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Evaluation of the aquifer characteristic of Nanka Sands using hydrogeological method in combination with Vertical Electrical Sounding (VES)

机译:水文地质方法结合垂直电测深(VES)评价南卡砂岩含水层特征

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In this study, we have coupled surface geophysical method with pumping test results to provide a cost effective and efficient alternative in aquifer parameter estimation. Vertical Electrical Sounding (VES) was carried out at 40 sites in the study area for the identification of the vertical variation in subsurface lithology and for the characterization of the aquifer system of the study area. The interpretation of the VES data revealed 3 to 5 geoelectric units with the depth to aquifer varying from 7 to 108m and the resistivity of the saturated layer varying between 42.9 and 8829 ohm-m. Using the geoelectric data, aquifer depth, hydraulic head and aquifer resistivity maps were prepare using appropriate software. Aquifer characteristics in the form of transmissivity and hydraulic conductivity calculated from interpreted VES results varied from 0.48 to 19.50m2/day and 0.06 to 3.75m/day respectively. This coupling has proved useful and most valuable in areas of scarce data such as the study area. @ JASEM
机译:在这项研究中,我们将地面地球物理方法与抽水试验结果相结合,为含水层参数估算提供了一种经济高效的选择。在研究区域的40个地点进行了垂直电测深(VES),以识别地下岩性的垂直变化并表征研究区域的含水层系统。对VES数据的解释揭示了3到5个地电单元,含水层的深度在7到108m之间变化,饱和层的电阻率在42.9到8829 ohm-m之间变化。利用地电数据,使用适当的软件准备了含水层深度,水头和含水层电阻率图。根据解释的VES结果计算出的透过率和水力传导率形式的含水层特征分别在0.48至19.50m2 /天和0.06至3.75m /天之间变化。事实证明,这种耦合在诸如研究领域之类的稀缺数据领域很有用,并且最有价值。 @ JASEM

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