磁撕裂的早期内部检测及其对托卡马克磁流体动力学稳定性的影响

M. D. Pandya, B. Chapman, K. McCollam, R. A. Myers, J. Sarff, B. S. Victor, D. P. Brennan, D. Brower, J. Chen, W. X. Ding, C. T. Holcomb, N. Logan, E. Strait
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引用次数: 0

摘要

利用法拉第效应极坐标法对 DIII-D 托卡马克进行的内部波动测量显示,在等离子体外部的传感线圈检测到撕裂模式之前,就已经出现了环形模式数 n = 3 的撕裂模式。该模式出现在 n = 2、1 模式之前,并且是在理想壁扭结贝塔极限值低于传感线圈首次探测到的值时通过内部测量首次探测到的。当首次检测到该模式时,线性电阻稳定性参数 Δ′ 显示出边缘稳定性,并一直持续到后来模式振幅开始随时间线性增加时--这共同表明了该模式的新古典起源。
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Early internal detection of magnetic tearing and implications for tokamak magnetohydrodynamic stability
Internal fluctuation measurements with Faraday-effect polarimetry in the DIII-D tokamak reveal the onset of a tearing mode with toroidal mode number n = 3 well before it is detected by the sensing coils external to the plasma. This mode appears before the n = 2, 1 modes and is first detected with internal measurements at a lower value of the ideal-wall kink beta limit than is indicated at the time of first detection by the sensing coils. When the mode is first detected, the linear resistive stability parameter, Δ′, indicates marginal stability and continues to do so until later when the mode amplitude begins increasing linearly with time—together suggesting a neoclassical origin for this mode.
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