Khan Ali Yousaf, Ullah Waheed, Niaz Abrar, Bibi Tehmina, Imtiaz Muhammad Mubashar, Fiaz Rashida, Gul Shehla, Hameed Kiran, Islam Fakhrul
Institute of Geology, University of Azad Jammu and Kashmir, Muzaffarabad, Pakistan.
Rabdan Academy, Abu Dhabi, 114646, UAE.
Sci Rep. 2024 Oct 26;14(1):25514. doi: 10.1038/s41598-024-76262-8.
An integrated approach using geophysical and geospatial techniques was employed to model the surface and subsurface water-bearing strata and assess aquifer vulnerability in the Sehnsa town, Kotli district, State of Azad Kashmir, Pakistan. The inadequate scientific studies in the hilly terrain with such complex geological conditions has led to the failure of the boreholes for groundwater extraction. For the evaluation of groundwater potential and subsurface lithology, 30 vertical electrical soundings (VES) stations utilizing the Schlumberger electrode configuration were completed, modeled and analyzed spatially. Numerous geoelectrical parameters like true resistivity, thickness of subsurface layers and Dar-Zarrouk parameters were evaluated. The subsurface lithology delineated comprised topsoil, clayey sand, sandstone, and boulder clays which closely resemble to the borehole lithologs available in the study area. The inversion model confirms the presence of patches of high-resistivity sandstone in the southwestern part of the study area with the maximum thickness of the aquifer up to 140 m. Most aquifers were classified as unconfined with Q-type resistivity curves. The protective overburden capacity of the aquifers is rated as poor at VES 1, 3-5, 8, 10-16, 18, 19, 22-25, 27 and 30 whereas the moderate category was found at VES 2, 9 and 20 and excellent at VES 7 and 28, respectively. Therefore, the VES stations with poor and moderate ratings of overburden protective capacity are vulnerable for surface contaminants. The aquifer recharge was associated with rainfall and partly from the Poonch River. The effective integration of geophysical and geospatial techniques in this study provides sufficient information about the regional water resources and gives a preliminary model that can facilitate efficient water resource management in the area. These approaches can be successfully applied to diverse geographical and hydrogeological sites due to their versatility and reliability.
采用地球物理和地理空间技术的综合方法,对巴基斯坦阿扎德克什米尔邦科特利区塞恩萨镇的地表水和地下含水层进行建模,并评估含水层脆弱性。在这种地质条件复杂的山区,科学研究不足导致了用于抽取地下水的钻孔失败。为了评估地下水潜力和地下岩性,利用施伦贝格尔电极配置完成了30个垂直电测深(VES)站的测量,并进行了空间建模和分析。评估了许多地电参数,如实电阻率、地下层厚度和达尔-扎鲁克参数。所划分的地下岩性包括表土、黏质砂土、砂岩和漂积黏土,与研究区域现有的钻孔岩性记录非常相似。反演模型证实,研究区域西南部存在高电阻率砂岩斑块,含水层最大厚度达140米。大多数含水层被归类为无压含水层,具有Q型电阻率曲线。在VES 1、3 - 5、8、10 - 16、18、19、22 - 25、27和30处,含水层的保护覆盖层能力被评为较差;而在VES 2、9和20处为中等,在VES 7和28处分别为优秀。因此,保护覆盖层能力评级为差和中等的VES站容易受到地表污染物的影响。含水层补给与降雨有关,部分来自蓬奇河。本研究中地球物理和地理空间技术的有效整合提供了有关区域水资源的充分信息,并给出了一个初步模型,可促进该地区的高效水资源管理。由于其通用性和可靠性,这些方法可成功应用于不同的地理和水文地质场地。