首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >Contaminant leaching from gold mining tailings dams in the Witwatersrand Basin, South Africa: A new geochemical modelling approach
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Contaminant leaching from gold mining tailings dams in the Witwatersrand Basin, South Africa: A new geochemical modelling approach

机译:南非威特沃特斯兰德盆地金矿尾矿坝中的污染物浸出:一种新的地球化学模拟方法

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In this study a new geochemical reaction modelling methodology is used to shed light on the geochemical processes within Witwatersrand tailings impoundments and the evaluation of the geochemical impacts for future mining projects is evaluated. Information from international and local studies on tailings sulphidic tailings impoundments is used to develop a conceptual understanding on a typical Witwatersrand gold tailings impoundment. The tailings impoundments consist of 3 distinct geochemical zones: Oxidation Zone (OZ), a Transition Zone (TZ) and a Reduction Zone (RZ). Individual reaction models are developed for each of the 3 zones. The output of one model is used as an input to the next in spatial order. The results of the final model represent the tailings basal seepage characteristics, which indicate the most likely impacts on groundwater resources. The model results agree with existing information on AMD in the Witwatersrand. The results indicate that the tailings basal seepage is likely to be acidic (pH of similar to 3.5), containing elevated concentrations of SO4 and trace metals (Al, Co, Cr, Cu, Mn, Ni, Zn and U). Predicted Fe concentrations are low, due to the low f(O2) in the TZ and RZ and the buffering effect of the precipitation of K-jarosite in the OZ and TZ. This study therefore indicates that the methodology employed produces results that can be correlated to existing information and can thus be used as a methodology in the assessments of impacts from sulphidic tailings material for future mining projects. (C) 2015 Elsevier Ltd. All rights reserved.
机译:在这项研究中,使用了一种新的地球化学反应建模方法,以阐明威特沃特斯兰德尾矿库中的地球化学过程,并对未来采矿项目的地球化学影响进行了评估。来自国际和地方研究的关于尾矿硫化物尾矿库的信息被用于发展对典型的威特沃特斯兰德金尾矿库的概念理解。尾矿库房由3个不同的地球化学区组成:氧化区(OZ),过渡区(TZ)和还原区(RZ)。针对3个区域中的每一个开发了单独的反应模型。一个模型的输出按空间顺序用作下一个模型的输入。最终模型的结果代表了尾矿的基础渗流特征,表明了对地下水资源的最可能影响。模型结果与Witwatersrand中有关AMD的现有信息一致。结果表明,尾矿的基础渗流很可能是酸性的(pH值接近3.5),其中含有较高浓度的SO4和微量金属(Al,Co,Cr,Cu,Mn,Ni,Zn和U)。由于TZ和RZ中的f(O2)低以及OZ和TZ中钾铁矾石沉淀的缓冲作用,因此预测的铁浓度较低。因此,这项研究表明,所采用的方法所产生的结果可以与现有信息相关,因此可以用作评估硫化尾矿材料对未来采矿项目的影响的方法。 (C)2015 Elsevier Ltd.保留所有权利。

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