Abstract
Tungsten-coated carbon tiles from a poloidal
cross-section of the divertor and several types of
erosion-
deposition probes from the shadowed areas in the divertor
were studied using heavy ion elastic recoil
detection to obtain quantitative and depth-resolved
deposition patterns. Deuterium, beryllium, carbon,
nitrogen and oxygen along with tungsten and Inconel
components are the main species detected in
the studied surface region. The top of Tile 1 in the
inner divertor is the main deposition area where
the greatest amounts of deposited species are measured.
Beryllium and tungsten-containing deposits
on the probes (test mirrors and quartz microbalance)
indicate that both low-Z and high-Z metals are
transported to remote areas. Deposition of nitrogen-15
tracer used for edge cooling only at the end of
experimental campaigns in 2012 was also detected giving
evidence that nitrogen is effectively retained
in wall components.
| Original language | English |
|---|---|
| Pages (from-to) | 814-817 |
| Journal | Journal of Nuclear Materials |
| Volume | 463 |
| DOIs | |
| Publication status | Published - 2015 |
| MoE publication type | A1 Journal article-refereed |
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