首页> 外文期刊>Journal of African earth sciences >Geochemistry and water quality assessment of central Main Ethiopian Rift natural waters with emphasis on source and occurrence of fluoride and arsenic
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Geochemistry and water quality assessment of central Main Ethiopian Rift natural waters with emphasis on source and occurrence of fluoride and arsenic

机译:埃塞俄比亚主要裂谷中部天然水的地球化学和水质评估,重点是氟化物和砷的来源和发生

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Drinking water supply for the Main Ethiopian Rift (MER) area principally relies on groundwater wells and springs and is characterized by natural source of elevated fluoride concentration. New analyses reveal that the F~- geochemical anomaly is associated with other potentially toxic elements such as As, U, Mo and B. Particularly, 35% of the 23 investigated groundwater wells and 70% of the 14 hot springs (and geo-thermal wells) show arsenic concentrations above the recommended limit of 10μg/L (WHO, 2006). Arsenic in groundwater wells has a positive correlation with Na~+ (R~2 = 0.63) and alkalinity (HCO_3~-;R~2 = 0.70) as well as with trace elements such as U (R~2 = 0.70), Mo (R~2 = 0.79) and V (R~2 - 0.68). PHREEQC speciation modelling indicates that Fe oxides and hydroxides are stable in water systems, suggesting their role as potential adsorbents that could influence the mobility of arsenic.rnChemical analyses of leachates from MER rhyolitic rocks and their weathered and re-worked fluvio-lacustrine sediments were performed to evaluate their contribution as a source of the mentioned geochemical anomalies. These leachates were obtained from a 1-year leaching experiment on powdered rocks and sediments mixed with distilled water (10 g:50 ml). They contain as much as 220 μg/L of As, 7.6 mg/L of F~-, 181 μg/L of Mo, 64 μg/L of U and 254 ug/L of V suggesting that the local sediments represent the main source and reservoir of toxic elements.rnThese elements, originally present in the glassy portion of the MER rhyolitic rocks were progressively concentrated in weathered and re-deposited products.rnTherefore, together with the renowned F~- problem, the possible presence of further geochemical anomalies have to be considered in water quality issues and future work has to investigate their possible health impact on the population of MER and other sectors of the East African Rift.
机译:埃塞俄比亚大裂谷(MER)地区的饮用水供应主要依赖于地下水井和泉水,其特点是氟化物浓度升高的天然来源。新的分析表明,F〜-地球化学异常与其他潜在的有毒元素(例如As,U,Mo和B)有关。特别是,在23个被调查的地下水井中有35%,在14个温泉中有70%(和地热)。孔)的砷浓度超过建议的10μg/ L的限值(WHO,2006)。地下水井中的砷与Na〜+(R〜2 = 0.63)和碱度(HCO_3〜-; R〜2 = 0.70)以及微量元素如U(R〜2 = 0.70),Mo有正相关关系(R〜2 = 0.79)和V(R〜2- 0.68)。 PHREEQC形态建模表明,Fe氧化物和氢氧化物在水系统中稳定,表明它们是可能影响砷迁移率的潜在吸附剂。进行了MER流变岩渗滤液及其风化和再加工后的河湖沉积物的化学分析评估它们作为上述地球化学异常源的贡献。这些沥出液是通过对粉状岩石和沉积物与蒸馏水(10 g:50 ml)混合进行的为期1年的浸出实验获得的。它们含有高达220μg/ L的As,7.6 mg / L的F〜-,181μg/ L的Mo,64μg/ L的U和254 ug / L的V,这表明本地沉积物是主要来源这些原本存在于MER流纹岩玻璃部分的元素逐渐集中在风化和再沉积的产品中。因此,再加上著名的F〜-问题,可能存在进一步的地球化学异常在水质问题中需要考虑的问题,未来的工作必须调查其对中东和北非裂谷及其他地区的MER人口可能造成的健康影响。

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