Abstract
13C methane puffing experiments were conducted on DIII-D in both L- and ELMy H-mode conditions. The puffing was toroidally symmetric into the crown of a series of well-characterized lower single-null discharges. The hydrocarbon breakup, carbon transport and deposition were modeled using the OEDGE interpretive code. Three separate hypotheses were tested using OEDGE to try to reproduce the experimental deposition: Radial variation of fast parallel flow, erosion of the puffed 13C deposited in the divertor, and a pinch in the inner scrape off layer (SOL) towards the separatrix. A fast parallel flow was imposed for all hypotheses. The magnitude and the distribution of the 13C deposition resulting from each hypothesis are compared. A fast parallel flow in the SOL toward the inner divertor combined with a pinch/drift of 10-30 m/s in the inner SOL towards the separatrix roughly reproduces the deposition in both the L- and H-mode experiments.
Original language | English |
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Pages (from-to) | 376-379 |
Number of pages | 4 |
Journal | Journal of Nuclear Materials |
Volume | 390-391 |
DOIs | |
Publication status | Published - 15 Jun 2009 |
MoE publication type | A1 Journal article-refereed |