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污染源活动停止20年后多元素污染土壤中金属和类金属的迁移性

Mobility of metals and metalloids in a multi-element contaminated soil 20 years after cessation of the pollution source activity.

作者信息

Clemente Rafael, Dickinson Nicholas M, Lepp Nicholas W

机构信息

School of Biological and Earth Sciences, Liverpool John Moores University, Byrom Street, Liverpool L3 3AF, UK.

出版信息

Environ Pollut. 2008 Sep;155(2):254-61. doi: 10.1016/j.envpol.2007.11.024. Epub 2008 Jan 14.

Abstract

Knowledge of trace element concentrations and mobility is important in the ecotoxicological assessment of contaminated soils. We analysed soil pore water under field conditions to provide new insights into the mobility of residual contaminants in the surface 50 cm of a highly contaminated woodland soil. Cadmium and Zn were highly mobile in the acidic soil, concentrations increasing with depth in soil pore water, showing considerable downward mobility. High levels of surface organic matter restricted the solubility of Cu, Pb and Sb, with highest concentrations being found close to the surface. Dissolved organic carbon in pore water had a strong influence on mobility of Cu, Zn, Pb and Sb. Elevated As had moved from the organic surface horizons but was largely immobilised in deeper layers and associated with Fe and Al oxides. The measured differential mobility of pollutants in the present study is highly relevant to protection of groundwater and other receptors.

摘要

了解微量元素浓度和迁移性对于受污染土壤的生态毒理学评估至关重要。我们在田间条件下分析了土壤孔隙水,以便对高度污染的林地土壤表层50厘米内残留污染物的迁移性提供新的见解。镉和锌在酸性土壤中具有高度迁移性,其在土壤孔隙水中的浓度随深度增加,显示出相当大的向下迁移性。高水平的表层有机物限制了铜、铅和锑的溶解度,最高浓度出现在靠近地表处。孔隙水中的溶解有机碳对铜、锌、铅和锑的迁移性有强烈影响。砷含量升高已从有机表层迁移,但在较深层基本固定,并与铁和铝的氧化物相关。本研究中测得的污染物迁移差异对保护地下水和其他受体高度相关。

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