European Commission, Joint Research Centre, Institute for Transuranium Elements, P.O. Box 2340, 76125 Karlsruhe, Germany.
Anal Chem. 2009 Oct 15;81(20):8327-34. doi: 10.1021/ac901100e.
Lead and strontium isotope ratios were used for the origin assessment of uranium ore concentrates (yellow cakes) for nuclear forensic purposes. A simple and low-background sample preparation method was developed for the simultaneous separation of the analytes followed by the measurement of the isotope ratios by multicollector inductively coupled plasma mass spectrometry (MC-ICPMS). The lead isotopic composition of the ore concentrates suggests applicability for the verification of the source of the nuclear material and by the use of the radiogenic (207)Pb/(206)Pb ratio the age of the raw ore material can be calculated. However, during data interpretation, the relatively high variation of the lead isotopic composition within the mine site and the generally high contribution of natural lead as technological contamination have to be carefully taken into account. The (87)Sr/(86)Sr isotope ratio is less prone to the variation within one mine site and less affected by the production process, thus it was found to be a more purposeful indicator for the origin assessment and source verification than the lead. The lead and strontium isotope ratios measured and the methodology developed provide information on the initial raw uranium ore used, and thus they can be used for source attribution of the uranium ore concentrates.
采用铅和锶同位素比值来评估铀矿石浓缩物(黄饼)的来源,以进行核取证。针对分析物的同时分离,开发了一种简单且背景低的样品制备方法,然后采用多接收电感耦合等离子体质谱法(MC-ICPMS)测量同位素比值。矿石浓缩物的铅同位素组成可用于验证核材料的来源,并且通过放射性(207)Pb/(206)Pb 比值,可以计算出原始矿石材料的年龄。然而,在数据解释过程中,必须仔细考虑矿山内部铅同位素组成的相对较高变化以及天然铅作为技术污染的普遍高贡献。(87)Sr/(86)Sr 同位素比值在一个矿山内部的变化较小,受生产过程的影响也较小,因此与铅相比,它被认为是评估来源和验证来源的更有意义的指标。测量得到的铅和锶同位素比值以及所开发的方法提供了有关初始原始铀矿石的信息,因此可用于铀矿石浓缩物的来源归属。