written as
Using the divergence formula, the elliptic operator in Eq. (414) is
written as
which is identical with Eq. (415).]
Using Eq. (415), the GS equation [Eq. (53)] is written
|
(421) |
which is the form of the GS equation in
coordinate
system.
Subsections
yj
2018-03-09