首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >Subsurface variations in arsenic mineralogy and geochemistry following long-term weathering of gold mine tailings
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Subsurface variations in arsenic mineralogy and geochemistry following long-term weathering of gold mine tailings

机译:金矿尾矿长期风化后砷矿物学和地球化学的地下变化

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Variations in arsenic (As) mineralogy and geochemical controls on its mobility were evaluated in subsurface tailings at the historical Montague and Goldenville mine sites in Nova Scotia, Canada. Tailings at these sites contain some of the highest As concentrations in Nova Scotia and are located in close proximity to local communities. Pore water in the subsurface tailings is characterized by circumneutral to alkaline pH (6.2 to 8.7) and mildly reducing to oxidizing redox conditions (+130 mV to +347 mV). Bulk chemistry, scanning electron microscopy, and synchrotron micro-X-ray diffraction analyses showed As mineral hosts differ with depth. The deepest tailings (max. 2 m) are in direct contact with partially decomposed vegetation, which supports reducing conditions and the precipitation of authigenic As and Fe sulfides. Under reducing conditions, dissolved As concentrations are also controlled by desorption of As from dissolution of Fe and Mn oxides and the sorption or co-precipitation of As with carbonates. These geochemical controls differ from those influencing dissolved As concentrations under oxidizing conditions. In the near surface, As mobility is controlled by oxidative dissolution of primary arsenopyrite, precipitation of secondary Fe arsenates, Fe oxyhydroxides and Mn oxides, secondary Ca-Fe arsenates, and sorption onto Fe oxyhydroxides and gangue minerals. Some of these mineral species are stable under different conditions yet occur in close association, indicating the importance of microenvironments. The results of this study show that the weathering characteristics of these tailings vary with depth, leading to the formation of new As hosts that are distinct from those observed in the near surface. Identification of these As hosts provides an understanding of current controls on As mobility and has implications for future reprocessing and/or remediation efforts. (C) 2016 Elsevier Ltd. All rights reserved.
机译:在加拿大新斯科舍省的历史悠久的蒙塔古和戈登维尔矿山的地下尾矿中,评估了砷(As)矿物学和地球化学控制其迁移率的变化。这些地点的尾矿中含有一些新斯科舍省最高的As浓度,并且紧邻当地社区。地下尾矿中的孔隙水的特征是环境pH值至碱性(6.2至8.7),并轻度还原至氧化还原条件(+130 mV至+347 mV)。大量化学,扫描电子显微镜和同步加速器X射线衍射分析表明,矿物主体随深度而不同。最深的尾矿(最大2 m)与部分分解的植被直接接触,这支持还原条件和自生砷和铁的硫化物的沉淀。在还原条件下,还可以通过溶解Fe和Mn氧化物引起的As解吸以及As与碳酸盐的吸附或共沉淀来控制溶解的As浓度。这些地球化学控制不同于那些在氧化条件下影响溶解砷浓度的控制。在近地表层中,迁移率受初级毒砂的氧化溶解,仲砷酸铁,Fe羟基氧化物和Mn氧化物,仲Ca-Fe砷酸盐的沉淀以及在Fe羟基氧化物和脉石矿物上的吸附控制。这些矿物质中的某些在不同条件下是稳定的,但密切相关,这表明了微环境的重要性。这项研究的结果表明,这些尾矿的风化特性随深度而变化,从而导致形成了新的As寄主,该新的As寄主不同于在近地表中观察到的那些寄主。这些As宿主的识别可帮助您了解当前对As迁移的控制,并对将来的后处理和/或补救工作具有影响。 (C)2016 Elsevier Ltd.保留所有权利。

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