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表土中砷的迁移性与稳定性

Arsenic mobility and stabilization in topsoils.

作者信息

Tyrovola Konstantina, Nikolaidis Nikolaos P

机构信息

Department of Environmental Engineering, Technical University of Crete, University Campus, 73100 Chania, Crete, Greece.

出版信息

Water Res. 2009 Apr;43(6):1589-96. doi: 10.1016/j.watres.2009.01.001. Epub 2009 Jan 18.

Abstract

Agricultural topsoil can be polluted with arsenic due to irrigation with contaminated water from geothermal sources. This work evaluates the mobility of arsenic in topsoils and stabilization of arsenic with zero valent iron (ZVI), in short term experiments. The objective of this study was the development of a simplified empirical model that can predict the concentration of iron released from ZVI and the concentration of arsenic remaining in the solution during short term stabilization experiments. The empirical model correlates the release of arsenic from soil with dissolved iron concentration during stabilization experiments, in different pH and ZVI/solution ratios. Reaction time and the ratio of ZVI/soil affect the efficiency of arsenic stabilization in topsoils with ZVI. In addition, the release/desorption experiments and adsorption experiments, under different conditions, showed that the concentration of arsenate desorbed from soil depends on the temperature. Higher concentrations of arsenate were reported, as the temperature increased.

摘要

由于使用来自地热源的受污染水进行灌溉,农业表层土壤可能会被砷污染。这项工作在短期实验中评估了砷在表层土壤中的迁移性以及零价铁(ZVI)对砷的固定作用。本研究的目的是开发一个简化的经验模型,该模型可以预测短期稳定实验期间从ZVI释放的铁的浓度以及溶液中残留的砷的浓度。该经验模型将稳定实验期间土壤中砷的释放与不同pH值和ZVI/溶液比例下溶解铁的浓度相关联。反应时间和ZVI/土壤比例会影响ZVI对表层土壤中砷的固定效率。此外,在不同条件下进行的释放/解吸实验和吸附实验表明,从土壤中解吸的砷酸盐浓度取决于温度。随着温度升高,报告的砷酸盐浓度更高。

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