School of Minerals and Energy Resources Engineering, The University of New South Wales, Sydney, NSW, Australia.
Division of Sustainable Resources Engineering, Graduate School of Engineering, Hokkaido University, Sapporo, Japan.
J Hazard Mater. 2022 Sep 15;438:129453. doi: 10.1016/j.jhazmat.2022.129453. Epub 2022 Jun 24.
Historical tailings storage facilities (TSFs) are either abandoned or sparsely rehabilitated promoting acid mine drainage (AMD) formation and heavy metal release. To sustainably manage these sites, a geochemical audit coupled with numerical simulation to predict AMD flow paths and heavy metal migration are valuable. In this study, a 40-year-old TSF in Hokkaido, Japan was investigated. Tailings in this historical TSF contain pyrite (FeS) while its copper (Cu) and zinc (Zn) contents were 1400-6440 mg/kg and 2800-22,300 mg/kg, respectively. Copper and Zn were also easily released in leaching tests because they are partitioned with the exchangeable phase (29% of Zn; 15% of Cu) and oxidizable fraction (25% of Zn; 33% of Cu). Kinetic modeling results attributed AMD formation to the interactions of pyrite and soluble phases in the tailings with oxygenated groundwater, which is supported by the sequential extraction and leaching results. Calibrations of groundwater/AMD flow and solute transport in the 2D reactive transport model were successfully done using hydraulic heads measured on-site and leaching results, respectively. The model forecasted the quality of AMD to deteriorate with time and AMD formation to continue for 1000 years. It also predicted ~24% AMD flux reduction, including lower Zn release with time when recharge reduction interventions are implemented on-site.
历史尾矿库(TSF)要么被废弃,要么只是简单修复,这促进了酸性矿山排水(AMD)的形成和重金属的释放。为了可持续管理这些场地,地质化学审计与数值模拟相结合,以预测 AMD 流径和重金属迁移是非常有价值的。在本研究中,对日本北海道一个 40 年历史的 TSF 进行了调查。该历史 TSF 中的尾矿含有黄铁矿(FeS),其铜(Cu)和锌(Zn)含量分别为 1400-6440 mg/kg 和 2800-22300 mg/kg。在浸出试验中,Cu 和 Zn 也很容易释放出来,因为它们与可交换相(Zn 的 29%;Cu 的 15%)和可氧化相(Zn 的 25%;Cu 的 33%)一起分配。动力学建模结果表明,AMD 的形成是由于尾矿中的黄铁矿和可溶性相与含氧地下水相互作用的结果,这与顺序提取和浸出结果相吻合。使用现场测量的水力水头和浸出结果分别对地下水/AMD 流和二维反应传输模型中的溶质传输进行了校准。该模型预测 AMD 的质量将随时间恶化,AMD 的形成将持续 1000 年。它还预测了~24%的 AMD 通量减少,包括当现场实施补给减少干预时,随着时间的推移 Zn 释放量的降低。