Loading…

Erosion at the inner wall of JET during the discharge campaign 2013–2014

•Erosion in the recessed areas of the inner wall during the second JET-ILW campaign was studied.•Rate and distribution of W erosion were the same as in first JET-ILW campaign and JET-C campaigns.•Erosion of Be decreased by a factor of about 2. The erosion of Be and W marker layers was investigated u...

Full description

Saved in:
Bibliographic Details
Published in:Nuclear materials and energy 2017-05, Vol.11 (C), p.20-24
Main Authors: Krat, S., Mayer, M., Bykov, I., Lungu, C.P., Aubin, G. de Saint, Widdowson, A., Carvalho, I.S.
Format: Article
Language:English
Citations: Items that this one cites
Items that cite this one
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
cited_by cdi_FETCH-LOGICAL-c481t-390306dacc4ca262f7c364d30e52ce1aebd78bd3f24ea6ff5e0962161339ebf33
cites cdi_FETCH-LOGICAL-c481t-390306dacc4ca262f7c364d30e52ce1aebd78bd3f24ea6ff5e0962161339ebf33
container_end_page 24
container_issue C
container_start_page 20
container_title Nuclear materials and energy
container_volume 11
creator Krat, S.
Mayer, M.
Bykov, I.
Lungu, C.P.
Aubin, G. de Saint
Widdowson, A.
Carvalho, I.S.
description •Erosion in the recessed areas of the inner wall during the second JET-ILW campaign was studied.•Rate and distribution of W erosion were the same as in first JET-ILW campaign and JET-C campaigns.•Erosion of Be decreased by a factor of about 2. The erosion of Be and W marker layers was investigated using long-term samples containing marker layers during the second ITER-like wall discharge campaign 2013–2014 (ILW-2). The samples were mounted in Be coated Inconel tiles between the inner wall guard limiters (IWGL). They were analyzed using elastic backscattering (EBS) before and after exposure. All samples showed noticeable erosion. The results were compared to the data for Be and W erosion rates for the first 2011–2012 JET ITER-like wall (ILW-1) campaign, and to the data for C erosion during the 2005–2009 campaign when JET was operated with a carbon wall. The mean W erosion rates and the toroidal and poloidal distributions of the W erosion were nearly the same for the ILW-1 and ILW-2 campaigns. The mean erosion rate of Be during the ILW-2 campaign was smaller by a factor of about two compared to the ILW-1 campaign.
doi_str_mv 10.1016/j.nme.2017.02.026
format article
fullrecord <record><control><sourceid>elsevier_doaj_</sourceid><recordid>TN_cdi_doaj_primary_oai_doaj_org_article_665d14dd3ef0469ba5720074f52c5d97</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><els_id>S2352179116303003</els_id><doaj_id>oai_doaj_org_article_665d14dd3ef0469ba5720074f52c5d97</doaj_id><sourcerecordid>S2352179116303003</sourcerecordid><originalsourceid>FETCH-LOGICAL-c481t-390306dacc4ca262f7c364d30e52ce1aebd78bd3f24ea6ff5e0962161339ebf33</originalsourceid><addsrcrecordid>eNqFUUtOwzAQjRBIoMIB2PkApHhsx6nFqirlJyQ2wNZy7HHr0iaVk1Kx4w7ckJNgWoRgA9JIY43fe_N5WXYMtA8U5OmsXy-wzyiUfcpSyJ3sgPGC5VAq2P3x3s-O2nZGKQXFBkzwg-xmHJs2NDUxHemmSEJdYyRrM5-TxpOb8T1xqxjqyebThdZOTZwgsWaxNGFSk9SUv7--pSQOsz1v5i0efeVe9nAxvh9d5bd3l9ej4W1uxQC6nCvKqXTGWmENk8yXlkvhOMWCWQSDlSsHleOeCTTS-wKpkgwkcK6w8pz3suutrmvMTC9jWJj4ohsT9KbQxIk2sQt2jlrKwoFwjqOnQqrKFCWjtBQ-tSqcKpPWyVarXeNyVf1SOw-Pw43aaqW5UgMBCZ7_D3_qppoBpJkTHrZ4m67cRvTfDKD60zo908k6_WmdpiyFTJyzLQfTDZ8DRt3agLVFFyLaLi0Z_mB_ACsHn5E</addsrcrecordid><sourcetype>Open Website</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype></control><display><type>article</type><title>Erosion at the inner wall of JET during the discharge campaign 2013–2014</title><source>ScienceDirect Journals</source><creator>Krat, S. ; Mayer, M. ; Bykov, I. ; Lungu, C.P. ; Aubin, G. de Saint ; Widdowson, A. ; Carvalho, I.S.</creator><creatorcontrib>Krat, S. ; Mayer, M. ; Bykov, I. ; Lungu, C.P. ; Aubin, G. de Saint ; Widdowson, A. ; Carvalho, I.S. ; JET contributors</creatorcontrib><description>•Erosion in the recessed areas of the inner wall during the second JET-ILW campaign was studied.•Rate and distribution of W erosion were the same as in first JET-ILW campaign and JET-C campaigns.•Erosion of Be decreased by a factor of about 2. The erosion of Be and W marker layers was investigated using long-term samples containing marker layers during the second ITER-like wall discharge campaign 2013–2014 (ILW-2). The samples were mounted in Be coated Inconel tiles between the inner wall guard limiters (IWGL). They were analyzed using elastic backscattering (EBS) before and after exposure. All samples showed noticeable erosion. The results were compared to the data for Be and W erosion rates for the first 2011–2012 JET ITER-like wall (ILW-1) campaign, and to the data for C erosion during the 2005–2009 campaign when JET was operated with a carbon wall. The mean W erosion rates and the toroidal and poloidal distributions of the W erosion were nearly the same for the ILW-1 and ILW-2 campaigns. The mean erosion rate of Be during the ILW-2 campaign was smaller by a factor of about two compared to the ILW-1 campaign.</description><identifier>ISSN: 2352-1791</identifier><identifier>EISSN: 2352-1791</identifier><identifier>DOI: 10.1016/j.nme.2017.02.026</identifier><language>eng</language><publisher>Elsevier Ltd</publisher><ispartof>Nuclear materials and energy, 2017-05, Vol.11 (C), p.20-24</ispartof><rights>2017 The Authors</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c481t-390306dacc4ca262f7c364d30e52ce1aebd78bd3f24ea6ff5e0962161339ebf33</citedby><cites>FETCH-LOGICAL-c481t-390306dacc4ca262f7c364d30e52ce1aebd78bd3f24ea6ff5e0962161339ebf33</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.sciencedirect.com/science/article/pii/S2352179116303003$$EHTML$$P50$$Gelsevier$$Hfree_for_read</linktohtml><link.rule.ids>230,314,780,784,885,3549,27924,27925,45780</link.rule.ids><backlink>$$Uhttps://urn.kb.se/resolve?urn=urn:nbn:se:kth:diva-211621$$DView record from Swedish Publication Index$$Hfree_for_read</backlink><backlink>$$Uhttps://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-399841$$DView record from Swedish Publication Index$$Hfree_for_read</backlink></links><search><creatorcontrib>Krat, S.</creatorcontrib><creatorcontrib>Mayer, M.</creatorcontrib><creatorcontrib>Bykov, I.</creatorcontrib><creatorcontrib>Lungu, C.P.</creatorcontrib><creatorcontrib>Aubin, G. de Saint</creatorcontrib><creatorcontrib>Widdowson, A.</creatorcontrib><creatorcontrib>Carvalho, I.S.</creatorcontrib><creatorcontrib>JET contributors</creatorcontrib><title>Erosion at the inner wall of JET during the discharge campaign 2013–2014</title><title>Nuclear materials and energy</title><description>•Erosion in the recessed areas of the inner wall during the second JET-ILW campaign was studied.•Rate and distribution of W erosion were the same as in first JET-ILW campaign and JET-C campaigns.•Erosion of Be decreased by a factor of about 2. The erosion of Be and W marker layers was investigated using long-term samples containing marker layers during the second ITER-like wall discharge campaign 2013–2014 (ILW-2). The samples were mounted in Be coated Inconel tiles between the inner wall guard limiters (IWGL). They were analyzed using elastic backscattering (EBS) before and after exposure. All samples showed noticeable erosion. The results were compared to the data for Be and W erosion rates for the first 2011–2012 JET ITER-like wall (ILW-1) campaign, and to the data for C erosion during the 2005–2009 campaign when JET was operated with a carbon wall. The mean W erosion rates and the toroidal and poloidal distributions of the W erosion were nearly the same for the ILW-1 and ILW-2 campaigns. The mean erosion rate of Be during the ILW-2 campaign was smaller by a factor of about two compared to the ILW-1 campaign.</description><issn>2352-1791</issn><issn>2352-1791</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2017</creationdate><recordtype>article</recordtype><sourceid>DOA</sourceid><recordid>eNqFUUtOwzAQjRBIoMIB2PkApHhsx6nFqirlJyQ2wNZy7HHr0iaVk1Kx4w7ckJNgWoRgA9JIY43fe_N5WXYMtA8U5OmsXy-wzyiUfcpSyJ3sgPGC5VAq2P3x3s-O2nZGKQXFBkzwg-xmHJs2NDUxHemmSEJdYyRrM5-TxpOb8T1xqxjqyebThdZOTZwgsWaxNGFSk9SUv7--pSQOsz1v5i0efeVe9nAxvh9d5bd3l9ej4W1uxQC6nCvKqXTGWmENk8yXlkvhOMWCWQSDlSsHleOeCTTS-wKpkgwkcK6w8pz3suutrmvMTC9jWJj4ohsT9KbQxIk2sQt2jlrKwoFwjqOnQqrKFCWjtBQ-tSqcKpPWyVarXeNyVf1SOw-Pw43aaqW5UgMBCZ7_D3_qppoBpJkTHrZ4m67cRvTfDKD60zo908k6_WmdpiyFTJyzLQfTDZ8DRt3agLVFFyLaLi0Z_mB_ACsHn5E</recordid><startdate>20170501</startdate><enddate>20170501</enddate><creator>Krat, S.</creator><creator>Mayer, M.</creator><creator>Bykov, I.</creator><creator>Lungu, C.P.</creator><creator>Aubin, G. de Saint</creator><creator>Widdowson, A.</creator><creator>Carvalho, I.S.</creator><general>Elsevier Ltd</general><general>Elsevier</general><scope>6I.</scope><scope>AAFTH</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>ADTPV</scope><scope>AFDQA</scope><scope>AOWAS</scope><scope>D8T</scope><scope>D8V</scope><scope>ZZAVC</scope><scope>ACNBI</scope><scope>DF2</scope><scope>DOA</scope></search><sort><creationdate>20170501</creationdate><title>Erosion at the inner wall of JET during the discharge campaign 2013–2014</title><author>Krat, S. ; Mayer, M. ; Bykov, I. ; Lungu, C.P. ; Aubin, G. de Saint ; Widdowson, A. ; Carvalho, I.S.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c481t-390306dacc4ca262f7c364d30e52ce1aebd78bd3f24ea6ff5e0962161339ebf33</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2017</creationdate><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Krat, S.</creatorcontrib><creatorcontrib>Mayer, M.</creatorcontrib><creatorcontrib>Bykov, I.</creatorcontrib><creatorcontrib>Lungu, C.P.</creatorcontrib><creatorcontrib>Aubin, G. de Saint</creatorcontrib><creatorcontrib>Widdowson, A.</creatorcontrib><creatorcontrib>Carvalho, I.S.</creatorcontrib><creatorcontrib>JET contributors</creatorcontrib><collection>ScienceDirect Open Access Titles</collection><collection>Elsevier:ScienceDirect:Open Access</collection><collection>CrossRef</collection><collection>SwePub</collection><collection>SWEPUB Kungliga Tekniska Högskolan full text</collection><collection>SwePub Articles</collection><collection>SWEPUB Freely available online</collection><collection>SWEPUB Kungliga Tekniska Högskolan</collection><collection>SwePub Articles full text</collection><collection>SWEPUB Uppsala universitet full text</collection><collection>SWEPUB Uppsala universitet</collection><collection>Directory of Open Access Journals (DOAJ)</collection><jtitle>Nuclear materials and energy</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Krat, S.</au><au>Mayer, M.</au><au>Bykov, I.</au><au>Lungu, C.P.</au><au>Aubin, G. de Saint</au><au>Widdowson, A.</au><au>Carvalho, I.S.</au><aucorp>JET contributors</aucorp><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Erosion at the inner wall of JET during the discharge campaign 2013–2014</atitle><jtitle>Nuclear materials and energy</jtitle><date>2017-05-01</date><risdate>2017</risdate><volume>11</volume><issue>C</issue><spage>20</spage><epage>24</epage><pages>20-24</pages><issn>2352-1791</issn><eissn>2352-1791</eissn><abstract>•Erosion in the recessed areas of the inner wall during the second JET-ILW campaign was studied.•Rate and distribution of W erosion were the same as in first JET-ILW campaign and JET-C campaigns.•Erosion of Be decreased by a factor of about 2. The erosion of Be and W marker layers was investigated using long-term samples containing marker layers during the second ITER-like wall discharge campaign 2013–2014 (ILW-2). The samples were mounted in Be coated Inconel tiles between the inner wall guard limiters (IWGL). They were analyzed using elastic backscattering (EBS) before and after exposure. All samples showed noticeable erosion. The results were compared to the data for Be and W erosion rates for the first 2011–2012 JET ITER-like wall (ILW-1) campaign, and to the data for C erosion during the 2005–2009 campaign when JET was operated with a carbon wall. The mean W erosion rates and the toroidal and poloidal distributions of the W erosion were nearly the same for the ILW-1 and ILW-2 campaigns. The mean erosion rate of Be during the ILW-2 campaign was smaller by a factor of about two compared to the ILW-1 campaign.</abstract><pub>Elsevier Ltd</pub><doi>10.1016/j.nme.2017.02.026</doi><tpages>5</tpages><oa>free_for_read</oa></addata></record>
fulltext fulltext
identifier ISSN: 2352-1791
ispartof Nuclear materials and energy, 2017-05, Vol.11 (C), p.20-24
issn 2352-1791
2352-1791
language eng
recordid cdi_doaj_primary_oai_doaj_org_article_665d14dd3ef0469ba5720074f52c5d97
source ScienceDirect Journals
title Erosion at the inner wall of JET during the discharge campaign 2013–2014
url http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-04T17%3A50%3A45IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-elsevier_doaj_&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Erosion%20at%20the%20inner%20wall%20of%20JET%20during%20the%20discharge%20campaign%202013%E2%80%932014&rft.jtitle=Nuclear%20materials%20and%20energy&rft.au=Krat,%20S.&rft.aucorp=JET%20contributors&rft.date=2017-05-01&rft.volume=11&rft.issue=C&rft.spage=20&rft.epage=24&rft.pages=20-24&rft.issn=2352-1791&rft.eissn=2352-1791&rft_id=info:doi/10.1016/j.nme.2017.02.026&rft_dat=%3Celsevier_doaj_%3ES2352179116303003%3C/elsevier_doaj_%3E%3Cgrp_id%3Ecdi_FETCH-LOGICAL-c481t-390306dacc4ca262f7c364d30e52ce1aebd78bd3f24ea6ff5e0962161339ebf33%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_id=info:pmid/&rfr_iscdi=true