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Relative Reactivity of Biogenic and Chemogenic Uraninite and Biogenic Non Crystalline U(IV)

机译:生物和化学成铀质岩和生物非结晶铀(IV)的相对反应性

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摘要

Aqueous chemical extractions and X-ray absorption spectroscopy (XAS) analyses were conducted to investigate the reactivity of chemogenic uraninite, nanoparticulate biogenic uraninite, and biogenic monomeric U(IV) species. The analyses were conducted in systems containing a total U concentration that ranged from 1.48 to 2.10 mM. Less than 0.02% of the total U was released to solution in extractions that targeted water soluble and ion exchangeable fractions. Less than 5% of the total U was solubilized via complexation with a 0.1 M solution of NaF. Greater than 90% of the total U was extracted from biogenic uraninite and monomeric U(IV) after 6 hours of reaction in an oxidizing solution of 50 mM K2S2O8. Additional oxidation experiments with lower concentrations (2 mM and 10 mM) of K2S2O8 and 8.2 mg L−1 dissolved oxygen suggested that monomeric U(IV) species are more labile than biogenic uraninite; chemogenic uraninite was much less susceptible to oxidation than either form of biogenic U(IV). These results suggest that non-crystalline forms of U(IV) may be more labile than uraninite in subsurface environments. This work helps fill critical gaps in our understanding of the behavior of solid-associated U(IV) species in bioremediated sites and natural uranium ore deposits.
机译:进行了水性化学提取和X射线吸收光谱(XAS)分析,以研究化学生成的尿素矿,纳米颗粒生物生成的尿素矿和生物生成的单体U(IV)物种的反应性。该分析是在总U浓度为1.48至2.10 mM的系统中进行的。在以水溶性和离子交换级分为目标的萃取中,只有不到0.02%的U释放到溶液中。通过与0.1 M NaF溶液络合可溶解少于5%的总U。在50 mM K2S2O8的氧化溶液中反应6小时后,从生物尿素和单体U(IV)中提取了总U的90%以上。在较低浓度(2 mM和10 mM)的K2S2O8和8.2 mg L -1 溶解氧的条件下进行的其他氧化实验表明,单体U(IV)物种比生物成矿的尿素更不稳定。与任何一种生物成因的U(IV)相比,化学成因的尿素矿对氧化的敏感性要低得多。这些结果表明,在地下环境中,非晶体形式的U(IV)可能比铀矿更不稳定。这项工作有助于填补我们对生物修复位点和天然铀矿床中与固体相关的U(IV)物种行为的理解的重大空白。

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