Gyrokinetic Equations for Strong-Gradient Regions
  A gyrokinetic theory is developed under a set of orderings applicable to the edge region of tokamaks and other magnetic confinement devices, as well as to internal transport barriers. The result is a practical set equations that is valid for large perturbation amplitudes [q{\delta}{\psi}/T = O(1), where {\delta}{\psi} = {\delta}{\phi} - v_par {\delta}A_par/c], which is straightforward to implement numerically, and which has straightforward expressions for its conservation properties. Here, q is the particle charge, {\delta}{\phi} and {\delta}A_par are the perturbed electrostatic and parallel magnetic potentials, v_par is the parallel velocity, c is the speed of light, and T is the temperature. The derivation is based on the quantity {\epsilon}:=({\rho}/{\lambda})q{\delta}{\psi}/T << 1 as the small expansion parameter, where {\rho} is the gyroradius and {\lambda} is the perpendicular wavelength. Physically, this ordering requires that the E\times B velocity and the component of the parallel velocity perpendicular to the equilibrium magnetic field are small compared to the thermal velocity. For nonlinear fluctuations saturated at "mixing-length" levels (i.e., at a level such that driving gradients in profile quantities are locally flattened), {\epsilon} is of order {\rho}/L, where L is the equilibrium profile scale length, for all scales {\lambda} ranging from {\rho} to L. This is true even though q{\delta}{\psi}/T = O(1) for {\lambda} ~ L. Significant additional simplifications result from ordering L/R =O({\epsilon}), where R is the spatial scale of variation of the magnetic field. We argue that these orderings are well satisfied in strong-gradient regions, such as edge and screapeoff layer regions and internal transport barriers in tokamaks, and anticipate that our equations will be useful as a basis for simulation models for these regions. 
Andris M. Dimits
physics.plasm-ph