首页> 外文期刊>Journal of earth system science >Application of multi-criteria decision making (MCDM) and electrical resistivity tomography (ERT) techniques for identification of groundwater recharge zone(s) in granitic hard rock aquifer
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Application of multi-criteria decision making (MCDM) and electrical resistivity tomography (ERT) techniques for identification of groundwater recharge zone(s) in granitic hard rock aquifer

机译:多标准决策(MCDM)和电阻率断层扫描(ERT)技术在花岗岩硬岩含水层地下水补给区识别技术中的应用

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Groundwater recharge is a hydrological process where water flows from sub-surface layers to the water table of the aquifer and is the backbone of the hydrogeological system. The present study is carried out in a granitic hard rock aquifer region within and surroundings of the CSIR-NGRI campus, Hyderabad. The aim of this study to identify the potential groundwater recharge zone(s) using GIS based multi-criteria decision making (MCDM) along with sub-surface mapping from Electrical Resistivity Tomography (ERT) technique. The assigned weight of the different thematic layers of surface and sub-surface parameters and their specific characteristics was determined based on their relative contribution to the groundwater recharge and thus the normalized weight was computed using MCDM technique. These thematic layers were integrated with the help of ArcGIS to accurately identify the recharge zones within the study region. The resulting recharge map has been categorized into five classes viz., very poor, poor, moderate, good and very good. Numerically 23.11% of the study area is in a moderate zone of recharge, 4.97% in good and very good zone, while 71.92% falls under the poor and very poor zone, i.e., unsuitable for groundwater recharge. The recharge zone map of the study area is found to be in agreement with 2D inverted resistivity models for two different time periods, which revealed distinct geological features and thus identified the near surface recharge property, where recharge zone resistivity values lie between ${sim}$20 and 70 $Omega$.m up to 11 m depth. Thus, the integrated results from the present study delineated groundwater recharge zone(s) for sustainable groundwater resources in the granitic hard rock system.
机译:地下水补给是一种水文过程,其中水从亚表面层流到含水层的水位,是水文地质系统的骨干。本研究在CSIR-NGRI校园内的花岗岩硬岩含水层区域和周围的Hyderabad进行。本研究的目的是使用基于GIS的多标准决策(MCDM)以及电阻率断层扫描(ERT)技术的子表面映射来识别潜在地下水充电区域。基于它们对地下水补给的相对贡献确定了表面和子表面参数的不同专题层的分配重量,并使用MCDM技术计算归一化重量。这些主题层借助ArcGIS集成,以准确地识别研究区域内的充电区。得到的充值地图已被分为五类张,非常差,差,差,温和,好,非常好。数值23.11%的研究区域位于适度的充电区域,良好且非常好的区域4.97%,而71.92%落在穷人和非常差的区域下,即不适合地下水充电。发现研究区域的充电区地图与两个不同的时间段的2D倒置电阻率模型一致,这揭示了不同的地质特征,从而确定了近表面充电性质,其中补给区域电阻率值在$ { SIM } $ 20和70 $ omega $ .m最多11米。因此,本研究中的综合结果划定了花岗岩硬岩系统中可持续地下水资源的地下水补给区域。

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