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首页> 外文期刊>Journal of Radiation Research and Applied Sciences >Characterization of uranium in soil samples from a prospective uranium mining in Serule, Botswana for nuclear forensic application
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Characterization of uranium in soil samples from a prospective uranium mining in Serule, Botswana for nuclear forensic application

机译:Serule植物核矿区铀矿区土壤样品中铀的表征核法医应用

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摘要

This study attempts a nuclear forensic characterization of uranium in soil samples from a prospective Serule mine in Botswana. The analysis involves the determination of forensic signatures found in uranium-bearing materials from the mine. These signatures include 232Th activity concentration, isotopic and activity ratios of 232Th/238U and 235U/238U, impurity concentration, rare earth elements (REE), as well as the mineralogy of the area, all of which were determined using both Inductively Coupled Plasma Mass Spectroscopy (ICP-MS) and X-ray Florescence (XRF) analytical techniques. Isotopic ratios determined reveal that there is a significant difference in the isotopic concentration, activity concentration of 232Th, 238U, and 235U, as well as the 232Th/238U isotope ratio between the uranium ores from each mine. The REE/chondrite analysis indicates clear patterns, suggesting that it is possible to use this feature as a unique identifier for Serule uranium ore source.
机译:本研究企图从博茨瓦纳一名前瞻性精灵矿区核法医表征土壤样本中的土壤样本。该分析涉及从矿井中含有铀材料中发现的法医签名。这些签名包括 232 th活性浓度,同位素和活性比 232 th / 238 U和 235 U / 238 U,杂质浓度,稀土元素(Ree)以及所述面积的矿物,所有这些都使用电感耦合等离子体质谱(ICP-MS)和X射线测定Flore(XRF)分析技术。同位素比例揭示了同位素浓度的显着差异, 232℃的活性浓度, 238 U和 235 U,如以及来自每个矿井的铀矿石之间的 232 th / 238 U同位素比。 REE / Chondrite分析表明明确的模式,表明可以将此功能用作SERUER铀矿源的唯一标识符。

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