Understanding the L-H isotope effect at the DIII-D tokamak and advancements in synthetic turbulence diagnostics

Author:

Callahan K.J.ORCID,Schmitz L.ORCID,Pratt Q.ORCID,Carter T.A.ORCID,Wang G.ORCID,Zhang H.,Holland C.ORCID,Haskey S.R.ORCID,Angulo A.ORCID,Bortolon A.ORCID,Effenberg F.ORCID,Belli E.A.ORCID,Chrystal C.ORCID,Thome K.E.ORCID,Ashourvan A.ORCID,Neiser T.ORCID,Knolker M.ORCID,Khabanov F.ORCID,Yan Z.ORCID,McKee G.R.ORCID,Chaban R.ORCID,Wilcox R.S.ORCID,Holm A.ORCID,Scotti F.ORCID,Truong D.ORCID,Gerrú R.ORCID

Abstract

Abstract It is determined that while heat flux differences between hydrogen and deuterium isotope experiments result from natural differences in carbon impurity content at DIII-D, it is not the origin of the low to high confinement mode (L-H) transition isotope effect. More specifically, a two times larger edge radial electric field in hydrogen compared to deuterium is uncovered and believed to play an important role. The origin of this radial electric field difference is determined to have two possible origins: differences in poloidal rotation and turbulent Reynolds stress in the closed field line region, and increased outer strike point temperatures and space potentials on open field lines. Experimental observations from both profile and turbulence diagnostics are supported by nonlinear gyrokinetic simulations using the code CGYRO. Simulations illustrated heat transport isotope effects in the plasma edge and shear layer resulting from differences in impurity content, electron non-adiabaticity, and main ion mass dependent E × B shear stabilization. Turbulence prediction comparisons from flux-matched CGYRO simulations to experimental measurements including electron temperature, density and velocity fluctuations are found to be in good agreement with available data. A dedicated DIII-D experiment in hydrogen was performed to seed more carbon than naturally occurring, to match deuterium experiments, and possibly reduce the L-H power threshold based on gyro-kinetic predictions. To our surprise, while ion temperature gradient (ITG) turbulence was stabilized, nodiscernible change in L-H power threshold were observed in these special hydrogen experiments. In particular, it is noticed that the edge radial electric field and Reynolds stress were observed as nearly unchanging in the presence of ITG stabilization. These experimental data have enabled a more comprehensive picture of the multitude of isotope effects at play in fusion experiments, and the important potential connection between the confined and unconfined plasma regions in regulating L-H transition dynamics.

Funder

Fusion Energy Sciences

Publisher

IOP Publishing

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