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dc.contributor.authorKRAJKO JUDITen_GB
dc.contributor.authorVARGA ZSOLTen_GB
dc.contributor.authorWALLENIUS Mariaen_GB
dc.contributor.authorMAYER Klausen_GB
dc.contributor.authorKONINGS Rudyen_GB
dc.date.accessioned2017-04-15T00:34:43Z-
dc.date.available2016-08-09en_GB
dc.date.available2017-04-15T00:34:43Z-
dc.date.created2016-08-04en_GB
dc.date.issued2016en_GB
dc.date.submitted2015-10-13en_GB
dc.identifier.citationJOURNAL OF RADIOANALYTICAL AND NUCLEAR CHEMISTRY vol. 309 no. 3 p. 1113-1121en_GB
dc.identifier.issn0236-5731en_GB
dc.identifier.urihttp://link.springer.com/article/10.1007%2Fs10967-016-4733-5en_GB
dc.identifier.urihttp://publications.jrc.ec.europa.eu/repository/handle/JRC97914-
dc.description.abstractThe applicability and limitations of sulphur isotope ratio as a nuclear forensic signature have been studied. The typically applied leaching methods in uranium mining processes were simulated for five uranium ore samples and the n(34S)/n(32S) ratios were measured. The sulphur isotope ratio variation during uranium ore concentrate (UOC) production was also followed using two real-life sample sets obtained from industrial UOC production facilities. Once the major source of sulphur is revealed, its appropriate application for origin assessment can be established. Our results confirm the previous assumption that process reagents have a significant effect on the n(34S)/n(32S) ratio, thus the sulphur isotope ratio is in most cases a process-related signature.en_GB
dc.description.sponsorshipJRC.G.II.6-Nuclear Safeguards and Forensicsen_GB
dc.format.mediumOnlineen_GB
dc.languageENGen_GB
dc.publisherSPRINGERen_GB
dc.relation.ispartofseriesJRC97914en_GB
dc.titleInvestigation of sulphur isotope variation due to different processes applied during uranium ore concentrate productionen_GB
dc.typeArticles in periodicals and booksen_GB
dc.identifier.doi10.1007/s10967-016-4733-5en_GB
JRC Directorate:Nuclear Safety and Security

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