Plasma and Fusion Research
Volume 1, 015 (2006)
Rapid Communications
- Center for Scientific Computation and Mathematical Modeling, The University of Maryland
Abstract
An ideal magnetohydrodynamic instability which is driven by sheared flow and which may be relevant to reversed-shear advanced tokamak operation is described. If there is flow shear at the qmin surface, relatively weak velocity shear can drive this instability, with a time scale of the flow. The flows may be signicantly slower than the ambient poloidal Alfvén velocity, and no inflection point is needed. Thus the time scale of the instability may be signicantly longer than that of the poloidal Alfvén transit time, and it might account for disruption of reversed-shear discharges recently observed in JT-60U.
Keywords
MHD, shear flow, instability, reversed-shear tokamak, disruption
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This paper may be cited as follows:
Tomoya TATSUNO and William DORLAND, Plasma Fusion Res. 1, 015 (2006).