Impact of avalanche type of transport on internal transport barrier formation in tokamak plasmas

被引:2
|
作者
Kin, F. [1 ,6 ]
Itoh, K. [2 ,3 ]
Bando, T. [4 ]
Shinohara, K. [1 ,5 ]
Oyama, N. [1 ]
Terakado, A. [1 ]
Yoshida, M. [1 ]
Sumida, S. [1 ]
机构
[1] Natl Inst Quantum Sci & Technol, Naka 3110193, Japan
[2] Chubu Univ, Frontier Res Inst, Kasugai 4878501, Japan
[3] Kyushu Univ, Res Ctr Plasma Turbulence, Kasuga 8168580, Japan
[4] Toyohashi Univ Technol, Toyohashi 4418580, Japan
[5] Univ Tokyo, Kashiwa 2778561, Japan
[6] Kyoto Univ, Inst Adv Energy, Uji 6110011, Japan
关键词
POLOIDAL ROTATION; TURBULENCE; EDGE; FLUX;
D O I
10.1038/s41598-023-46978-0
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
In magnetic fusion plasmas, a transport barrier is essential to improve the plasma confinement. The key physics behind the formation of a transport barrier is the suppression of the micro-scale turbulent transport. On the other hand, long-range transport events, such as avalanches, has been recognized to play significant roles for global profile formations. In this study, we observed the impact of the avalanche-type of transport on the formation of a transport barrier for the first time. The avalanches are found to inhibit the formation of the internal transport barrier (ITB) observed in JT-60U tokamak. We found that (1) ITBs do not form in the presence of avalanches but form under the disappearance of avalanches, (2) the surface integral of avalanche-driven heat fluxe is comparable to the time rate change of stored energy retained at the ITB onset, (3) the mean E x B flow shear is accelerated via the ion temperature gradient that is not sustained under the existence of avalanches, and (4) after the ITB formation, avalanches are damped inside the ITB, while they remain outside the ITB.
引用
收藏
页数:9
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