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Factors that influence coal mine drainage chemistry West Coast, South Island, New Zealand

机译:影响煤矿排水化学的因素西海岸,新西兰南岛

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摘要

Coal mine drainage chemistry on the West Coast of the South Island is highly variable; pH ranges from about 2-8, and chemical concentrations vary by several orders of magnitude. Factors that influence mine drainage chemistry on the West Coast include regional geology, mine type, hydrogeology, and local geology. At a regional scale, mine drainage chemistry is bimodal and relates to geological formations. Mines within the Paparoa Coal Measures have neutral mine drainage, whereas those within the Brunner Coal Measures have acid mine drainage. This is related to the availability of SO_4 during coal measures deposition and, in combination with Fe and organic material, the subsequent formation of pyrite during burial. Paparoa Coal Measures were deposited in alluvial to lucustrine environments where SO_4 was relatively unavailable, whereas Brunner Coal Measures were deposited in alluvial to estuarine to marginal marine settings where marine SO_4 was abundant. Brunner Coal Measures acid mine drainage chemistry is influenced by mine type; open cast mines have Al- and trace element-rich acid mine drainage compared to underground mines. Acid mine drainage forming reactions that release trace elements and Al proceed more rapidly and completely at open cast mines where mine waste has a higher reactive surface area compared to waste rock at underground mines. Brunner coal mine drainage chemistry is also influenced by hydrogeology where flooded underground mines release less acid than free-draining mines because there is less oxygen available to react with pyrite. In addition, local geology overprints mine drainage chemistry where differences in acid mine drainage chemistry arise from changes in contributing lithologies either within a single mine or between different coalfields. Identification of factors that control mine drainage chemistry enables prediction of mine drainage chemistry. These predictions have application to the mining industry for managing, mitigating, monitoring, and remediation of mine drainages that would otherwise cause negative environmental impact.
机译:南岛西海岸的煤矿排水化学变化很大。 pH值约为2-8,化学浓度变化几个数量级。影响西海岸矿山排水化学的因素包括区域地质,矿山类型,水文地质和当地地质。在区域范围内,矿山排水化学是双峰的,并且涉及地质构造。 Paparoa煤炭措施中的煤矿具有中性矿井排水,而Brunner煤炭措施中的煤矿具有酸性矿井排水。这与煤层沉积过程中SO_4的可用性以及与铁和有机材料的结合以及随后在埋葬过程中形成黄铁矿有关。 Paparoa煤系沉积在相对于SO_4相对缺乏的冲积至浅水环境中,而Brunner煤系沉积于海洋SO_4丰富的冲积至河口至边缘海洋环境中。 Brunner Coal措施公司酸性矿山的排水化学受矿山类型的影响。与地下矿山相比,露天矿具有富含Al和微量元素的酸性矿山排水。与露天矿的废石相比,露天矿的酸性矿山排水形成反应释放出微量元素和铝,反应更快,更完全,而露天矿的反应表面积更大。 Brunner煤矿的排水化学也受到水文地质的影响,因为与可排水黄铁矿反应的氧气较少,淹没的地下矿井释放的酸少于自由排水的矿井。此外,当地的地质特征覆盖了矿山的排水化学,其中酸性矿山的排水化学差异是由于单个矿山内或不同煤田之间的贡献岩性变化而引起的。识别控制矿井排水化学的因素可以预测矿井排水化学。这些预测已应用于采矿业,以管理,缓解,监测和补救可能会造成负面环境影响的矿井排水。

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