q=2 sawteeth and major disruptions in tokamaks
- 1 February 1986
- journal article
- conference paper
- Published by AIP Publishing in Physics of Fluids
- Vol. 29 (2) , 475-482
- https://doi.org/10.1063/1.865433
Abstract
In numerical simulations of q=2 tearing modes, the maximum amplitude of the mode is found to increase rapidly as the safety factor on axis q(0) rises above 1.5. The associated magnetic islands grow to the center of the column, encompassing virtually the entire plasma cross section. As a result of the formation of these very large islands, the hot central plasma is rapidly convected out to the edge of the column, thereby destroying central confinement. Experimental evidence from several tokamaks linking the formation of these very large islands with major disruptions is presented. Typically, major disruptions are observed to occur in two (or more) stages. During the first stage(s) q rises on axis while the final stage, which terminates the discharge, is associated with the violent growth of an m=2 perturbation. Under some circumstances q=2 sawteeth are predicted to occur. Evidence for such sawteeth in a divertor tokamak is discussed.Keywords
This publication has 15 references indexed in Scilit:
- Coherent nonlinear destabilization of tearing modes: The effect of the mass flowPhysics of Fluids, 1985
- Cascade properties of shear Alfvén wave turbulencePhysics of Fluids, 1985
- Are Vacuum Bubbles a Cause of Major Disruptions in Tokamaks?Physical Review Letters, 1984
- Reconnection rates of magnetic fields including the effects of viscosityPhysics of Fluids, 1984
- Effects of toroidicity on resistive tearing modesPhysics of Fluids, 1983
- Nonlinear coupling of tearing modes with self-consistent resistivity evolution in tokamaksPhysics of Fluids, 1980
- Coalescence of Magnetic IslandsPhysical Review Letters, 1980
- Reply to the comments on "Simulation of large magnetic islands: A possible mechanism for a major tokamak disruption"Physical Review A, 1978
- Comments on "Simulation of large magnetic islands: A possible mechanism for a major tokamak disruption"Physical Review A, 1978
- Simulation of Large Magnetic Islands: A Possible Mechanism for a Major Tokamak DisruptionPhysical Review Letters, 1977