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Trace Element Geochemistry of Groundwater ofWinder, Balochistan, Pakistan and its Appraisalfor Irrigation Water Quality

机译:巴基斯坦Bal路支省Winder地下水中的微量元素地球化学及其对灌溉水质量的评价

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Aims: The study is aimed to evaluate the concentration of trace elements and irrigation quality of the groundwater of Winder, Balochistan, Pakistan.Study Design: The ophiolitic rocks of the study area upon weathering, contributed a large amount of certain trace elements to the groundwater. Samples of groundwater were collected and analyzed for trace elements.Place and Duration of Study: The study area lays in the southern extremity of 450km long Bela Ophiolite, Balochistan, Pakistan. The work was carried out during 2011-2012.Methodology: Sample collection and estimation of physical properties and chemical composition of water were carried out using standard procedures. The concentrations of trace elements were estimated by using Atomic Absorption Spectrophotometer.Results: The trace elements concentration in the groundwater were found in the range of 8-800 for Zn, 14-107 for Cu, 13-103 for Cr, 32-1814 for Fe, 15-102 for Mn, 01-430 for Ni, 01-28 for Co, 16-139 for Pb and 1-30mg/kg for Cd.Conclusion: The present study revealed Fe>Ni>Zn>Pb>Cu>Cr>Mn>Cd>Co trend of abundance. Bivariate and ternary plots suggested alliance with the nearby exposed rocks. The statistical analysis of the trace elements data in form of correlation matrix and principal component analysis (PCA), further verify dissolution of trace elements from ophiolitic and sedimentary rocks.The concentration of trace elements of the groundwater is discussed in relation to biological function in the plants and found within the safe range as compared to the permissible limit for irrigation purpose.
机译:目的:本研究旨在评估巴基斯坦Bal路支斯坦温德(Winder)地下水中微量元素的浓度和灌溉质量。研究设计:风化研究区域的脂石质岩石对地下水贡献了大量的某些微量元素。研究地点和持续时间:研究区域位于巴基斯坦Bal路支斯坦长450公里的Bela蛇绿岩的南端。该工作于2011年至2012年进行。方法:采用标准程序进行样品收集以及水的物理性质和化学组成的估算。结果:用原子吸收分光光度计估算了微量元素的浓度。结果:地下水中微量元素的浓度范围为:锌为8-800,铜为14-107,铬为13-103,铬为32-1814。 Fe,Mn 15-102,Ni 01-430,Co 01-28,Pb 16-139,Cd 1-30mg / kg。结论:本研究表明Fe> Ni> Zn> Pb> Cu> Cr> Mn> Cd> Co的富集趋势。二元和三元图表明与附近裸露的岩石结盟。以相关矩阵和主成分分析(PCA)的形式对微量元素数据进行统计分析,进一步验证了微量元素在脂滑石和沉积岩中的溶解。讨论了地下水中微量元素的浓度与生物功能的关系。并在与灌溉目的允许的限制相比的安全范围内找到植物。

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