Institute of Geology, University of the Punjab, Lahore, 54590, Pakistan.
Geological Survey of Pakistan, Lahore, Pakistan.
Environ Monit Assess. 2023 Nov 9;195(12):1435. doi: 10.1007/s10661-023-12049-0.
In the central part of Bari Doab in Punjab Province of Pakistan, the factors such as sporadic rainfall pattern, decrement of water in rivers, subsurface salinity and excessive mining of groundwater have badly affected the hydrogeology and recharge system of aquifer. The present research work is an endeavour to evaluate the characteristics and potential of aquifer for its future sustainable availability within the study area of central part of Bari Doab. The geophysical studies, pumping tests data, borehole logs and Dar-Zarrouk parameters were used integrally to evaluate the aquifer hydraulic and hydrologic parameters in the study area. VES technique of geophysical investigations using Schlumberger electrodes configuration was carried out at sparsely distributed 435 locations. Litho-logs and VES results altogether decipher that the subsurface alluvial succession is primarily composed of intermixed layers of sand, gravel, clay, silt and some kankar inclusions. The VES data allied with pumping test analysis of test wells in the study area were used to evaluate the aquifer hydraulic properties. Comparatively low values of discharge rate, hydraulic conductivity and transmissivity were evaluated in two wells whilst relatively higher values of these parameters were evaluated in rest of six wells. The results of hydrologic parameters also confirm the results of hydraulic parameters in the wells. Finally, the Dar-Zarrouk parameters were used for the estimation of hydraulic parameters for whole study area and the aquifer zones of relatively high and low potential were delineated.
在巴基斯坦旁遮普省的 Bari Doab 中心地带,降雨模式零星、河流水量减少、地下盐分和过度开采地下水等因素严重影响了含水层的水文地质和补给系统。本研究工作旨在评估含水层的特征和潜力,以确保在 Bari Doab 中心地带的研究区域内未来的可持续利用。综合利用地球物理研究、抽水试验数据、钻孔日志和 Dar-Zarrouk 参数来评估研究区域内的含水层水力和水文参数。在 435 个稀疏分布的地点进行了地球物理调查的 VES 技术,使用 Schlumberger 电极配置。岩心日志和 VES 结果共同揭示,地下冲积层主要由砂、砾石、粘土、粉砂和一些钙质结核混合层组成。将研究区域内测试井的 VES 数据与抽水试验分析相结合,用于评估含水层的水力特性。两口井的排水量、水力传导率和导水率值较低,而其余六口井的这些参数值较高。水文参数的结果也证实了井中水力参数的结果。最后,使用 Dar-Zarrouk 参数来估算整个研究区域和高潜力和低潜力含水层区的水力参数。