摘要:

Neoclassical transport coefficients for ion and impurity species in the plateau to Pfirsch–Schlu¨ter regime are calculated using sources of particles and heat as driving forces. In the Pfirsch–Schlu¨ter regime, such sources can lead to a reversal of the usual inward flux of impurities.

ISSN:0031-9171    

DOI:10.1063/1.861716

出版商:AIP    

年代:1977

数据来源: AIP