Transport by intermittent convection in the boundary of the DIII-D tokamak

被引:335
作者
Boedo, JA [1 ]
Rudakov, D
Moyer, R
Krasheninnikov, S
Whyte, D
McKee, G
Tynan, G
Schaffer, M
Stangeby, P
West, P
Allen, S
Evans, T
Fonck, R
Hollmann, E
Leonard, A
Mahdavi, A
Porter, G
Tillack, M
Antar, G
机构
[1] Univ Calif San Diego, Energy Res Ctr, La Jolla, CA 92093 USA
[2] Univ Wisconsin, Madison, WI 53706 USA
[3] Gen Atom Co, San Diego, CA USA
[4] Univ Toronto, Toronto, ON, Canada
[5] Lawrence Livermore Natl Lab, Livermore, CA USA
关键词
D O I
10.1063/1.1406940
中图分类号
O35 [流体力学]; O53 [等离子体物理学];
学科分类号
070204 ; 080103 ; 080704 ;
摘要
Intermittent plasma objects (IPOs) featuring higher pressure than the surrounding plasma, and responsible for similar to 50% of the ExB(T) radial transport, are observed in the scrape off layer (SOL) and edge of the DIII-D tokamak [J. Watkins , Rev. Sci. Instrum. 63, 4728 (1992)]. Conditional averaging reveals that the IPOs, produced at a rate of similar to 3x10(3) s(-1), are positively charged and also polarized, featuring poloidal electric fields of up to 4000 V/m. The IPOs move poloidally at speeds of up to 5000 m/s and radially with ExB(T)/B-2 velocities of similar to 2600 m/s near the last closed flux surface (LCFS), and similar to 330 m/s near the wall. The IPOs slow down as they shrink in radial size from 4 cm at the LCFS to 0.5 cm near the wall. The IPOs appear in the SOL of both L and H mode discharges and are responsible for nearly 50% of the SOL radial ExB transport at all radii; however, they are highly reduced in absolute amplitude in H-mode conditions. (C) 2001 American Institute of Physics.
引用
收藏
页码:4826 / 4833
页数:8
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