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Effects of flow on uranium speciation in soils impacted by acidic waste fluids

机译:流动对受酸性废液影响的土壤中铀形态的影响

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摘要

Radioactive acidic liquid waste is a common byproduct of uranium (U) and plutonium (Pu) enrichment and recycling processes whose accidental and planned release has led to a significant input of U into soils and sediments across the world, including at the U.S. DOE's Hanford site (WA, USA). Because of the particularly hazardous nature of U, it is important to predict its speciation when introduced into soils and sediments by acidic waste fluids. Of fundamental importance are the coupled effects of acid-driven mineral transformation and reactive transport on U speciation. To evaluate the effect of waste-fluid residence time and co-associated dis-solved phosphate concentrations on U speciation in impacted soils and sediments, uncontaminated surface materials (from the Hanford Site) were reacted with U-containing synthetic acidic waste fluids (pH 2) amended with dissolved phosphate concentrations in both batch (no flow) and flow-through column systems for 7-365 days. By comparing dissolved U behavior and solid phase speciation as a function of flow regimen, we found that the availability of proton-promoted dissolution products (such as Si) to sequester U into uranyl silicates was dependent on waste fluid-sediment contact time as uranyl silicates were not detected in short contact time flow -through systems but were detected in no-flow, long contact time, reactors. Moreover, the dominance of uranyl phosphate as neoprecipitate U scavenger (principally in the form of meta-ankoleite) in phosphate amended systems confirmed the importance of phosphate amendments for an efficient sequestration of U in the soils and sediments. Overall, our experiments suggest that the formation of uranyl silicates in soils impacted by acidic waste fluids is likely to be limited unless reaction products are allowed to accumulate in soil pores, highlighting the importance of investigating soil U speciation in flow-through, transport-driven systems as opposed to no -flow, batch systems. This study provides insights into uranium speciation and its potential changes under acidic conditions for better prediction of risks and subsequent development of efficient remediation strategies.
机译:放射性酸性液体废物是铀(U)和钚(Pu)浓缩和回收过程的常见副产品,其意外和计划的释放导致铀大量输入到世界各地的土壤和沉积物中,包括美国能源部的汉福德基地(美国华盛顿州)。由于铀的特殊危险性,当被酸性废液引入土壤和沉积物时,预测其形态非常重要。至关重要的是酸驱动的矿物转化和反应性转运对 U 形态形成的耦合效应。为了评估废液停留时间和共伴溶解磷酸盐浓度对受影响土壤和沉积物中U形态的影响,将未受污染的表面材料(来自汉福德场地)与含U的合成酸性废液(pH值2)反应,在分批(无流动)和流通柱系统中用溶解的磷酸盐浓度修正7-365天。通过比较溶解的 U 行为和固相形态作为流动方案的函数,我们发现质子促进的溶解产物(如 Si)将 U 螯合到铀酰硅酸盐中的可用性取决于废液-沉积物接触时间,因为硅酸铀酰在短接触时间流通系统中未检测到,但在无流动中被检测到, 接触时间长,反应器。此外,磷酸铀酰作为新沉淀物铀清除剂(主要以间位铀石的形式)在磷酸盐改良体系中占主导地位,证实了磷酸盐改良剂对于有效封存土壤和沉积物中铀的重要性。总体而言,我们的实验表明,除非允许反应产物在土壤孔隙中积聚,否则在受酸性废液影响的土壤中硅酸铀酰的形成可能会受到限制,这突出了在流通、运输驱动的系统中研究土壤 U 形态的重要性,而不是无流动、间歇系统。本研究提供了对铀形态及其在酸性条件下的潜在变化的见解,以便更好地预测风险并随后制定有效的补救策略。

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