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Trace element geochemistry of the Keana brines field, middle Benue trough, Nigeria

机译:尼日利亚贝努中槽的基亚纳盐田的微量元素地球化学

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A trace elements study of various samples from the Keana brines field, middle Benue Trough was carried-out to determine the extent to which Pb-Zn-S and BaSO_4 mineralisations have affected the quality of the brines and the waters in the area. Different sample media such as well-water, pond water, brine spring pool water, stream water, stream sediments etc. were analysed. Geochemical results show that Cu, Zn, Pb, As and S are concentrated in the waters (0.3, 0.36, 0.05, 0.07 and 1 1,5 ppm respectively). These elements are more concentrated in both the spring and pond waters, suggesting that the spring water could have acted as the transport medium for these elements released from deep-seated sources. Transitions elements (Ti, V, Cr, Fe, Co, Ni and Sr) are concentrated in the waters. Compared to the World Health Organization (WHO) admissible limits, the well waters present very high concentrations in Cd (0.56 ppm) and Sb (0.40 ppm) (200x and 70x WHO admissible values respectively). There is a preferential concentration of transition elements (Ti, V, Fe, Co and Ni) in the sediments (41.38, 362, 52.21, 269 and 54 ppm respectively) than in the waters (0.70, 0.05, 5.6, 0.04 and 0.02 ppm respectively). Similarly, Cu, Zn, Pb and As are concentrated in the sediments (44, 72, 41 and 14 ppm respectively). The concentrations of transition elements (Ti, V, Cr, Fe, Co and Ni) in the refined salt were highly elevated (784, 363, 283, 105, 59.2 and 42.6 ppm respectively) (7000-10,000x well water). Similarly, the concentrations of As, Pb, Br and Sr in the refined salt were also alarming (11.6, 16.4, 16.4 and 122 ppm respectively), (1000, 700, 3000 and 20,000x well water values respectively). S on the other hand is absent. One of the striking features is the absence of I, Cd, Sb and Se in the refined salt crystals which were detected in the waters and the brines. Compared to WHO admissible values, the refined salt crystal concentrations for Ni (426 ppm) and Cr (283 ppm) were also very high (2000x WHO values respectively) and to a lesser extent Cu (26.9 ppm) and Zn (21.7 ppm) (12 and 7x WHO values respectively).
机译:进行了对中贝努埃海槽Keana盐水田中各种样品的微量元素研究,以确定Pb-Zn-S和BaSO_4矿化对该地区盐水和水质的影响程度。分析了不同的样品介质,例如井水,池塘水,盐水泉池水,溪流水,溪流沉积物等。地球化学结果表明,铜,锌,铅,砷和硫集中在水中(分别为0.3、0.36、0.05、0.07和1 1.5 ppm)。这些元素更多地集中在泉水和池塘水中,这表明泉水可能充当了从深源释放的这些元素的运输媒介。过渡元素(Ti,V,Cr,Fe,Co,Ni和Sr)集中在水中。与世界卫生组织(WHO)的容许限值相比,井水的Cd(0.56 ppm)和Sb(0.40 ppm)浓度很高(分别为WHO容许值的200x和70x)。沉积物中的过渡元素(Ti,V,Fe,Co和Ni)的优先浓度(分别为41.38、362、52.21、269和54 ppm)比水域(0.70、0.05、5.6、0.04和0.02 ppm)优先分别)。同样,铜,锌,铅和砷也集中在沉积物中(分别为44、72、41和14 ppm)。精制盐中的过渡元素(Ti,V,Cr,Fe,Co和Ni)的浓度高度升高(分别为784、363、283、105、59.2和42.6 ppm)(7000-10,000x井水)。同样,精制盐中的As,Pb,Br和Sr的浓度也令人震惊(分别为11.6、16.4、16.4和122 ppm)(分别为1000、700、3000和20,000x井水值)。另一方面,S不存在。显着特征之一是在水和盐水中检测到的精制盐晶体中不含I,Cd,Sb和Se。与WHO允许值相比,Ni(426 ppm)和Cr(283 ppm)的精制盐晶体浓度也很高(分别为2000x WHO值),而Cu(26.9 ppm)和Zn(21.7 ppm)的程度较小(分别是12和7倍的WHO值)。

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