Groundwater Potential Zone Mapping of Ondo State Using Multi-criteria Technique and Hydrogeophysics

Epuh Ee, Joshua Eo, Elesho Ao, Orji Mj, Damilola Om, Adetoro Pt
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引用次数: 4

Abstract

The delineation of groundwater potential zones in Ondo State was carried out using Remote Sensing, Geographic Information Systems (GIS) and Hydrogeophysics. In this study, various thematic maps such as: soil map, slope, drainage map, land use/Land cover map, geological map, rainfall map, lineaments map were obtained from enhanced satellite imagery. These maps were overlaid in terms of weighed overlay method using Spatial Analysis tool in Arc GIS 10.5. During weighed overlay analysis, different ranks were given to each individual parameter of each thematic map and weights were assigned according to their influence. Results showed that spatial distribution of the most promising sites for groundwater exploration was dependent on the interrelated factors of lithology, topography and geologic structure. The groundwater potential map obtained from the study area showed that 17.5% of the total study area lie within the “very high” potential zone, 12.0% of the area falls within the “high”, 39.5% lies within the “moderate” zone, 25.7% lies within the “low “potential zone while 5.3% lies within the very low potential zone. The very high potential areas lie within the sedimentary zone in the southern part of the study area with high alluvial deposits, while the “very low” prospect zone lies majorly within the basement complex zone in the northern part of the study area. The query results on Ijapo Vertical electric sounding (VES) data analysis shows the presence of four lithology: top soil, sand (which contains the fresh water), sand clay (which contains the brackish water) and the clay (which contains the saline water). The boreholes susceptible to salt water intrusion were identified and the best drilling point with respect to depth were also determined.
基于多准则技术和水文地球物理的Ondo州地下水潜力带填图
利用遥感、地理信息系统(GIS)和水文地球物理学对Ondo州地下水潜力区进行了圈定。本研究利用增强卫星影像获取土壤图、坡度图、水系图、土地利用/土地覆被图、地质图、雨量图、地貌图等专题地图。使用Arc GIS 10.5中的空间分析工具,按加权叠加法对这些地图进行叠加。在加权叠加分析中,对每个专题图的各个参数赋予不同的等级,并根据其影响程度分配权重。结果表明,地下水勘探潜力点的空间分布受岩性、地形和地质构造等因素的影响。研究区地下水电位分布图显示,研究区17.5%的区域处于“极高”电位区,12.0%的区域处于“高”电位区,39.5%的区域处于“中等”电位区,25.7%的区域处于“低”电位区,5.3%的区域处于“极低”电位区。极低远景区主要位于研究区北部基底杂岩带内,极低远景区主要位于研究区南部高冲积层沉积带内。对Ijapo垂直电测深(VES)数据分析的查询结果显示,存在4种岩性:表层土、砂(含淡水)、砂粘土(含微咸水)和粘土(含盐水)。确定了易受盐水侵入的钻孔,确定了相对于深度的最佳钻孔点。
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