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Oxidation Dynamics and Composition of the Flotation Plant Derived Tailing Impoundment Aquisgrana (Spain)

机译:浮选厂尾矿蓄水阿奎斯格拉纳(西班牙)的氧化动力学和组成

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A tailing impoundment situated in the mining district of La Carolina (Spain), which stores waste resulting from the washing of Pb and Ag sulphides, was studied 30 years after it was abandoned. Fibre optic sensors were installed to record humidity, temperature, electrical conductivity and oxygen content in the pores down to a depth of 35.5 m. The oxygen profiles show an oxidised thickness of 5 m, meaning that the speed of the advancing oxidation front is estimated as 15 cm year(-1). Sediment samples were obtained from different depths, and parameters such as pH, carbonates and metal(loid)s, among others, were analysed. High concentrations of As (> 500 mg kg(-1)), Fe (> 34,000 mg kg(-1)), Mn (> 900 mg kg(-1)), Pb (> 8000 mg kg(-1)) and Zn (> 5000 mg kg(-1)) were found. A piezometer was installed to enable the water inside the tailing pond to be sampled, and this presented high contents of SO42- (> 2400 mg L-1), Fe (> 28,000 mu g L-1), Mn (> 7800 mu g L-1) and Zn (> 7000 mu g L-1), suggesting that the mineral leaching was related to the oscillations in the water table. The water from two drainage adits situated at the foot of the impoundment was also analysed, as well as surface water both upstream and downstream from it. The speciation-saturation models applied for these water samples indicated that in spite of the contamination potential of the impoundment, the deterioration in the quality of the river water is mainly due to the discharge from mining drains and the dissolution processes of precipitates accumulated along the riverbanks.
机译:在废弃的30年后,对位于拉卡罗来纳(西班牙)矿区的尾矿库进行了研究,该尾矿库存储了因洗涤铅和硫化银而产生的废物。安装了光纤传感器以记录直至35.5 m深度的孔中的湿度,温度,电导率和氧含量。氧分布显示出5 m的氧化厚度,这意味着前进的氧化锋的速度估计为15 cm年(-1)。从不同深度获得了沉积物样品,并分析了诸如pH,碳酸盐和金属(金属)等参数。高浓度的As(> 500 mg kg(-1)),Fe(> 34,000 mg kg(-1)),Mn(> 900 mg kg(-1)),Pb(> 8000 mg kg(-1))和锌(> 5000 mg kg(-1))被发现。安装了压力计,以便对尾矿池中的水进行采样,结果显示出高含量的SO42-(> 2400 mg L-1),Fe(> 28,000 mu g L-1),Mn(> 7800 mu g L-1)和Zn(> 7000μg L-1),表明矿物浸出与地下水位的波动有关。还分析了位于蓄水池底部的两个排水口的水,以及上游和下游的地表水。用于这些水样的形态饱和度模型表明,尽管蓄水场有潜在的污染潜力,但河水水质的下降主要归因于采矿排水沟的排放以及沿河岸堆积的沉淀物的溶解过程。 。

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