Saudi Geological Survey, Jeddah, Saudi Arabia.
Geography and GIS Department, Faculty of Arts and Humanities, King Abdulaziz University, Jeddah, Saudi Arabia.
Ground Water. 2019 Nov;57(6):940-950. doi: 10.1111/gwat.12870. Epub 2019 Mar 18.
In arid and hyper-arid zones, groundwater exploration is one of the most significant ways to locate potential new water supplies. Geophysical prospecting is currently the most successfully used method for locating new supplies, but it is rather costly. Satellite remote sensing (RS) detection, however, with its integration of Geographic Information Systems (GIS) provides the best chance for identifying and initially evaluating water-bearing formations. In the western part of Saudi Arabia, Wadi Na'man has for centuries been one of the major water sources for the city of Makkah Al-Mukarramah. It is therefore very important to find appropriate groundwater potential (GP) zones in this wadi for water supply. This study utilizes RS and GIS techniques, and also studies the hydrogeological, geological, and geomorphological characteristics that have significant impact on groundwater occurrence in Wadi Na'man. Representative layers are generated for each component and each given a weight ratio that depends on the level of influence. The overlay and integration of these thematic layers was used to produce a map that shows the most promising potential groundwater areas and classifies local potentials as either low, medium, or high. The results also reveal that the areas overall-rated as "promising" (i.e., classified as medium or high) represent approximately 17-25% of the total basin area and consist mainly of Quaternary sediments and connected fractured rock areas.
在干旱和极干旱地区,地下水勘探是寻找潜在新水源的最重要方法之一。地球物理勘探是目前定位新水源最成功的方法,但成本相当高。然而,卫星遥感(RS)探测与地理信息系统(GIS)的结合为识别和初步评估含水地层提供了最佳机会。在沙特阿拉伯西部,瓦迪纳曼(Wadi Na'man)几个世纪以来一直是麦加市(Makkah Al-Mukarramah)的主要水源之一。因此,在这条河谷中寻找合适的地下水潜力(GP)区对于供水非常重要。本研究利用 RS 和 GIS 技术,研究了对地下水赋存有重大影响的水文地质、地质和地貌特征。为每个组件生成代表性层,并为每个组件分配一个权重比,该权重比取决于影响程度。对这些专题层进行叠加和集成,生成一张地图,显示最有希望的潜在地下水区域,并将局部潜力分为低、中、高三种类型。结果还表明,总体评价为“有希望”(即中等或高)的区域约占总流域面积的 17-25%,主要由第四纪沉积物和连通的断裂岩石区组成。