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A study of physico-chemical properties of groundwater in a coastal aquifer sandwiched between marine and brackish water bodies

机译:沿海含水层的地下水的物理化学性质研究夹在海水和咸水体系之间

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The present study was carried out to understand the quality of groundwater and to delineate the subsurface formations in an area of 30 km~2 situated between backwater Vembanad Lake on the eastern side and Arabian Sea on the western side. The physico chemical studies involve pH, conductivity, total hardness, cations (Ca,Mg,Na,K), anions (HCO_3, Cl, PO_4, SO_4) and Fe. Wells in this area are shallow with 2 to 4 m depth and the water table in these wells varies from 1.5 to 2 m. Industrial pollutants and sewages do not influence the wells in the area and are very well protected from seepage by proper lining inside the wells. Samples collected from 12 open wells were used for the study. The physico chemical properties of the samples were compared between the eastern side (the brackish water side) and the western side (marine side). The above properties were further compared with the drinking water standards set up by the World Health Organization. To delineate the subsurface formations electrical resistivity soundings were carried out at an interval of 3 km. in the study area.
机译:本研究进行了解地下水的质量,并在西部的东侧和阿拉伯海的后水vembanad湖之间划分了30公里〜2的地下地层。物理化学研究涉及pH,导电性,总硬度,阳离子(Ca,Mg,Na,K),阴离子(HCO_3,Cl,Po_4,SO_4)和Fe。该区域的井浅,深度为2至4米,这些井中的水桌子从1.5到2米变化。工业污染物和污水不会影响该地区的井,并且通过井内的适当衬里,从渗出方面非常受到良好的保护。从12个开放井收集的样品用于研究。在东侧(咸水侧)和西侧(海面)之间比较样品的物理化学性质。与世界卫生组织建立的饮用水标准相比,上述性质进一步。为了描绘地下地层,电阻率探测以3km的间隔进行。在研究区。

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