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Operationally defined associations of arsenic and copper from soil and mine waste in south-west England

机译:英格兰西南部土壤和矿山废料中砷和铜的操作性定义关联

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摘要

Arsenic and copper fractionation was studied in contaminated soil and mine waste materials from a mining site in Devon, UK. Ten soil samples with Cu concentrations ranging from 300-6144 mg/kg and As concentrations ranging from 5512-39715 mg/kg were sequentially extracted using the modified method of Tessier et al. (1979) and Wenzel et al. (2001). The Classical Tessier et al. (1979) scheme was shown to be inadequate for studying either Cu or As fractionation as it severely underestimated the Fe-oxide associated fraction. The Modified Tessier et al. (1979) scheme, including the two additional steps specifically targeting Fe-oxides, was shown adequate for both Cu and As fractionation; however the Wenzel et al. (2001) protocol allows the prediction of changes in lability of As in various solid phases as a result of soil remediation or alteration in environmental factors. In agreement with other studies, arsenic was found to be held predominantly in the amorphous Fe-oxide fraction (55%-94%), which can be potentially mobilised with a change in redox conditions. A significant proportion of As can also be remobilised from the soils through the process of anion exchange. Copper presented a different fractionation pattern as it was distributed mainly between the organic/sulfide and the Fe-Mn oxide fractions. Although the total concentrations of Cu in the soils are much lower than As, Cu appears to be solubilised to a much greater extent as indicated by the higher percentage contribution of Cu in the easily mobilisable fractions.
机译:对英国德文郡一个采矿场的受污染的土壤和矿山废料中的砷和铜进行了分级分离。使用Tessier等人的改进方法,依次提取了十个土壤样品,其中Cu的浓度范围为300-6144 mg / kg,As的浓度范围为5512-39715 mg / kg。 (1979)和Wenzel等。 (2001)。古典Tessier等。 (1979)的方案被证明不足以研究Cu或As的分馏,因为它严重低估了Fe-氧化物相关的馏分。修改后的Tessier等。 (1979)的方案,包括另外两个针对铁氧化物的步骤,被证明足以分离铜和砷。然而,温泽尔等。 (2001年)协议允许预测由于土壤修复或环境因素改变而导致的各种固相中砷的不稳定性变化。与其他研究一致,发现砷主要存在于无定形的Fe-氧化物级分(55%-94%)中,随着氧化还原条件的改变,砷可能被转移。还可以通过阴离子交换过程从土壤中去除大量的砷。铜表现出不同的分馏模式,因为它主要分布在有机/硫化物和Fe-Mn氧化物之间。尽管土壤中铜的总浓度远低于砷,但铜的溶解度似乎要高得多,这表明易迁移部分中铜的贡献率较高。

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