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Solid-Phase Distribution and Leaching Behaviour of Nickel and Uranium in a Uranium Waste-Rock Piles

机译:铀废岩桩中镍和铀的固相分布和浸出行为

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摘要

The potential risk of surface and groundwater contamination by the heavy metals and radionuclides leached from uranium waste-rock piles (UWRP) is a major environmental concern in the uranium-mining district of Northern Saskatchewan, Canada. The main objective of this study was to evaluate the nickel and uranium leaching behaviour in the UWRP lithological materials. In addition to the chemical characterization, these selected UWRP geomedia samples were also subjected to the sequential extraction procedure, availability test to quantify leaching potential and cumulative leaching test (CLT). Sequential extractions results demonstrated substantial observed differences in the Ni and U distribution patterns among various operationally defined geochemical fractions. A large fraction of total Ni concentration was associated with non-labile residual fraction while U was mainly present in the labile fractions. The observed labile Ni and U concentrations also remained relatively high in the gneissic basement materials and underlying organic-rich lake sediment. In case of basement materials, both Ni and U concentrations in solution with the first CLT fraction exceeds their maximum permissible levels in both surface and groundwater. Leaching test results confirmed that Ni and U teachability depends on their total content distribution in various solid phase fractions, and several geochemical processes are controlling the solubility of Ni and U geochemical phases in the UWRP. Our experimental data suggest the potential for a long-term risk to surface and groundwater contamination from these UWRP.
机译:在加拿大北部萨斯喀彻温省的铀矿开采区,铀废石堆(UWRP)浸出的重金属和放射性核素对地表和地下水的潜在污染风险是一个主要的环境问题。这项研究的主要目的是评估UWRP岩性材料中镍和铀的浸出行为。除化学表征外,还对这些选定的UWRP土工样品进行了顺序提取程序,可用性测试以量化浸出潜力和累积浸出测试(CLT)。连续提取结果表明,在各种可操作定义的地球化学馏分之间,Ni和U分布模式存在明显的差异。总镍浓度的很大一部分与不稳定的残留分数有关,而铀主要存在于不稳定的分数中。在片麻岩基底材料和下面富含有机物的湖泊沉积物中,观察到的不稳定的镍和铀浓度也仍然相对较高。对于基底材料,溶液中具有第一CLT分数的Ni和U浓度均超过其在地表水和地下水中的最大允许含量。浸出测试结果证实,镍和铀的可教性取决于它们在各种固相部分中的总含量分布,并且几种地球化学过程正在控制镍和铀地球化学相在UWRP中的溶解度。我们的实验数据表明,这些UWRP可能长期污染地表和地下水。

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