首页> 外文期刊>Journal of Applied Geophysics >Combined DC resistivity and induced polarization (DC-IP) for mapping the internal composition of a mine waste rock pile in Nova Scotia, Canada
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Combined DC resistivity and induced polarization (DC-IP) for mapping the internal composition of a mine waste rock pile in Nova Scotia, Canada

机译:组合直流电阻率和诱导极化(DC-IP),用于在加拿大新斯科舍省的矿井废岩桩的内部组成

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Mine waste rock piles (WRPs) can contain sulfidic minerals whose interaction with oxygen and water can generate acid mine drainage (AMD). Thus, WRPs can be a long-term source of environmental pollution. Since the generation of AMD and its release into the environment is dependent on the net volume and bulk Composition of waste rock, effective characterization of WRPs is necessary for successful remedial design and monitoring. In this study, a combined DC resistivity and induced polarization (DC-IP) approach was employed to characterize an AMD-generating WRP in the Sydney Coalfield, Nova Scotia, Canada. Two-dimensional (2D) DC-IP imaging with 6 survey lines was performed to capture the full WRP landform. 2D DC results indicated a highly heterogeneous and moderately conductive waste rock underlain by a resistive bedrock containing numerous fractures. 2D IP (chargeability) results identified several highly-chargeable regions within the waste, with normalized chargeability delineating regions specific to waste mineralogy only. Three-dimensional (3D) DC-IP imaging, using 17 parallel lines on the plateau of the pile, was then used to focus on the composition of the waste rock. The full 3D inverted DC-IP distributions were used to identify coincident and continuous zones (isosurfaces) of low resistivity (30 Omega-m) and high normalized chargeability (0.4 mS/m) that were inferred as generated AMD (leachate) and stored AMD (sulfides), respectively. Integrated geological, hydrogeological and geochemical data increased confidence in the geoelectrical interpretations. Knowledge on the location of potentially more reactive waste material is extremely valuable for improved long-term AMD monitoring at the WRP. (C) 2018 Elsevier B.V. All rights reserved.
机译:矿井废岩桩(WRP)可含有磺基矿物,其与氧气和水的相互作用可以产生酸性矿渗流(AMD)。因此,WRP可以是环境污染的长期来源。由于AMD的产生及其进入环境的释放取决于废岩的净体积和块状组成,因此有效表征WRP是成功的修复设计和监测所必需的。在该研究中,使用组合的直流电阻率和诱导极化(DC-IP)方法来表征在加拿大新斯科舍省悉尼煤田的AMD生成的WRP。进行二维(2D)DC-IP成像,具有6条测量线以捕获完整的WRP地貌。 2D DC结果表明,通过含有许多骨折的​​电阻基岩,高度异质和中等导电的废岩。 2D IP(充电能力)结果确定了废物内的几个高度收费的区域,仅具有常规的充电性划分区域,仅为废矿物学。然后使用三维(3D)DC-IP成像,然后使用桩平台上的17个平行线,专注于废岩的组成。完整的3D反相DC-IP分布用于识别低电阻率的重合和连续区域(ISOSurFace),以及所产生的AMD(渗滤液)推断的高电阻率(& 0.4ms / m) )分别和储存AMD(硫化物)。综合地质,水文地质和地球化学数据提高了地电气解释的置信度。关于潜在的反应性废料的位置的知识对于改善WRP的长期AMD监测来说是极大的价值。 (c)2018 Elsevier B.v.保留所有权利。

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