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Yoon, Eisung
Fusion and Plasma Application Research Lab.
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Study of up-down poloidal density asymmetry of high-Z impurities with the new impurity version of XGCa

Author(s)
Dominski, J.Chang, C. S.Hager, R.Helander, P.Ku, S.Yoon, Eisung
Issued Date
2019-10
DOI
10.1017/S0022377819000722
URI
https://scholarworks.unist.ac.kr/handle/201301/30681
Fulltext
https://www.cambridge.org/core/journals/journal-of-plasma-physics/article/study-of-updown-poloidal-density-asymmetry-of-high-z-impurities-with-the-new-impurity-version-of-xgca/266838714C514A96F39786BFBA1AC6E2
Citation
JOURNAL OF PLASMA PHYSICS, v.85, no.5, pp.905850510
Abstract
Addition of multispecies impurity ions to the total-f gyrokinetic particle-in-cell code XGCa is reported, including a cross-verification of neoclassical physics against the NEO code. This new version of the neoclassical gyrokinetic code XGCa is used to benchmark and confirm the previous reduced-equation-based prediction that high- impurity particles in the Pfirsch–Schlüter regime can exhibit a significant level of up–down poloidal asymmetry, through the large parallel friction force, and thus influence the radial plasma transport significantly. The study is performed in a plasma with weak toroidal rotation. In comparison, when the impurity particles are in the plateau regime, the up–down poloidal asymmetry becomes weak, with the parallel friction force becoming weaker than the parallel viscous force. It is also found that the linearization of the perturbed distribution function, based on the small poloidal asymmetry assumption, can become invalid. Using the numerical data from XGCa, each term in the parallel fluid force-balance equation have been analysed to find that both the main ions and the electrons respond to the poloidal potential variation adiabatically when the high- tungsten possesses large poloidal variation.
Publisher
Cambridge University Press
ISSN
0022-3778
Keyword (Author)
fusion plasmaplasma simulation
Keyword
NEOCLASSICAL TRANSPORTCOLLISION OPERATORSIMULATIONPLASMACONDUCTIVITYEQUILIBRIA

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