Magnetic island deformation due to sheared flow and viscosity

被引:27
作者
Ren, C
Chu, MS
Callen, JD
机构
[1] Univ Wisconsin, Madison, WI 53706 USA
[2] Gen Atom Co, San Diego, CA 92186 USA
关键词
D O I
10.1063/1.873363
中图分类号
O35 [流体力学]; O53 [等离子体物理学];
学科分类号
070204 ; 080103 ; 080704 ;
摘要
A partial differential equation for a two-dimensional magnetohydrodynamic (MHD) equilibrium with flow and viscosity is derived. The equation is used to describe the deformation of the magnetic island caused by the viscous drag of a sheared flow. The deformation is characterized by the phase gradient of the magnetic perturbation across a magnetic island. This phase gradient has been observed experimentally in electron cyclotron emission data from the DIII-D tokamak [J. L. Luxon and L. G. Davis, Fusion Technol. 8, 441 (1985)]. (C) 1999 American Institute of Physics. [S1070-664X(99)02904-3].
引用
收藏
页码:1203 / 1207
页数:5
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