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From Salt Balance to Contaminant Flux: Managing Water Quality Risk Using a Systems Approach

机译:从盐平衡到污染物助核:使用系统方法管理水质风险

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We used a salt balance to describe contaminant transfer within a mine water system. The system included mine workings, mineral processing plants, water storages (both clean and dirty), and tailings storage facilities as components. Analysis of modelling results identified sub-systems associated with potential water quality risks. In particular, approximately 6 000 tonnes of dissolved salts associated with the tailings component could not be accounted for. Under the prevailing regulatory regime, this could be a significant water quality risk. However, the fragmented monitoring network and poorly characterised hydrogeology was not able to resolve the magnitude of the risk.The cost of developing a tailings source term was significantly less than the cost of upgrading the groundwater monitoring network. Therefore, the tailings sub-system was characterised in detail. This involved collecting tailings process water and drain samples. We also collected tailings samples from various depths in the facility. Geochemical and hydraulic analysis of the tailings allowed an indicative source term to be developed. This quantified the contaminant flux through the tailings during deposition and after closure.During the operational phase approximately 1 000 tonnes per year of dissolved salts actually leaves the tailings as seepage through the footprint. The residual salt mass leaves the tailings at the rate of approximately 250 tonnes per year once the tailings have desaturated.The improved resolution of the tailings sub-system indicated that the tailings are a sink for dissolved salts in the mine water system. The fine particle size and low permeability of the tailings under compaction, is a natural mitigation that limits the rate of salt release. Therefore, the magnitude of the water quality risk was found to be moderate
机译:我们使用盐平衡来描述矿井水系统内的污染物转移。该系统包括矿山工作,矿物加工厂,水上储物(清洁脏),以及尾矿储存设施作为组件。建模结果分析确定了与潜在水质风险相关的子系统。特别地,无法解释与尾矿部件相关的约6000吨的溶解盐。根据现行监管制度,这可能是一个显着的水质风险。然而,分散的监测网络和表现差的水文地质无法解决风险的幅度。发展尾矿源期限的成本显着低于升级地下水监测网络的成本。因此,尾矿子系统的特征是详细的。这涉及收集尾矿工艺水和排水样品。我们还收集了设施中的各种深度的尾矿样本。尾矿的地球化学和水力分析允许开发指示性源术语。这通过尾矿期间通过尾矿和关闭后量化污染物通量。每年溶解盐的操作阶段约为1 000吨,实际上通过占地面积离开尾矿。一旦尾矿已经去饱和,残留的盐质量将以约250吨的速率离开尾矿。尾矿子系统的改进分辨率表明尾矿是矿井水系统中溶解盐的水槽。在压实下尾矿的细粒尺寸和低渗透性是一种自然缓解,限制了盐释放速率。因此,发现水质风险的大小是适中的

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