Abstract
Tungsten erosion and re-deposition at the upper outer divertor of the Experimental Advanced Superconducting Tokamak has been modelled using the 3D Monte Carlo code ERO. The measured divertor plasma condition in attached L mode discharges with upper single null configuration has been used to build the background plasma in the simulations. The tungsten gross erosion rate is mainly determined by carbon impurity in the background plasma. Increasing carbon concentration can first increase and afterwards suppress the tungsten erosion rate. Taking into account the material mixing surface model, the influence of eroded particles returning to the surface on sputtering has been studied. Sputtering by eroded particles returning to the surface can significantly enhance the gross erosion by reduction of the carbon ratio within the surface interaction layer and by increasing the erosion rate due to sputtering by both eroded tungsten and carbon particles. Modelling indicates that carbon deposition occurs on the dome plate and part of the vertical plate close to the dome plate, whereas tungsten net erosion occurs on most of the vertical plate. The modelling results are in reasonable agreement with the experimental WI spectroscopy.
Original language | English |
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Article number | 092512 |
Journal | Physics of Plasmas |
Volume | 24 |
Issue number | 9 |
DOIs | |
State | Published - 1 Sep 2017 |
Externally published | Yes |
Bibliographical note
Publisher Copyright:© 2017 Author(s).
Funding
This work has been supported by the National Magnetic Confinement Fusion Science Program of China (Grant Nos. 2013GB107004 and 2013GB105003), the National Natural Science Foundation of China (Grant Nos. 11375010, 11675218, and 11575243), and the Sino-German Center for Research Promotion under Contract No. GZ769.
Funders | Funder number |
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National Natural Science Foundation of China | 11575243, 11675218, 11375010 |
Chinesisch-Deutsche Zentrum für Wissenschaftsförderung | GZ769 |
National Magnetic Confinement Fusion Program of China | 2013GB105003, 2013GB107004 |