含铁土壤矿物表面对铀的吸附/解吸

S. Ha, D. Kyung, Woojin Lee
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引用次数: 5

摘要

采用连续塔式反应器对纯土壤环境中铀(U)的吸附/解吸进行了研究。此外,我们还利用量子计算在分子尺度上研究了铀在活石表面的吸附/解吸机理。我们观察到,注射U (1 μM) 20 d后,可检测到0.1 μM以下的U。然而,通过注射CARB溶液(1.44 × 10 M NaHCO3和2.8 × 10 M Na2CO3),吸收的U在24 h内全部从活石表面分离。通过交换能计算,我们发现UO2 (CO3)2和UO2 (CO3)3具有比UO2 (OH)2更高的排斥能。本研究结果可用于预测铀在污染场地和修复场地中的行为。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Adsorption/desorption of uranium on iron-bearing soil mineral surface
In this study, we evaluated the adsorption/desorption of uranium (U) in pure soil environment using continuous column reactor. We additionally investigated the adsorption/desorption mechanism of U on vivianite surface in molecular scale using quantum calculation. We observed that below 0.1 μM of U was detected after 20 d from U injection (1 μM) in adsorption test. However, all of absorbed U was detached from vivianite surface in 24 h by injection of CARB solution (1.44 × 10 M NaHCO3 and 2.8 × 10 M Na2CO3). Based on exchange energy calculation, we found that UO2 (CO3)2 and UO2 (CO3)3 species have higher repulsive energy than UO2 (OH)2 species. The results obtained from this study could be applied to predict the behavior of uranium in contaminated and remediation sites.
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