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Distribution of naturally occurring radionuclides (U, Th) in Timahdit black shale (Morocco)

机译:提马迪特黑页岩(摩洛哥)中天然存在的放射性核素(U,Th)的分布

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Attention has been focused recently on the use of Moroccan black oil shale as the raw material for production of a new type of adsorbent and its application to U and Th removal from contaminated wastewaters. The purpose of the present work is to provide a better understanding of the composition and structure of this shale and to determine its natural content in uranium and thorium. A black shale collected from Timahdit (Morocco) was analyzed by powder X-ray diffraction and SEM techniques. It was found that calcite, dolomite, quartz and clays constitute the main composition of the inorganic matrix. Pyrite crystals are also present. A selective leaching procedure, followed by radiochemical purification and α-counting, was performed to assess the distribution of naturally occurring radionuclides. Leaching results indicate that ~(238)U, ~(235)U, ~(234)U, ~(232)Th, ~(230)Th and ~(228)Th have multiple modes of occurrence in the shale. U is interpreted to have been concentrated under anaerobic conditions. An integrated isotopic approach showed the preferential mobilization of uranium carried by humic acids to carbonate and apatite phases. Th is partitioned between silicate minerals and pyrite.
机译:最近,注意力集中在使用摩洛哥黑油页岩作为生产新型吸附剂的原料及其在从污染废水中去除U和Th的应用中。本工作的目的是更好地了解该页岩的组成和结构,并确定其在铀和th中的天然含量。通过粉末X射线衍射和SEM技术分析了从提马哈迪特(摩洛哥)收集的黑色页岩。发现方解石,白云石,石英和粘土是无机基质的主要成分。硫铁矿晶体也存在。进行了选择性浸出程序,然后进行放射化学纯化和α计数,以评估天然存在的放射性核素的分布。浸出结果表明,〜(238)U,〜(235)U,〜(234)U,〜(232)Th,〜(230)Th和〜(228)Th在页岩中有多种发生方式。 U被解释为在厌氧条件下浓缩。一种综合的同位素方法表明,腐殖酸携带的铀优先迁移到碳酸盐和磷灰石相。 Th在硅酸盐矿物和黄铁矿之间分配。

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