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首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >Acid drainage reassessment of mining tailings, Black Swan Nickel Mine, Kalgoorlie, Western Australia
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Acid drainage reassessment of mining tailings, Black Swan Nickel Mine, Kalgoorlie, Western Australia

机译:西澳大利亚州卡尔古利黑天鹅镍矿的尾矿酸排泄评估

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This paper describes the geochemical testing of mine tailings sourced from the Black Swan Ni Mine located near Kalgoorlie, Western Australia. Acid-base accounting was used to provide an indication of the acid generating capacity of two kinds of mining tailings: disseminated-ore tailings from the Cygnet Tailings Dam Storage Facility (CTDSF) and massive-ore tailings from the Silver Swan Tailings Dam Storage Facility (SSTDSF). All of the tailings in SSTDSF have acid generating potential which is consistent with previous research reports. New findings in this paper reveal that approximately 16% of the tailings in CTDSF have the potential to be acid generating. In contrast, previous reports state that the disseminated-ore tailings are classified as non-acid forming. Most of the potential acid generating tailings in the CTDSF are found in the upper-middle sections of the tailings profile, but some are located at the bottom of the tailings dam. The upper-middle section of the tailings is oxidized because these tailings have interacted with atmospheric O-2 and rain and surface water. Oxidation of the bottom tailings in the CTDSF may be due to infiltration of ground water into hidden fractures under the east bank of CTDSF, which caused these tailings to oxidize under closed and reduced conditions.The acid drainage in the tailings dam storage facility was observed 3 a, after the development of the Black Swan Nickel project. This delayed production of acid drainage was likely due to the slow rates of acid neutralization provided by alteration gouge minerals such as Mg/Fe-carbonates (magnesite-siderite series) associated with the Ni ores. The acid drainage leaking from the tailings dams has contaminated neighboring ground water via increased acidity and heavy metals.Because of the potential acid generation in some of the disseminated ore tailings, it is inadvisable to use disseminated ore tailings as cover materials in the storage facility to isolate the underlying potentially-acid-forming tailings from O-2 and water, as proposed by previous research reports. (C) 2004 Elsevier Ltd. All rights reserved.
机译:本文介绍了来自位于西澳大利亚卡尔古利附近的黑天鹅镍矿的矿山尾矿的地球化学测试。酸碱法可用来表明两种采矿尾矿的产酸能力:小天鹅尾矿坝存储设施(CTDSF)的散矿尾矿和银天鹅尾矿坝存储设施的大矿石尾矿( SSTDSF)。 SSTDSF中的所有尾矿都有产酸的潜力,这与以前的研究报告一致。本文的新发现表明,CTDSF中约有16%的尾矿具有产酸的潜力。相反,以前的报告指出,分散的矿石尾矿被归类为非酸形成。 CTDSF中大多数潜在的产酸尾矿位于尾矿剖面的中上部分,但有些位于尾矿坝的底部。尾矿的中上部分被氧化,因为这些尾矿与大气中的O-2以及雨水和地表水相互作用。 CTDSF底部尾矿的氧化可能是由于地下水渗入CTDSF东岸下方的隐蔽裂缝,导致这些尾矿在封闭和还原条件下被氧化。在尾矿坝存储设施中观察到酸排出3 a,在开发黑天鹅镍项目之后。酸排泄的延迟产生可能是由于与镍矿石相关的变质凿岩矿物(例如Mg / Fe碳酸盐(菱镁矿-菱铁矿系列))提供的酸中和速度缓慢。尾矿坝泄漏的酸排出物通过增加酸度和重金属污染了附近的地下水。由于某些散布的矿石尾矿可能产生酸,因此不建议使用散布的矿石尾矿作为存储设施中的覆盖材料如先前的研究报告所建议,从O-2和水中分离出潜在的潜在酸形成尾矿。 (C)2004 Elsevier Ltd.保留所有权利。

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