Non-uniformity of fluctuation characteristics inside an edge magnetic island in Heliotron J

A. Miyashita, S. Ohshima, R. Matoike, F. Kin, S. Kobayashi, S. Kado, T. Minami, T. Mizuuchi, S. Konoshima, Hiroyuki Okada, S. Inagaki, K. Nagasaki
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Abstract

Non-uniform fluctuation characteristics are observed within an edge magnetic island in Heliotron J. The island possesses a long connection length comparable to the confined region. These fluctuations are measured using a Langmuir probe. The island’s presence is confirmed through the plasma response, observed in the modulation amplitude of electron temperature and its phase delay relative to the heat source in a heat modulation experiment. Within the island, the electron density is notably high, accompanied by distinct profiles of electron temperature and electric field, likely attributable to the magnetic island. Contrary to expectations, density fluctuations within the edge magnetic island are not locally minimized, despite the reduced gradient of the profile within the island. Statistical analysis shows a suppression of intermittent transport inside the island, while intermittent fluctuations increase towards the exterior. A further analysis to segregate turbulence-driving and spreading factors reveals that both turbulence-driven and spreading contributions are comparably significant inside the island. Additionally, the non-uniform turbulence results in a spatially structured fluctuation-driven particle flux. Overall, the experimental findings indicate that fluctuation characteristics exhibit notable non-uniformity both inside and near the island. This non-uniformity potentially complicates heat transport and may lead to three-dimensional, asymmetric transport within and at the periphery of the islands.
Heliotron J 中边缘磁岛内部波动特性的不均匀性
在 Heliotron J 中的边缘磁岛内观察到了非均匀波动特性。这些波动是使用朗缪尔探针测量的。在热调制实验中,从电子温度的调制幅度及其相对于热源的相位延迟中观察到的等离子体响应证实了磁岛的存在。在磁岛内部,电子密度明显偏高,同时伴有明显的电子温度和电场曲线,这可能与磁岛有关。与预期相反的是,尽管磁岛内部的密度波动梯度减小,但边缘磁岛内部的密度波动并没有局部最小化。统计分析显示,磁岛内部的间歇传输受到抑制,而间歇波动则向外部增加。对湍流驱动因素和扩散因素的进一步分析表明,湍流驱动因素和扩散因素在岛内的作用相当显著。此外,非均匀湍流导致了空间结构上的波动驱动颗粒通量。总之,实验结果表明,波动特性在岛内和岛附近都表现出明显的不均匀性。这种不均匀性可能会使热传输复杂化,并可能导致岛屿内部和外围的三维非对称传输。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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