Main-Ion Intrinsic Toroidal Rotation Profile Driven by Residual Stress Torque from Ion Temperature Gradient Turbulence in the DIII-D Tokamak

B. A. Grierson, W. X. Wang, S. Ethier, G. M. Staebler, D. J. Battaglia, J. A. Boedo, J. S. deGrassie, and W. M. Solomon
Phys. Rev. Lett. 118, 015002 – Published 6 January 2017

Abstract

Intrinsic toroidal rotation of the deuterium main ions in the core of the DIII-D tokamak is observed to transition from flat to hollow, forming an off-axis peak, above a threshold level of direct electron heating. Nonlinear gyrokinetic simulations show that the residual stress associated with electrostatic ion temperature gradient turbulence possesses the correct radial location and stress structure to cause the observed hollow rotation profile. Residual stress momentum flux in the gyrokinetic simulations is balanced by turbulent momentum diffusion, with negligible contributions from turbulent pinch. The prediction of the velocity profile by integrating the momentum balance equation produces a rotation profile that qualitatively and quantitatively agrees with the measured main-ion profile, demonstrating that fluctuation-induced residual stress can drive the observed intrinsic velocity profile.

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  • Received 20 May 2016

DOI:https://doi.org/10.1103/PhysRevLett.118.015002

© 2017 American Physical Society

Physics Subject Headings (PhySH)

  1. Physical Systems
Plasma Physics

Authors & Affiliations

B. A. Grierson1,*, W. X. Wang1, S. Ethier1, G. M. Staebler2, D. J. Battaglia1, J. A. Boedo3, J. S. deGrassie2, and W. M. Solomon2

  • 1Princeton Plasma Physics Laboratory, Princeton University, Princeton, New Jersey 08543, USA
  • 2General Atomics, P.O. Box 85608, San Diego, California 92186-5608, USA
  • 3Center for Energy Research, University of California San Diego, 9500 Gilman Drive, La Jolla, California 92093-0417, USA

  • *bgriers@pppl.gov

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Vol. 118, Iss. 1 — 6 January 2017

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