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

机译:酸性坑湖(伊比利亚黄铁矿带)漏出矿井水的原因和影响

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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,La Zarza pit湖(西班牙西南部)发生泄漏,导致向奥迪尔河释放了约270,000 m(3)的极酸性水。约有780 x 10(3)kg的铁,170 x 10(3)kg的铝,2.15 x 10(3)kg的砷以及大量其他痕量金属和准金属溢出。这项研究的目的是解释地雷泄漏对接收水体的原因,后果和影响。为此,沿矿区,河流和河口进行了广泛的采样,并进行了矿坑湖的水文模型研究。已被酸性矿山排水系统(AMD)污染的奥迪尔河主干道约53公里受到了影响。矿井漏水对奥迪尔河的水质产生了越来越大的影响。因此,河流中某些元素的溶解浓度增加了450倍。例如铁435 mg / L,砷As 0.41 mg / L。由于较低的pH值(约2.5),大多数金属(例如Cu,Zn,Mn,Cd)以溶解相的形式运到河口,表现出保守的行为,并且仅由于稀释而降低了其浓度。然而,由于铁的沉淀和吸附/共沉淀过程,沿河的Fe,Cr,Pb,Se,Sb,Ti,V,尤其是As的溶解浓度显着下降。在河口的上部区域,还记录到金属浓度显着增加(高达77倍)。水平衡表明,坑湖存在地下水输入(至少占总量的16%),这可能是由于矿区雨水的局部渗透所致。与坑湖相连的古代平地可能存在,这表明如果不采取适当的预防措施,可能再次发生潜在的释放。 (C)2019 Elsevier Ltd.保留所有权利。

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