Study of DIII-D tungsten erosion processes by using a carbon–tungsten mixed material model
Creators
- 1. University of Science and Technology of China, Hefei (China)
- 2. Oak Ridge Associated Universities, Oak Ridge, TN (United States)
- 3. General Atomics, PO Box 85608, San Diego, CA 92186-5608 (United States)
- 4. University of Toronto Institute for Aerospace Studies, Toronto M3H 5T6 (Canada)
- 5. Oak Ridge National Laboratory, Oak Ridge, TN 37830 (United States)
Description
Highlights: • Both inter- and intra-ELM tungsten erosion mechanisms are studied by using carbon-tungsten mixed material model in this paper, • The tungsten erosion is found to be dominated by carbon, with different origin for carbon between ELMs and during ELMs. • For inter-ELM, the tungsten is mainly eroded by locally redeposited low charge state carbon. • For intra-ELM, the C6+ originated from the pedestal region is found to dominate the tungsten erosion in the near separatrix region, whereas the locally redeposited low charge state C fluxes lead to a nonnegligible tungsten erosion in the outer SOL region. • These results suggest that modeling of W erosion during ELMs needs to include impurity transport from the pedestal to the divertor during an ELM. -- Abstract: The tungsten erosion process for an H-mode discharge from the DIII-D Metal Rings Campaign is modeled using OEDGE and TRIM.SP. The OEDGE code is employed to calculate tungsten erosion between edge-localized modes (ELMs). Then a newly developed semi-analytical carbon–tungsten mixed material model based on TRIM.SP is used to simulate the intra-ELM tungsten gross erosion profiles. The tungsten erosion is found to be dominated by carbon, with different origin for carbon between ELMs and during ELMs. For inter-ELM, the tungsten is mainly eroded by locally redeposited low charge state carbon, while for intra-ELM, the C6+ originated from the pedestal region is found to dominate the tungsten erosion in the near separatrix region, whereas the locally redeposited low charge state C fluxes lead to a nonnegligible tungsten erosion in the outer SOL region. These results suggest that modeling of W erosion during ELMs needs to include impurity transport from the pedestal to the divertor during an ELM. In addition, for both inter- and intra-ELM simulation, a carbon coverage of 30% on the tungsten surface is needed to reproduce the measured erosion at the divertor target.
Availability note (English)
Available from http://dx.doi.org/10.1016/j.nme.2018.12.020Additional details
Identifiers
- DOI
- 10.1016/j.nme.2018.12.020;
- PII
- S2352179118301352;
Publishing Information
- Journal Title
- Nuclear Materials and Energy
- Journal Volume
- 18
- Journal Page Range
- p. 141-146
- ISSN
- 2352-1791
INIS
- Country of Publication
- United Kingdom
- Country of Input or Organization
- International Atomic Energy Agency (IAEA)
- INIS RN
- 54120444
- Subject category
- S70: PLASMA PHYSICS AND FUSION TECHNOLOGY;
- Descriptors DEI
- CARBON; CHARGE STATES; COMPUTERIZED SIMULATION; DIVERTORS; DOUBLET-3 DEVICE; EDGE LOCALIZED MODES; EROSION; H-MODE PLASMA CONFINEMENT; PLASMA; SOLS; SURFACES; TUNGSTEN
- Descriptors DEC
- CLOSED PLASMA DEVICES; COLLOIDS; CONFINEMENT; DISPERSIONS; ELEMENTS; INSTABILITY; MAGNETIC CONFINEMENT; METALS; NONMETALS; PLASMA CONFINEMENT; PLASMA INSTABILITY; PLASMA MACROINSTABILITIES; REFRACTORY METALS; SIMULATION; THERMONUCLEAR DEVICES; TOKAMAK DEVICES; TRANSITION ELEMENTS
Optional Information
- Copyright
- Copyright (c) 2018 The Authors. Published by Elsevier Ltd.