Composition and hydrogen isotope retention analysis of co-deposited C/Be layers

被引:46
作者
Baldwin, MJ
Schmid, K
Doerner, RP
Wiltner, A
Seraydarian, R
Linsmeier, C
机构
[1] Univ Calif San Diego, Energy Res Ctr, La Jolla, CA 92093 USA
[2] Univ Calif San Diego, Dept Mech & Aerosp Engn, La Jolla, CA 92093 USA
[3] EURATOM, Max Planck Inst Plasmaphys, D-85748 Garching, Germany
关键词
desorption; deuterium inventory; PISCES-B; erosion and deposition;
D O I
10.1016/j.jnucmat.2004.09.043
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
A neutral Be atom source and deposition probe have been installed on PISCES-B to simulate ITER diverter erosion and deposition phenomena where Be impurity concentration in the plasma, up to 10%, is expected due to first wall erosion. Graphite target erosion by deuterium plasma is found to be significantly reduced with as little as similar to 0.1% Be impurities in the plasma [K. Schmid, MJ. Baldwin, R. Doerner, these Proceedings]. Deposited Be on the target is re-eroded and leads to deposited layers in the target vicinity, that are sampled with the deposition probe. These layers are Be rich and contain only small C concentrations (< 3 at.%). The ratio of co-deposited deuterium to deposited beryllium (D/Be) decreases rapidly with increasing probe temperature up to 573 K. D/Be values are systematically lower and O/Be values higher compared to similar experiments in TPE [R.A. Causey, D.S. Walsh, J. Nucl. Mater. 254 (1998) 84]. The difference is likely due to different target-collector geometries and incident hydrogen isotope fluxes during collection. (c) 2004 Elsevier B.V. All rights reserved.
引用
收藏
页码:590 / 594
页数:5
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