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Simulations of tokamak disruptions including self-consistent temperature evolution

A. Bondeson1986年被引用 32Nuclear FusionIF 3出版社

Three-dimensional simulations of tokamaks have been carried out, including self-consistent temperature evolution with a highly anisotropic thermal conductivity. The simulations extend over the transport time-scale and address the question of how disruptive current profiles arise at low-q or high-density operation. Sharply defined disruptive events are triggered by the m/n = 2/1 resistive tearing mode, which is mainly affected by local current gradients near the q = 2 surface. If the global current gradient between q = 2 and q = 1 is sufficiently steep, the m = 2 mode starts a shock which accelerates towards the q = 1 surface, leaving stochastic fields, a flattened temperature profile and turbulent plasma behind it. For slightly weaker global current gradients, a shock may form, but it will dissipate before reaching q = 1 and may lead to repetitive minidisruptions which flatten the temperature profile in a region inside the q = 2 surface.

日本語訳

トカマクの三次元シミュレーションを、強い異方性を持つ熱伝導率を伴う自己無撞着な温度発展を含めて実施した。シミュレーションは輸送時間スケールにわたり、低q運転または高密度運転において、どのようにしてディスラプションを引き起こす電流分布が生じるのかという問題を扱う。明確に定義されたディスラプション事象は、q=2面付近の局所的な電流勾配に主に影響されるm/n=2/1抵抗性テアリングモードによって引き起こされる。q=2とq=1の間の大域的電流勾配が十分に急峻である場合、m=2モードはq=1面に向かって加速するショックを開始し、その後方に確率的磁場構造、平坦化された温度分布、および乱流プラズマを残す。大域的電流勾配がわずかに弱い場合、ショックは形成され得るが、q=1に到達する前に消散し、q=2面内の領域で温度分布を平坦化する反復的なミニディスラプションを引き起こす可能性がある。

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Plasma disruptionTokamak disruption
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