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Metal contamination of the environment by placer and primary gold mining in the Adola region of southern Ethiopia

机译:埃塞俄比亚南部阿多拉地区的砂金和原生金矿开采对环境的金属污染

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摘要

Primary and placer gold mining sites in southern Ethiopia were studied to see the contribution of mining to the accumulation of metals in different environmental media. Sediment, water and plant samples were analyzed for Al, Mn, Fe, As, Ni, Cr, Cu, Co, Pb, W, Sb, Mo, Zn and V. Water parameters (pH, Eh, TDS, anions and cations) were also measured. The sediment analyses results show that the most abundant metals are Ni (average 224.7 mg/kg), Cr (199 mg/kg), Cu (174.2 mg/kg), V (167.3 mg/kg), Zn (105.5 mg/kg), Pb (61.5 mg/kg) and As (59.7 mg/kg) in the primary gold mining sites while the placer sites show high concentration of V (average 301.2 mg/kg), Cr (260.4 mg/kg), Zn (179 mg/kg), Ni (113.4 mg/kg), Cu (46.7 mg/kg), As (32.2 mg/kg) and Co (31 mg/kg). The metals Cu, Ni, W, Cr, As and Pb in primary and Sb, W, Cr, Ni, Zn, As and Mo in placer gold mining sites have geoaccumulation indexes (I_(geo)) from one to four indicating considerable accumula- tion of these metals. Waters from both primary and placer mining sites are near neutral to alkaline. Arsenic (average 92.8 μg/l), Ni (276.6 μg/l), Pb (18.7 μg/l), Sb (10.7 μg/l), Mn (1 mg/l), Fe (8.3 mg/l) and Al (23.8 mg/l) exceeded the guideline value for drinking water. Plants show high concentration of Cr (average 174.5 mg/kg), Ni (163.5 mg/kg), Zn (96 mg/kg) and W (48 mg/kg). Zinc, W, Mo, Ni and Cr show the maximum biological absorption coefficient (BAC) ranging 0.4-1.7, 0.1-104.6, 1.1-2.6, 0.2-1.6 and 0.2-3.6, respectively, and the results suggest bioaccumulation of these elements in plants. The minerals especially sulfides in the ore aggregate are the ultimate source of the metals. The release of the metals into the environmental media is facilitated (in addition to normal geologic processes) by human activities related to gold mining.
机译:对埃塞俄比亚南部的主要和砂金矿产地进行了研究,以了解采矿对不同环境介质中金属积累的贡献。分析了沉积物,水和植物样品中的Al,Mn,Fe,As,Ni,Cr,Cu,Co,Pb,W,Sb,Mo,Zn和V.水参数(pH,Eh,TDS,阴离子和阳离子)也进行了测量。沉积物分析结果表明,最丰富的金属是镍(平均224.7 mg / kg),铬(199 mg / kg),铜(174.2 mg / kg),钒(167.3 mg / kg),锌(105.5 mg / kg)。 ),主要金矿中的Pb(61.5 mg / kg)和As(59.7 mg / kg),而砂矿中的V(平均301.2 mg / kg),Cr(260.4 mg / kg),Zn( 179毫克/千克),镍(113.4毫克/千克),铜(46.7毫克/千克),砷(32.2毫克/千克)和钴(31毫克/千克)。砂矿金矿中的金属Cu,Ni,W,Cr,As和Pb以及砂金矿中的Sb,W,Cr,Ni,Zn,As和Mo的地质累积指数(I_(geo))从1到4表明有大量的积累-这些金属的阳离子。来自初级开采和砂矿开采的水都接近中性至碱性。砷(平均92.8μg/ l),镍(276.6μg/ l),铅(18.7μg/ l),锑(10.7μg/ l),锰(1 mg / l),铁(8.3 mg / l)和铝(23.8 mg / l)超出了饮用水的指导值。植物显示出高浓度的Cr(平均174.5 mg / kg),Ni(163.5 mg / kg),Zn(96 mg / kg)和W(48 mg / kg)。锌,钨,钼,镍和铬的最大生物吸收系数(BAC)分别为0.4-1.7、0.1-104.6、1.1-2.6、0.2-1.6和0.2-3.6,结果表明这些元素在水中的生物累积植物。矿石聚集物中的矿物特别是硫化物是金属的最终来源。与金矿开采有关的人类活动促进了金属向环境介质的释放(除了正常的地质过程之外)。

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