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Evolution of Acid Mine Drainage from a Coal Waste Rock Pile Reclaimed with a Simple Soil Cover

机译:简单土壤覆盖回收煤Waste石堆酸性排水的演变

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Waste rock piles (WRPs) are commonly remediated with cover systems to limit water and oxygen influx and mitigate the impacts of acid mine drainage (AMD) on the environment. While numerous types of cover systems exist, simple, single-layer soil covers remain an attractive option due to their low cost and simplicity of installation. Since knowledge of their long-term performance in humid climates is limited, this study was undertaken to assess and predict a single-layer cover system at a WRP in Nova Scotia, Canada. A two-dimensional finite element model was developed to simulate variably saturated flow and solute transport at the WRP and surrounding area. Key parameters collected during five years of field monitoring, including moisture contents, groundwater levels and dissolved metal concentrations, were used to produce a well-calibrated and verified model. Early results confirm that the cover system has already decreased AMD into both groundwater (reduced water infiltration/seepage in the WRP) and surface water (eliminated contaminated surface water runoff). Long-term acidity depletion rates indicate that all sulphidic minerals within the pile will be oxidized within 34 years, but due to the slow leaching rates into water, it will take over 9000 years to deplete all acidity. Numerical simulations predict the evolution of groundwater and surface water quality over time until full acidity depletion. Current work involves kinetic tests on waste rock samples to more accurately access the annual generation and release of AMD.
机译:石堆(WRP)通常通过覆盖系统进行修复,以限制水和氧气的流入并减轻酸性矿山排水(AMD)对环境的影响。尽管存在多种类型的覆盖系统,但简单,单层的土壤覆盖物因其成本低廉和安装简单而仍然是一种有吸引力的选择。由于对它们在潮湿气候中的长期性能的了解有限,因此本研究旨在评估和预测加拿大新斯科舍省WRP的单层覆盖系统。建立了二维有限元模型,以模拟WRP及其周围区域的可变饱和流动和溶质运移。在五年的现场监测中收集到的关键参数,包括水分含量,地下水位和溶解金属浓度,被用于建立一个经过良好校准和验证的模型。早期结果证实,覆盖系统已将AMD减少到地下水(减少WRP中的水渗透/渗漏)和地表水(消除了受污染的地表水径流)中。长期的酸耗率表明堆肥中的所有硫化矿物将在34年内被氧化,但是由于向水中的缓慢浸出率,将需要9000年的时间才能耗尽所有酸度。数值模拟预测了地下水和地表水水质随时间的变化,直至完全耗尽酸度。当前的工作包括对废石样品进行动力学测试,以更准确地获取AMD的年生成量和释放量。

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