Abstract
The isotope effect, hydrogen (H) versus deuterium (D), on the gross beryllium (Be) erosion yield has been measured in ohmic limiter plasmas in JET tokamak by spectroscopic means. A simplified method to extract the effective sputtering yield from the quotient of the radiances of the D α or D 3 and the Be II lines at 527 nm was applied. A clear isotope effect has been found, the erosion yield of D being about a factor of 2 larger compared to H in the whole explored plasma density range. This is in agreement with physical sputtering data obtained with H+ and D+ ion beams and also with material surface computer simulations. The already published contribution of chemically assisted physical sputtering has been also identified here. Currently the study is being extended to tritium (T) and D-T plasmas and the effect of helium mixtures.
Original language | English |
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Article number | 126021 |
Journal | Nuclear Fusion |
Volume | 62 |
Issue number | 12 |
DOIs | |
State | Published - Dec 2022 |
Externally published | Yes |
Bibliographical note
Publisher Copyright:© EURATOM 2022.
Funding
This work has been carried out within the framework of the EUROfusion Consortium, funded by the European Union via the Euratom Research and Training Programme (Grant Agreement No. 101052200—EUROfusion). Views and opinions expressed are however those of the author(s) only and do not necessarily reflect those of the European Union or the European Commission. Neither the European Union nor the European Commission can be held responsible for them.
Funders | Funder number |
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European Commission | 101052200—EUROfusion |
Keywords
- JET
- beryllium
- erosion
- isotope
- limiter
- spectroscopy
- sputtering