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首页> 外文期刊>Environmental Science and Pollution Research >Occurrence and distribution of selected heavy metals and boron in groundwater of the Gulf of Khambhat region, Gujarat, India
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Occurrence and distribution of selected heavy metals and boron in groundwater of the Gulf of Khambhat region, Gujarat, India

机译:印度古吉拉特邦甘拜特海湾地区地下水中某些重金属和硼的赋存与分布

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摘要

The concentration of selected heavy metals, like As, Co, Cr, Cu, Fe, Mn, Ni, Pb, and Zn as well as B, was measured by inductively coupled plasma-optical emission spectrometry (ICP-OES) in groundwater samples from vari ous locations in the Gulf of Khambhat (GoK), an inlet of the Arabian Sea in the state of Gujarat, India, during post-monsoon, winter, and pre-monsoon seasons in a year. Most heavy elements are characterized by low mobility under slightly alkaline and reducing conditions; concentrations in confined aquifers are smaller than the maximum permissible values for drinking water. The temporal changes indicate that a majority of metals is entering the aquifer during monsoon. Principle component analysis of the heavy metal data suggests that Co, Cu, Cd, and Zn are interrelated with each other and derived significantly from anthropogenic route, while input of Pb and Cr may be due to atmospheric deposition in the study area. Both weathering of rocks and anthropogenic input were found to be main sources of elements in the groundwater. The heavy metal levels in groundwaters of the GoK region in comparison with some of the European and Asian sites were higher; however, these metal levels were found to be compa rable with few urban sites in the world.
机译:通过电感耦合等离子体发射光谱法(ICP-OES)测量了来自地下水的样品中选定的重金属(如As,Co,Cr,Cu,Fe,Mn,Ni,Pb和Zn以及B)的浓度。一年中的季风后,冬季和季风前季节,印度印度古吉拉特邦阿拉伯海的入口坎布哈特湾(GoK)的位置各不相同。大多数重元素的特征是在弱碱性和还原条件下的迁移率较低;密闭含水层中的浓度小于饮用水的最大允许值。时间变化表明季风期间大多数金属进入含水层。重金属数据的主成分分析表明,Co,Cu,Cd和Zn相互关联,并且显着来源于人为途径,而Pb和Cr的输入可能是由于研究区域的大气沉积所致。岩石的风化和人为的投入都是地下水中元素的主要来源。与欧洲和亚洲一些地区相比,GoK地区地下水中的重金属含量更高;但是,发现这些金属水平与世界上很少的城市站点具有可比性。

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