首页> 外文期刊>International Journal of Economic and Environment Geology >Demarcation of Groundwater Potential Zones by Electrical Resistivity Survey (ERS) Islamabad, Pakistan
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Demarcation of Groundwater Potential Zones by Electrical Resistivity Survey (ERS) Islamabad, Pakistan

机译:通过巴基斯坦伊斯兰堡的电阻率调查(ERS)划分地下水潜在区域

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A newly developed D-12 housing sector is at the Margalla foot-hills in Islamabad. This housing sector is facing tremendous groundwater problem due to frequent dry boreholes. After conducting the reconnaissance survey, data from the already drilled wells were recorded at different points throughout the study area for measuring average water table and the average total depth. The electrical resistivity survey was conducted in the sector for exploration of groundwater at six different locations with the help of SAS 4000 Terameter using Schlumberger configuration. The acquired data were used to determine the true resistivity on the basis of standard curves. The curves were matched with the borehole data and the surface geological map to prepare lithologic columns based on the true resistivities. Two zones have been categorized for future domestic use, i.e. prospective and non-prospective. The study shows dependence of localization of the aquifers upon the fault-related folding of the area. The aquifers are of two types i.e. shallow unconfined and deeper confined. The unconfined aquifers are found in the alluvium, whereas the confined aquifers are found in the sands of the Murree Formation. The confining beds constitute Murree clays and the shales.
机译:伊斯兰堡的Margalla山麓有一个新开发的D-12住房部门。由于频繁的干燥钻孔,该房屋部门面临着巨大的地下水问题。进行勘测之后,在整个研究区域的不同点记录来自已钻井的数据,以测量平均地下水位和平均总深度。电阻率调查是在使用Schlumberger配置的SAS 4000 Terameter的帮助下在六个不同位置进行地下水勘探的。采集的数据用于根据标准曲线确定真实电阻率。将曲线与井眼数据和地表地质图进行匹配,以基于真实电阻率制备岩性柱。为了将来的家庭使用,已经将两个区域分类,即预期的和非预期的。研究表明,含水层的局部性取决于该区域与断层有关的褶皱。含水层有两种类型,即浅无限制和深封闭。在冲积层中发现了无侧限含水层,而在Murree组的砂中发现了无侧限含水层。约束层由Murree粘土和页岩组成。

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