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Chemical Speciation and Potential Mobility of Heavy Metals in the Soil of Former Tin Mining Catchment

机译:旧锡矿集水区土壤中重金属的化学形态和势能迁移

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摘要

This study describes the chemical speciation of Pb, Zn, Cu, Cr, As, and Sn in soil of former tin mining catchment. Total five sites were selected for sampling and subsequent subsamples were collected from each site in order to create a composite sample for analysis. Samples were analysed by the sequential extraction procedure using optical emission spectrometry (ICP OES). Small amounts of Cu, Cr, and As retrieved from the exchangeable phase, the ready available for biogeochemical cycles in the ecosystem. Low quantities of Cu and As could be taken up by plants in these kind of acidic soils. Zn not detected in the bioavailable forms while Pb is only present in negligible amounts in very few samples. The absence of mobile forms of Pb eliminates the toxic risk both in the trophic chain and its migration downwards the soil profile. The results also indicate that most of the metals have high abundance in residual fraction indicating lithogenic origin and low bioavailability of the metals in the studied soil. The average potential mobility for the metals giving the following order: Sn > Cu > Zn > Pb > Cr > As.
机译:这项研究描述了前锡矿流域土壤中铅,锌,铜,铬,砷和锡的化学形态。共选择五个地点进行采样,并从每个地点收集后续子样本,以创建用于分析的复合样本。使用光发射光谱法(ICP OES)通过顺序提取程序分析样品。从可交换相中回收少量的Cu,Cr和As,可用于生态系统中的生物地球化学循环。在这类酸性土壤中,植物可能吸收少量的铜和砷。在生物样品中未检测到锌,而铅在极少数样品中的含量可忽略不计。缺乏可移动形式的Pb消除了营养链及其向下迁移至土壤剖面的毒性风险。结果还表明,大多数金属的残留分数很高,表明成岩起源和金属在土壤中的生物利用度低。金属的平均电势迁移率具有以下顺序:Sn> Cu> Zn> Pb> Cr> As。

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