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Causes and impacts of a mine water spill from an acidic pit lake (Iberian Pyrite Belt)

机译:来自酸性坑湖(Iberian Pytite带)的矿井水溢出的原因及影响

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In May 2017, a spill from La Zarza pit lake (SW Spain) resulted in the release of approximately 270,000 m(3) of extremely acidic waters to the Odiel River. Around 780 x 10(3)kg of Fe, 170 x 10(3)kg of Al, 2.15 x 10(3)kg of As and high amounts of other trace metals and metalloids were spilled. The purpose of this study is to explain the causes, consequences and impacts of the mine spill on the receiving water bodies. To this end, an extensive sampling along the mine site, river and estuary as well as a hydrological model of the pit lake was performed. Around 53 km of the Odiel River's main course, which was already contaminated by acid mine drainage (AMD), were affected. The mine spill resulted in an incremental impact on the Odiel River water quality. Thus, dissolved concentrations of some elements increased in the river up to 450 times; e.g. 435 mg/L of Fe and 0.41 mg/L of As. Due to low pH values (around 2.5), most metals (e.g., Cu, Zn, Mn, Cd) were transported in the dissolved phase to the estuary, exhibiting a conservative behavior and decreasing their concentration only due to dilution. However, dissolved concentrations of Fe, Cr, Pb, Se, Sb, Ti, V and especially As decreased significantly along the river due to Fe precipitation and sorption/coprecipitation processes. At the upper zone of the estuary, a noticeable increment of metal concentrations (up to 77 times) was also recorded. The water balance illustrates the existence of groundwater inputs (at least 16% of total) to the pit lake, due probably to local infiltration of rainwater at the mining zone. The probable existence of an ancient adit connected to the pit lake indicates that potential releases could occur again if adequate prevention measures are not adopted. (C) 2019 Elsevier Ltd. All rights reserved.
机译:2017年5月,来自La Zarza Pit Lake(SW Spain)的泄漏,导致大约270,000米(3)个极其酸性的水域释放到Odiel河上。溢出了约780×10(3)千克,170×10(3)千克,2.15×10(3)千克,2.15×10(3)千克的AS和大量的其他痕量金属和金属体。本研究的目的是解释矿井溢出对接收水体的原因,后果和影响。为此,沿着矿山,河流和河口以及坑湖的水文模型进行了广泛的采样。距离Odiel River的主要课程约53公里,已经受到酸性矿山排水(AMD)的污染,受到影响。矿井泄漏导致对Odiel河水质量的增量影响。因此,在河水中溶解浓度增加450次;例如435毫克/升Fe和0.41毫克/升。由于低pH值(约2.5),大多数金属(例如,Cu,Zn,Mn,Cd)在溶解的相中运输到河口,表现出保守的行为,并且仅由于稀释而降低它们的浓度。然而,由于Fe沉淀和吸附/共沉淀过程,溶解浓度的Fe,Cr,Pb,Se,Sb,Ti,V尤其如此显着降低。在河口的上部区域,还记录了金属浓度的显着增量(高达77次)。水平显示出在坑湖的地下水输入(总共总共的16%),这可能是矿井雨水的局部渗透。连接到坑湖的古代Adit的可能存在表明如果未采用充分的预防措施,可能会再次发生潜在的释放。 (c)2019 Elsevier Ltd.保留所有权利。

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