Dynamics of erosion and deposition in tokamaks

被引:28
作者
Kreter, A. [1 ]
Brezinsek, S. [1 ]
Coad, J. P. [2 ]
Esser, H. G. [1 ]
Fundamenski, W. [2 ]
Philipps, V. [1 ]
Pitts, R. A. [3 ]
Rohde, V. [4 ]
Tanabe, T. [5 ]
Widdowson, A. [2 ]
机构
[1] Forschungszentrum Julich, Inst Energieforsch Plasmaphys, Assoc EURATOM FZJ,Trilateral Euregio Cluster, D-52425 Julich, Germany
[2] UKAEA Euratom Fus Assoc, Culham Sci Ctr, Abingdon, Oxon, England
[3] Assoc EURATOM EPFL, CRPP, CH-1015 Lausanne, Switzerland
[4] Max Planck Inst Plasma Phys, EURATOM Assoc, D-85748 Garching, Germany
[5] Kyushu Univ, Interdisciplinary Grad Sch Engn Sci, Higashi Ku, Fukuoka 8128581, Japan
基金
英国工程与自然科学研究理事会;
关键词
ASDEX UPGRADE; QUARTZ MICROBALANCE; RE-DEPOSITION; EDGE PLASMAS; DIII-D; DIVERTOR; JET; CARBON; RETENTION; TRANSPORT;
D O I
10.1016/j.jnucmat.2009.01.041
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
In recent years, a general qualitative understanding has been reached about the major pathways of material migration in divertor tokamaks. Main chamber wall components have been identified as the major source of material erosion. The eroded material is transported by scrape-off layer flows, in the case of the ion B x del B drift pointing towards the X-point, predominately towards the inner divertor leg, where it is deposited in the form of amorphous layers. On JET, where carbon is the main plasma-facing material, it has been found that the presence of deposited carbon rich layers determines the dynamic characteristics of further re-distribution of carbon, in particular towards remote areas. The transport from the strike point to the deposition location is mainly line-of-sight. The amount of eroded carbon depends on the surface type, with lower rates for the bare CFC and higher rates for deposited layers. The erosion rates in the inner divertor increase non-linearly with increasing ELM energies. (C) 2009 Elsevier B.V. All rights reserved.
引用
收藏
页码:38 / 43
页数:6
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