首页> 外文会议>International Mine Water Conference >ISOTOPIC FINGERPRINTING OF GROUND WATER NITRATE SOURCES AROUND ANGLO PLATINUM'S RPM MOGALAKWENA OPERATION (LIMPOPO PROVINCE, SOUTH AFRICA)
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ISOTOPIC FINGERPRINTING OF GROUND WATER NITRATE SOURCES AROUND ANGLO PLATINUM'S RPM MOGALAKWENA OPERATION (LIMPOPO PROVINCE, SOUTH AFRICA)

机译:Anglo Platinum的RPM Mogalakwena手术(南非湖泊省)的地下水硝酸盐来源的同位素指纹纹理

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In response to allegations made by the NGO ActionAid in early 2008 that the highly elevated nitrate levels found in groundwater in communities adjacent to Anglo's RPM Mogalakwena operation originate from activities at the platinum mine, Anglo American conducted isotope studies (both in-house and through independent researchers) with the aim to identify the natural and anthropogenic groundwater nitrate sources in the area. Results of the in-house study are presented in this paper.The results of this study demonstrate that at least three isotopically distinct nitrate end-member sources exist in the area and that mixing between these end-members can readily explain the observed compositional variations in the dataset. One of the identified end-member sources is nitrate from community-related septic waste or manure, and contamination from this source is shown to be the most likely cause of highly elevated groundwater nitrate contents in Ga-Molekana village. In contrast, effluents from the mine can be ruled out as a source of nitrate in groundwaters at Ga-Molekana on the basis of the isotopic/hydrochemical data and the westerly/south-westerly groundwater flow direction in the area.Another important nitrate end-member source identified in the area is isotopically consistent with nitrate from soil or possibly from waste rock material, as suggested by leachate data for rock material from a blast site in the Zwartfontein South Pit. The limited data available to date suggest that the source of this end-member may lie within the mine area. Mixing calculations suggest, however, that prior to the addition of nitrate from this end-member the waters must have already had highly elevated nitrate concentrations, probably due to contamination with nitrate from community-related septic effluents or manure upstream from the operation. The extent to which nitrate fluxes from the soil/waste rock end-member to the groundwater are natural or are enhanced/caused by mining-related activities is the subject of ongoing investigation.
机译:为应对2008年初非政府组织ActiveID的指控,邻近盎格鲁的RPM Mogalakwena运营的地下水中发现的地下水中发现的高度浓度硝酸盐水平来源于铂金矿的活动,英国美国进行了同位素研究(内部和通过独立研究人员)目的是鉴定该地区的天然和人为地下水硝酸盐来源。本文提出了内部研究的结果。该研究的结果表明,该区域中至少存在三个同位素不同的硝酸盐末端构件源,并且这些端构件之间的混合可以容易地解释观察到的组成变化数据集。其中一个鉴定的末端元件来源是来自与社区相关的化脓废物或粪肥的硝酸盐,并且来自该来源的污染被证明是Ga-Molekana村的高度升高的地下水硝酸盐含量的最可能原因。相比之下,矿井中的流出物可以根据同位素/水化学数据和地区的同位素/水化学数据和西方/南风地下水流动方向作为地下水的硝酸盐源。另外重要的硝酸盐末端 - 该地区鉴定的成员源与来自土壤或可能来自废岩材料的硝酸盐,如Zwartfontein南坑的爆炸部位的岩石材料所建议的。迄今为止可用的有限数据表明,这一最终成员的来源可能位于矿区内。然而,混合计算表明,在从该端构件中加入硝酸盐之前,水必须已经具有高度升高的硝酸盐浓度,这可能是由于硝酸硝酸盐从群落相关的化脓流出物或粪便上游粪便。从土壤/废岩端构件到地下水的硝酸盐通量的程度是自然的或由采矿相关活动的增强/引起的是正在进行的调查的主题。

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