首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >Trace metal and As solid-phase speciation in sulphide mine tailings - Indicators of spatial distribution of sulphide oxidation in active tailings impoundments
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Trace metal and As solid-phase speciation in sulphide mine tailings - Indicators of spatial distribution of sulphide oxidation in active tailings impoundments

机译:硫化矿尾矿中的痕量金属和As固相形态-活性尾矿库中硫化物氧化空间分布的指标

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Redistribution of potentially harmful metals and As was studied based on selective extractions in two active sulphide mine tailings impoundments in Finland. The Hitura tailings area contains residue from Ni ore processing, while the Luikonlahti site includes tailings from the processing of Cu-Co-Zn-Ni and talc ores. To characterize the element solid-phase speciation with respect to sulphide oxidation intensity and the water saturation level of the tailings, drill cores were collected from border zones and mid-impoundment locations. The mobility and solid-phase fractionation of Ni, Cu, Co, Zn, Cr, Fe, Ca, Al, As, and S were analysed using a 5-step non-sequential (parallel) selective extraction procedure. The results indicated that metal redistribution and sulphide oxidation intensity were largely controlled by the disposal history and strategy of the tailings (sorting, exposure of sulphides due to delayed burial), impoundment structure and water table, and reactivity of the tailings. Metal redistribution suggested sulphide weathering in the tailings surface, but also in unsaturated proximal areas beside the earthen dams, and in water-saturated bottom layers, where O-2-rich infiltration is possible. Sulphide oxidation released trace metals from sulphide minerals at both locations. In the Hitura tailings, with sufficient buffering capacity, pH remained neutral and the mobilized metals were retained by secondary Fe precipitates deeper in the oxidized zone. In contrast, sulphide oxidation-induced acidity and rise in the water table after oxidation apparently remobilized the previously retained metals in Luikonlahti. In general, continuous disposal of tailings decreased the sulphide oxidation intensity in active tailings, unless there was a delay in burial and the reactive tailings were unsaturated after deposition.
机译:在芬兰的两个活性硫化物矿尾矿库中,基于选择性萃取对潜在有害金属和砷的重新分布进行了研究。 Hitura尾矿区包含来自镍矿石加工的残渣,而Luikonlahti地点包括来自Cu-Co-Zn-Ni和滑石矿石加工的残渣。为了表征元素固相形态相对于硫化物的氧化强度和尾矿的水饱和度水平,从边界区域和中蓄水位置收集了钻芯。使用5步非连续(平行)选择性萃取程序分析了Ni,Cu,Co,Zn,Cr,Fe,Ca,Al,As和S的迁移率和固相分馏。结果表明,金属的重新分布和硫化物的氧化强度在很大程度上受尾矿的处置历史和策略(排序,由于埋葬延迟而导致硫化物暴露),蓄水结构和地下水位以及尾矿的反应性的控制。金属的重新分布表明,硫化物在尾矿表面,以及在土坝旁边的不饱和近端区域以及在水饱和的底层(可能富含O-2的渗透)中都遭受了风化作用。硫化物的氧化释放了两个位置的硫化物矿物中的微量金属。在Hitura尾矿中,由于具有足够的缓冲能力,pH值保持中性,并且动员的金属被次级Fe沉淀物保留在氧化区深处。相比之下,硫化物氧化引起的酸度和氧化后地下水位的上升显然使先前保留在Luikonlahti的金属迁移。通常,连续处置尾矿会降低活性尾矿中的硫化物氧化强度,除非延迟了埋葬时间并且沉积后反应性尾矿是不饱和的。

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