首页> 外文期刊>Journal of African Earth Sciences >Characterization and environmental impact assessment of gold mine tailings in arid regions: A case study of Barramiya gold mine area, Eastern Desert, Egypt
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Characterization and environmental impact assessment of gold mine tailings in arid regions: A case study of Barramiya gold mine area, Eastern Desert, Egypt

机译:干旱地区金矿尾矿的特征及环境影响评价-以埃及东部沙漠Barramiya金矿区为例

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Geochemical and mineralogical characterization and environmental impact assessment were performed on Barramiya gold mine tailings, Eastern Desert, Egypt. The Barramiya gold mine is situated within ophiolitede-corated Nugrus suture zone, which composed of dismembered sequence of highly deformed and metamorphosed mafic to ultramafic rocks and their hydrothermal alteration products (carbonate rocks), interbedded with meta-volcano clastic rocks of the Nubian Shield. Morphometric parameters were quantified using ArcGIS 10.0 with Shuttle Radar Topography Mission (SRTM) maps. A total of four tailings samples were gathered and analysed by XRF, XRD, ICP-OES/MS and ESEM. Tailings are characterized by homogeneous silty fine sand, high carbonates in the form of dolomite and ankerite, and low sulfides content in the form of arsenopyrite and pyrite relics. High concentration averages of heavy elements are found for As (2936 mg/kg), Cr (237 mg/kg), Sr (219 mg/kg), Ni (150 mg/kg), V (131 mg/kg), Zn (64 mg/kg), Cu (51 mg/kg), Co (19 mg/kg) and Pb (12 mg/kg). They reflect mafic and ultramafic rocks, graphite schists, and quartz veins of the study area. Gypsum is present as secondary phase, identified in the shrinkage crack fillings. Morphometric drainage basin parameters for wadi Barramiya basin show rectangular to subdendritic drainage pattern with a moderate hazard degree. This study recommends designing multiple-layered dry cover, overlain by plant cover at uppermost part for treatment of the gold mine tailings; otherwise, wind and water erosion can easily remove all dissolved and unconsolidated material that absorb heavy elements and would create a potential risk to the surrounding ecosystem.
机译:在埃及东部沙漠的Barramiya金矿尾矿进行了地球化学和矿物学表征以及环境影响评估。巴拉米亚(Barramiya)金矿位于蛇麻岩状的Nugrus缝合带内,该断裂带由高度变形和变质的镁铁质到超镁铁质岩及其热液蚀变产物(碳酸盐岩)的解体序列组成,并与努比亚盾构的超火山碎屑岩互层。使用带有Shuttle Radar Topography Mission(SRTM)地图的ArcGIS 10.0对形态学参数进行了量化。总共收集了四个尾矿样品,并通过XRF,XRD,ICP-OES / MS和ESEM进行了分析。尾矿的特征是均质粉质细砂,白云石和铁矾石形式的高碳酸盐,毒砂和黄铁矿遗迹形式的低硫化物。砷(2936 mg / kg),铬(237 mg / kg),锶(219 mg / kg),镍(150 mg / kg),钒(131 mg / kg),锌的重元素的高浓度平均值(64 mg / kg),Cu(51 mg / kg),Co(19 mg / kg)和Pb(12 mg / kg)。它们反映了研究区域的镁铁质和超镁铁质岩石,石墨片岩和石英脉。石膏存在于次生相中,在收缩裂纹填料中已确定。旱谷巴拉米亚盆地的形态排水盆地参数显示为矩形至亚树突状排水模式,危害程度中等。本研究建议设计多层干式覆盖层,在最上部覆盖植物覆盖层,以处理金矿尾矿。否则,风蚀和水蚀会轻易清除所有吸收和吸收重元素的溶解和未固结材料,并对周围的生态系统造成潜在风险。

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