First results from the 10Be marker experiment in JET with ITER-like wall

被引:5
|
作者
Bergsaker, H. [1 ]
Possnert, G. [2 ]
Bykov, I. [1 ]
Heinola, K. [3 ]
Petersson, P. [1 ]
Miettunen, J. [4 ]
Widdowson, A. [7 ]
Riccardo, V. [7 ]
Nunes, I. [7 ]
Stamp, M. [7 ]
Brezinsek, S.
Groth, M. [4 ]
Kurki-Suonio, T. [4 ]
Likonen, J. [5 ]
Coad, J. P. [5 ]
Borodin, D. [8 ]
Kirschner, A. [8 ]
Schmid, K. [6 ]
Krieger, K. [6 ]
机构
[1] Royal Inst Technol KTH, Assoc EURATOM VR, Div Fus Plasma Phys, Stockholm, Sweden
[2] Uppsala Univ, Assoc EURATOM VR, Tandem Lab, S-75105 Uppsala, Sweden
[3] Univ Helsinki, Dept Phys, Assoc EURATOM TEKES, Helsinki 00560, Finland
[4] Aalto Univ, Assoc EURATOM TEKES, Aalto 00076, Finland
[5] VTT, Assoc EURATOM TEKES, Espoo 02044, Finland
[6] Max Planck Inst Phys & Astrophys, EURATOM Assoc, D-85748 Garching, Germany
[7] Culham Sci Ctr, EURATOM CCFE Fus Assoc, Abingdon OX14 3DB, Oxon, England
[8] Forschungszentrum Julich, IEF Plasmaphys, TEC, Assoc EURATOM FZJ, D-52425 Julich, Germany
基金
英国工程与自然科学研究理事会;
关键词
materials; erosion; tokamaks; migration;
D O I
10.1088/0029-5515/54/8/082004
中图分类号
O35 [流体力学]; O53 [等离子体物理学];
学科分类号
070204 ; 080103 ; 080704 ;
摘要
When the ITER-like wall was installed in JET, one of the 218 Be inner wall guard limiter tiles had been enriched with Be-10 as a bulk isotopic marker. During the shutdown in 2012-2013, a set of tiles were sampled nondestructively to collect material for accelerator mass spectroscopy measurements of Be-10 concentration. The letter shows how the marker experiment was set up, presents first results and compares them to preliminary predictions of marker redistribution, made with the ASCOT numerical code. Finally an outline is shown of what experimental data are likely to become available later and the possibilities for comparison with modelling using the WallDYN, ERO and ASCOT codes are discussed.
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页数:4
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