50th Annual Meeting of the Division of Plasma Physics
Volume 53, Number 14
Monday–Friday, November 17–21, 2008;
Dallas, Texas
Session YI2: Transport and Zonal Flows
9:45 AM–12:45 PM,
Friday, November 21, 2008
Room: Landmark B
Chair: Greg Hammett, Princeton Plasma Physics Laboratory
Abstract ID: BAPS.2008.DPP.YI2.6
Abstract: YI2.00006 : Gyrokinetic Turbulence Driven Toroidal Momentum Transport and Comparison to Experimental Observations*
12:15 PM–12:45 PM
Preview Abstract
Abstract
Author:
Weixing Wang
(Princeton Plasma Physics Laboratory)
Global gyrokinetic simulations using the GTS code [1] have
found that a large inward flux of toroidal momentum is driven
robustly in the post saturation phase of ion temperature
gradient (ITG) turbulence. As a consequence, core plasma
rotation spins up resulting in $\Delta u_{\parallel}$ a few
percent of $v_{th}$ in the case with no momentum source at the
edge. The underlying physics for the inward flux is identified
to be the generation of residual stress due to the $k_
{\parallel}$ symmetry breaking [2] induced by self-generated
zonal flow shear which is quasi-stationary in global
simulations. The elatively low level momentum flux in the long-
time steady state appears to be approximately diffusive, with
effective $\chi_{\phi}/\chi_i$ on the order of unity, in broad
agreement with experimental observations and theory predictions
for ITG turbulence [3]. Neoclassical simulations using the GTC-
NEO code [4] also show that the ion temperature gradient can
drive a significant inward nondiffusive momentum flux. However,
the overall neoclassical contribution to the momentum transport
is negligibly small compared to experimental levels for NSTX
and DIII-D plasmas. It is also found that finite residual
turbulence can survive strong mean ExB shear flow induced
damping. This residual turbulence in the presence of strong
$\bf{E}\times\bf{B}$ shear may drive an insignificant ion heat
flux reasonably close to the neoclassical value, and a finite
momentum flux significantly higher than the neoclassical level.
Moreover, the equilibrium $\bf{E}\times\bf{B}$ flow shear is
found to reduce the turbulence driven transport for energy more
efficiently than for momentum. These findings may offer an
explanation for rather peculiar observations of near
neoclassical ion heat and anomalous momentum transport in
experiments, which has been often observed in various machines,
but with little theoretical understanding. [1] W.X. Wang et
al., Phys. Plasmas 14, 072306 (2007). [2] O.D. Gurcan et al.,
Phys. Plasmas 14, 042306 (2007). [3] N. Mattor and P.H.
Diamond, Phys. Fluids 31, 1180 (1988). [4] W.X. Wang et al.,
Phys. Plasmas 13, 082501 (2006). In collaboration
with: T.S. Hahm, S. Ethier, S.M. Kaye, W.W. Lee, G. Rewoldt,
W.M. Tang (PPPL), P.H. Diamond (UCSD), M. Adams (Columbia U.).
*Work supported by U.S. DOE Contract DE-AC02-76-CH03073 and the SciDAC GPS-TTBP project.
To cite this abstract, use the following reference: http://meetings.aps.org/link/BAPS.2008.DPP.YI2.6