Grup MAiMA, SGR Mineralogia Aplicada, Geoquímica i Hidrogeologia (MAGH), Departament de Mineralogia, Petrologia i Geologia Aplicada, Facultat de Ciències de la Terra, Institut de Recerca de l'Aigua (IdRA), Universitat de Barcelona (UB), Martí i Franquès s/n, 08028 Barcelona, Spain.
Grup MAiMA, SGR Mineralogia Aplicada, Geoquímica i Hidrogeologia (MAGH), Departament de Mineralogia, Petrologia i Geologia Aplicada, Facultat de Ciències de la Terra, Institut de Recerca de l'Aigua (IdRA), Universitat de Barcelona (UB), Martí i Franquès s/n, 08028 Barcelona, Spain.
Sci Total Environ. 2023 Sep 10;890:164446. doi: 10.1016/j.scitotenv.2023.164446. Epub 2023 May 24.
Porphyry-style copper deposits are characterized by low Cu grades and high tonnages, resulting in large mine tailing volumes disposed in impoundments. Due to the mining tailing sizes, waterproofing techniques cannot be applied along the dam base. Therefore, to minimize seepage towards the aquifers, pumping wells are usually installed as hydraulic barriers. Currently, there is a controversy over whether or not the water extracted from hydraulic barriers should be counted as the use of new water rights. Consequently, a growing interest to develop tools to trace and quantify the tailing impacts in groundwater and to determine the water pumped amount subjected to water rights exist. In the present study, isotope data (δH-HO, δO-HO, δS-SO and δO-SO) are proposed as a tool to quantify tailings seepage towards groundwater and to assess hydraulic barriers effectiveness. To illustrate this approach usefulness, the Quillayes porphyry Cu tailing impoundment (Chile) case study is presented. The multi-isotopic approach revealed that tailing waters are highly evaporated showing high SO content (~1900 mg L) derived from primary sulfate ore dissolution, whereas freshwaters, derived from recharge water, have low SO contents (10-400 mg L) resulting from the interaction with geogenic sulfides from barren host rock. The δH and δO values of groundwater samples collected downstream from the impoundment suggest a mixing at different proportions of highly evaporated water from the mine tailing waters and non-evaporated regional fresh groundwater. Cl/SO, δS-SO/δO-SO, δS-SO/ln(SO) and δH-HO/δO-HO mixing models allowed to determine that groundwater located closer to the impoundment had a mine tailing water contribution from 45 to 90 %, whereas those located farther away had lower contribution (5-25 %). Results confirmed the stable isotope usefulness to determine the water origin and to calculate the hydraulic barrier efficiencies and the pumped water proportions unrelated to the mining tailing subject to the water rights.
斑岩型铜矿的特点是铜品位低、吨位高,导致大量矿山尾矿堆积在堤坝中。由于尾矿粒径较大,无法沿坝基进行防水处理。因此,通常会安装抽水井作为水力屏障,以最大限度地减少向含水层的渗漏。目前,对于从水力屏障中抽取的水是否应算作新的水权使用存在争议。因此,人们越来越有兴趣开发工具来追踪和量化尾矿对地下水的影响,并确定受水权限制的抽水量。在本研究中,同位素数据(δH-H2O、δO-H2O、δS-SO4 和 δO-SO4)被提议作为量化尾矿向地下水渗漏并评估水力屏障有效性的工具。为了说明这种方法的有用性,本文介绍了智利 Quillayes 斑岩铜尾矿坝的案例研究。多同位素方法表明,尾矿水蒸发强烈,SO4 含量高(~1900 mg/L),源于原矿硫酸盐的溶解,而源于补给水的淡水 SO4 含量较低(10-400 mg/L),这是由于与贫宿主岩石中的地球成因硫化物相互作用所致。从尾矿坝下游采集的地下水样品的 δH 和 δO 值表明,高度蒸发的尾矿水和非蒸发的区域淡水以不同比例混合。Cl/SO4、δS-SO4/δO-SO4、δS-SO4/ln(SO4) 和 δH-H2O/δO-H2O 混合模型表明,靠近尾矿坝的地下水有 45%至 90%的尾矿水贡献,而远离尾矿坝的地下水贡献较低(5%至 25%)。结果证实了稳定同位素在确定水的来源、计算水力屏障效率以及计算与矿山尾矿无关的受水权限制的抽水量方面的有用性。