Joel Emmanuel S, Olasehinde Peter I, Adagunodo Theophilus A, Omeje Maxwell, Oha Ifeanyi, Akinyemi Marvel L, Olawole Olukunle C
Department of Physics, Covenant University, Ota, Nigeria.
Department of Geophysics, University of Ilorin, Ilorin, Nigeria.
Heliyon. 2020 Jan 31;6(1):e03327. doi: 10.1016/j.heliyon.2020.e03327. eCollection 2020 Jan.
Groundwater is a vital natural resource that plays a significant function in sustainability of living things on earth. Its exploration requires special skill for optimum exploitation. Shuttle Radar Topography Mission (SRTM)and Vertical Electrical Sounding (VES) were used to detectthe stratigraphy and subsurface structures controlling the groundwater system around Iju - Ota, Ogun State, Southwestern Nigeria. Nineteen (19) VES points were carried out where there were dense concentrations of lineaments and interconnected to establish the connection of the observed lineaments with groundwater occurrence in the study area using Schlumberger array, with electrode spacing of AB/2 varying from 180 to 320 m. The analysis of SRTM data revealedthe dominating structural NE-SW and NW-SE trends, which control aquifer structure. The geoelectrical parameters from the VES results were used to map the stratigraphic sequences in the study area. Six (6) units that comprisethe topsoil, lateritic clay, clayey sand, mudstone, sand (main aquifer), and shale or clay were identified in the study area. The aquiferous unit around Iju - Ota axis ranged from 30 to 80 m. Theextracted from the hill shaded SRTM data and the result of VES revealed that the thickness of the aquifer is as a result of interconnectivity of the lineaments observed in the SRTM data suggesting that the groundwater occurrence in the study area is chiefly controlled by these fractures.
地下水是一种至关重要的自然资源,对地球上生物的可持续发展起着重要作用。对其进行勘探需要特殊技能以实现最优开采。利用航天飞机雷达地形测绘任务(SRTM)和垂向电测深(VES)来探测控制尼日利亚西南部奥贡州伊朱-奥塔周围地下水系统的地层和地下结构。在节理密集且相互连通的地方进行了19个VES点的测量,使用施伦贝格阵列建立观测节理与研究区域地下水赋存情况的联系,电极间距AB/2从180米到320米不等。对SRTM数据的分析揭示了控制含水层结构的主要NE-SW和NW-SE构造趋势。利用VES结果的地电参数绘制了研究区域的地层序列图。在研究区域确定了六个单元,包括表土、红土粘土、粘土质砂、泥岩、砂(主要含水层)以及页岩或粘土。伊朱-奥塔轴周围的含水层单元厚度在30至80米之间。从SRTM山体阴影数据中提取的信息以及VES结果表明,含水层的厚度是由于SRTM数据中观测到的节理相互连通所致,这表明研究区域的地下水赋存主要受这些裂缝控制。