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Impact of river overflowing on trace element contamination of volcanic soils in south Italy: Part Ⅰ. Trace element speciation in relation to soil properties

机译:河流溢流对意大利南部火山土壤微量元素污染的影响:第一部分。微量元素形态与土壤特性的关系

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Volcanic soils affected by different numbers of polluted river flooding events were investigated. Chromium and Cu were the major soil contaminants. Nickel, Fe, Zn and Mn total content never exceeded the Italian mandatory limits. The distribution of Cr and Cu total contents among studied soils indicated that only Cr contamination was related to overflowing events. In polluted soils, sequential chemical extractions revealed a preferential association of Cr and Cu with organic forms. A progressive Cr insolubilization with ageing was observed. Significant amounts of Cr and Cu were extracted by NH_4-oxalate, suggesting metals association with short-range-prder aluminosilicates and organo-mineral complexes. Possible methodological drawbacks in the use of the EU-BCR chemical speciation protocol on volcanic soils are discussed. Micromorphology and SEM/WDS analyses revealed Cr and Cu enriched silt and clay coatings in surface and subsurface soil horizons, suggesting a transfer of metal-rich sediments along the soil pore network with water movement.
机译:研究了受不同数量的河水污染事件影响的火山土壤。铬和铜是主要的土壤污染物。镍,铁,锌和锰的总含量从未超过意大利的强制性限值。 Cr和Cu总含量在研究土壤中的分布表明只有Cr污染与溢出事件有关。在受污染的土壤中,连续化学萃取显示出Cr和Cu与有机形式的优先结合。观察到随着时间的流逝,铬逐渐溶解。 NH_4-草酸酯可萃取出大量的Cr和Cu,表明金属与短距离投递的铝硅酸盐和有机-矿物配合物缔合。讨论了在火山土壤上使用EU-BCR化学物种形成规程可能存在的方法学缺陷。微观形貌和SEM / WDS分析表明,表层和地下土壤层中富含Cr和Cu的淤泥和粘土覆盖层,表明随着水的移动,富含金属的沉积物沿土壤孔隙网络转移。

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