The procedure works in the following way: Start with an initial
guess for magnetic island widths for the resonant helical
harmonics being considered. Determine the effect of each magnetic
island on the background current density and pressure profile near
each mode rational surface. The background axisymmetric current
density and pressure profile and flux surface shapes (such as
elongation and triangularity) can be taken, for example, from the
evolving solution in an integrated modeling code. A solution is
found for each harmonic of the perturbation
from the set of coupled
differential equations (7) and (8) together
with ancillary equations (9) and (10) for
and
. The Hamada coordinate
metric elements (the geometric terms in
Eqs. (11-13)) are used to compute the harmonic
mixing of the perturbed magnetic field components
. An adaptive ordinary
differential equation solver [9] can be used to
integrate the equations for
and
from the magnetic axis to the plasma boundary or perfectly
conducting wall. The island widths are adjusted iteratively until
all the solutions match the boundary conditions at the wall. The
width of each magnetic island acts like a nonlinear eigenvalue for
the two point boundary value problem in which the perturbed
magnetic field radial component vanishes at the magnetic axis and
at a perfectly conducting wall at the plasma edge. For a
self-consistent treatment, this algorithm is used in an integrated
modeling code and the transport is enhanced across each island, as
described in the next section.
At each stage in the iteration, the amplitudes of the perturbed magnetic field harmonics are adjusted to be consistent with the widths of the corresponding magnetic islands, using Eq. (28). In most other treatments of tearing modes, the differential equation for the perturbation is integrated from the magnetic axis outward to the island, and then from the wall inward to the island, and the solution is matched across the island. When there are multiple harmonics that are mixing with one another (through Eqs. (11-13)), it is simpler to integrate all the harmonics together from the magnetic axis to the outer boundary condition at the wall. With finite island widths and the resulting modifications of the profiles described in section 1.3 above, an adaptive ODE solver [9] can integrate all the harmonics from the magnetic axis through the islands to the outer boundary condition.
The algorithm described above applies to an arbitrary number of
helical harmonics in any background axisymmetric geometry with
arbitrary cross-section, aspect ratio, and plasma . The
algorithm is simple enough to be used in an integrated predictive
modeling code. Island widths change as the plasma profiles
evolve. The algorithm does not apply to tearing modes that do not
saturate in time, such as the
tearing mode that drives
sawtooth crashes.