首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >Trace element and U isotope analysis of uraninite and ore concentrate: Applications for nuclear forensic investigations
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Trace element and U isotope analysis of uraninite and ore concentrate: Applications for nuclear forensic investigations

机译:铀酸盐和矿石浓缩物的痕量元素与U同位素分析:核法医调查的应用

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Abstract Uranium ore concentrate (UOC), is an important intermediate material in the nuclear fuel cycle. Trace element distributions in UOCs can be related to the geologic conditions in which the source uranium ore formed, and hence are characteristic for each deposit type. These chemical signatures can then potentially be used as an essential tool for nuclear forensic analysis of derivative radioactive materials. In this study, several samples of UOC and uraninite extracted from sandstone-hosted roll front deposits in the Powder River basin U province in Wyoming (USA) have been analyzed for their trace element abundances and U isotopic compositions. UOCs were analyzed both in solution mode-inductively coupled plasma mass spectrometry (SM-ICP-MS) subsequent bulk sample digestion, and at high-spatial resolution (10s of micron scale) using a laser ablation (LA)-ICP-MS technique. Comparison of trace elemental abundances obtained by SM- and LA-ICP-MS indicates corroborating results, with comparable chondrite-normalized rare earth element (REE) patterns; those obtained by LA-ICP-MS show a slightly larger variation in absolute elemental abundances compared with corresponding bulk sample digestions. U isotopic measurements for UOCs and uraninite were conducted by solution mode multi-collector (MC)-ICP-MS. 238U/235U, 235U/234U and 238U/234U ratios for uraninite and UOC overlap and confirm a lack of significant isotopic fractionation during the fabrication process. The results reported here assert the validity of analyzing UOC for source attribution purposes and simultaneously demonstrate that corroborating trace element signatures can be obtained with both LA and SM-ICP-MS analytical techniques for U-rich materials relevant to the nuclear fuel cycle. REE abundances and U isotopes did not fractionate during early ore processing of materials investigated in this study. Highlights ? Corroborating trace element analyses are obtained regardless of sampling technique. ? No differentiation of trace element signatures occurs during U ore processing. ? U isotope ratios are established for corresponding U ore and ore concentrate. ? The origin of uranium ore concentrate is determined using forensic indicators. ]]>
机译:<![CDATA [ 抽象 铀矿石浓缩物(UOC),是核燃料循环中的重要中间材料。 uocs中的痕量元素分布可以与形成的源铀矿石的地质条件有关,并且因此是每个沉积物的特征。然后可以将这些化学特性可能被用作衍生放射性物质的核法医分析的基本工具。在这项研究中,已经分析了在怀俄明州(美国)中粉河流域U省的砂岩宿主卷前沉积物中提取的几种uoc和铀矿样品已经分析了它们的微量元素丰度和U同位素组合物。在溶液电感耦合等离子体质谱(SM-ICP-MS)随后的体积消化中分析UOC,以及使用激光烧蚀(LA)-ICP-MS技术的高空间分辨率(10S微米级)。 SM-and La-ICP-MS获得的痕量元素丰度的比较表明了腐蚀的结果,具有可比的软骨态标准化稀土元素(REE)图案;通过La-ICP-MS获得的那些与相应的散装样品消化相比显示出绝对元素丰度的稍大变化。通过溶液模式多收集器(MC)-ICP-MS进行UOC和铀岩的Uocs和铀岩的同位素测量。 238> 238 u / 235 u, 235 < / ce:sup> u / 234 u和 238 u / 234 UANINITE和UOC的比率重叠并确认在制造过程中缺乏显着的同位素分级。结果报告的结果断言了对源归属目的分析UOC的有效性,并同时证明可以使用与核燃料循环相关的U-Rich材料的LA和SM-ICP-MS分析技术获得相关的痕量元素签名。 REE丰富和U同位素在本研究中调查的材料的早期矿石加工过程中没有分馏。 突出显示 < CE:PARA ID =“P0010”View =“全部”>无论采样技术如何获得相关的跟踪元素分析。 在U ORE处理期间没有发生跟踪元素签名的差异。 U同位素比率是est用于相应的U矿石和矿石浓缩物。 使用法医指标确定铀矿石浓缩物的来源。 ]]>

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