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预测铀和锝在受污染酸性地下水滴定过程中的吸附。

Prediction of uranium and technetium sorption during titration of contaminated acidic groundwater.

机构信息

Institute of Tibetan Plateau Research, Chinese Academy of Sciences, 18 Shuangqing Road, P.O. Box 2871, Beijing 100085, China.

出版信息

J Hazard Mater. 2010 Jun 15;178(1-3):42-8. doi: 10.1016/j.jhazmat.2010.01.040. Epub 2010 Jan 15.

Abstract

This study investigates uranium and technetium sorption onto aluminum and iron hydroxides during titration of acidic groundwater. The contaminated groundwater exhibits oxic conditions with high concentrations of NO(3)(-), SO(4)(2-), U, Tc, and various metal cations. More than 90% of U and Tc was removed from the aqueous phase as Al and Fe precipitated above pH 5.5, but was partially resolublized at higher pH values. An equilibrium hydrolysis and precipitation reaction model adequately described variations in aqueous concentrations of metal cations. An anion exchange reaction model was incorporated to simulate sulfate, U and Tc sorption onto variably charged (pH-dependent) Al and Fe hydroxides. Modeling results indicate that competitive sorption/desorption on mixed mineral phases needs to be considered to adequately predict U and Tc mobility. The model could be useful for future studies of the speciation of U, Tc and co-existing ions during pre- and post-groundwater treatment practices.

摘要

本研究调查了酸性地下水滴定过程中铀和锝在铝和铁氢氧化物上的吸附。受污染的地下水呈氧化状态,含有高浓度的硝酸盐、硫酸盐、U、Tc 和各种金属阳离子。在 pH 值高于 5.5 时,Al 和 Fe 沉淀,超过 90%的 U 和 Tc 从水相中去除,但在较高 pH 值下部分重新溶解。平衡水解和沉淀反应模型充分描述了金属阳离子在水溶液中的浓度变化。阴离子交换反应模型被纳入以模拟可变电荷(pH 依赖性)的 Al 和 Fe 氢氧化物上的硫酸盐、U 和 Tc 吸附。模型结果表明,需要考虑混合矿物相上的竞争吸附/解吸,以充分预测 U 和 Tc 的迁移性。该模型可用于未来研究地下水预处理和后处理过程中 U、Tc 和共存离子的形态。

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