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17–22 Oct 2016
Kyoto International Conference Center
Japan timezone

Turbulence-Flow Coupling and Poloidal Main-Ion Flow Acceleration Preceding the L-H Transition

19 Oct 2016, 08:30
4h
Kyoto International Conference Center

Kyoto International Conference Center

Takaragaike, Sakyo-ku, Kyoto 606-0001 Japan
Poster EXS - Magnetic Confinement Experiments: Stability Poster 3

Speaker

Mr L. Schmitz (University of California-Los Angeles)

Description

Understanding flow drive and damping across the relevant ion collisionality range is crucial for connecting the L-H transition trigger physics to the macroscopic L-H power threshold scaling. This is of utmost importance for minimizing the auxiliary heating power required for H-mode access in burning plasmas. It is shown here for the first time that the main-ion poloidal flow acceleration is quantitatively consistent with Reynolds-stress-driven shear flow amplification across the entire edge shear layer, leading to the observed dipolar shear layer structure inside the last closed flux surface (LCFS). The poloidal flow damping rate is found to be consistent with the neoclassical plateau regime at intermediate density n=3x10^19 m^-3. This work in He plasmas substantially extends previous work on L-H transitions induced by limit cycle oscillations (LCO), and on fast (regular) L-H transitions, [1-3]. We present direct, high resolution measurements of the poloidal and toroidal main ion flow during the trigger phase of the L-H transition, using He main-ion CER. The measured E×B velocity modulation at the start of the LCO is in phase with the local ion poloidal velocity modulation, indicating flow in opposite directions just inside the LCFS and near the bottom of the E_r well. In contrast, the laboratory frame toroidal velocity is not significantly modulated during LCO. It is demonstrated that (i) the Reynolds stress gradient changes sign across the shear layer, consistent with the observed poloidal flow propagation in opposite directions; (ii) the measured Reynolds stress drive is quantitatively balanced by the ion flow acceleration and damping terms. This data presents compelling quantitative evidence that the L-mode-LCO transition is triggered via E×B shear flow amplification mediated by the perpendicular Reynolds stress gradient. Long-range toroidal E×B flow correlation in the LCO peaks at intermediate plasma density around the L-H power threshold minimum. This work was supported by the US Department of Energy under DE-FG02-08ER54984, DE-AC02-09CH11466, DE-FG02-89ER53296, DE-FG02-08ER 54999, DE-FC02-04ER54698, DE-AC05-06OR23100 and DE-FG02-06ER54871. [1] L. Schmitz, et al., Phys. Rev. Lett. 108, 155002 (2012). [2] G. Tynan et al., Nucl. Fusion 53, 073053 (2013). [3] Z. Yan, et al., Phys Rev. Lett. 107, 055004 (2014).
Country or International Organization United States
Paper Number EX/P3-11

Primary author

Mr L. Schmitz (University of California-Los Angeles)

Co-authors

C. Chrystal (Oak Ridge Associated Universities) C.C. Petty (General Atomics) David Eldond (Princeton Plasma Physics Laboratory) G.R. McKee (University of Wisconsin-Madison) K.H. Burrell (General Atomics) L. Bardoczi (University of California-Los Angeles) L. Zeng (University of California-Los Angeles) P. Gohil (General Atomics) P.H. Diamond (University of California-San Diego) R. Groebner (General Atomics) T.L. Rhodes (University of California-Los Angeles) W.A. Peebles (University of California-Los Angeles) Z. Yan (University of Wisconsin-Madison)

Presentation materials