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OCHRE PRECIPITATES AND ACID MINE DRAINAGE IN A MINE ENVIRONMENT

机译:矿山环境中的OCEC沉淀物和酸性矿山排水

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This paper is focused to characterize the ochre precipitates and the mine water effluents of some old mine adits and settlingpits after mining of polymetallic ores in Slovakia. It was shown that the mine water effluents from two different typesof deposits (adits; settling pits) have similar composition and represent slightly acidic sulphate water (pH in range5.60-6.05, sulphate concentration from 1160 to 1905 g.dm~(-3)). The ochreous precipitates were characterized by methodsof X-ray diffraction analysis (XRD), scanning electron microscopy (SEM) and B.E.T. method for measuring the specificsurface area and porosity. The dominant phases were ferrihydrite with goethite or goethite with lepidocrocide.
机译:本文着重介绍了斯洛伐克多金属矿石开采后一些老矿坑和沉降坑的the石沉淀物和矿山废水的特征。结果表明,两种不同类型矿床(进水口,沉降坑)的矿井出水成分相似,代表的是弱酸性硫酸水(pH值在5.60-6.05范围内,硫酸盐浓度在1160至1905 g.dm〜(-3)之间。 ))。通过X射线衍射分析(XRD),扫描电子显微镜(SEM)和B.E.T.测量比表面积和孔隙率的方法。主导相为带针铁矿的水铁矿或带吡doc环磷酰胺的针铁矿。

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