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Integrated hydrogeophysical assessment of groundwater potential in the Ogun drainage basin, Nigeria

机译:尼日利亚的Ogun排水盆地的地下水潜力的综合水域评估

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This study explores possible groundwater areas in the Ogun drainage basin in Ogun State, Nigeria, using the Vertical Electrical Sounding VES system for remote sensing and GIS. Thematic maps are built as geodatabase or GIS layers of lineament density, lithology, land use and land cover, drainage and slopes. Each layer is given weights based on a pair comparison of considerable factors in the retention, storage and transmission of groundwater. Potentials are created through the analysis process hierarchy (AHP) in a GIS environment that includes five thematic maps with factors that result in groundwater occurrence and movement using weighted overlay. We assigned weightages of factors influencing groundwater prospects such that lithology had the highest (43%) followed by lineament density (33%). Slope weighed (13%) and drainage density (7%). The least groundwater contributor in the study area, {is the} land use/land cover was assigned 4%. The AHP consistency ratio CR was calculated to be 0.04 for this analysis which is less than the threshold consistency value of 0.10. The result of the study showed that high groundwater potential occupies 3818.57km~2 (21%) and low potential areas constitute 1022.50 km2 (6%) of the study area including. The moderate and very low potentials occupy the highest coverage constitute about 5530.63 km2 (31%) and 7725.37 km2 (42%) respectively. Validation of the aquifers from the VES shows that the GIS analysis map for groundwater potential corresponds to field results. However, it is suggested to add more detailed VES data, well data/ pumping tests into the GPZ map for accurate validation.
机译:这项研究使用用于遥感和GIS的垂直电气发声VES系统探索了尼日利亚Ogun State的Ogun排水盆地的可能地下水区域。主题地图是作为谱系密度,岩性,土地使用和土地覆盖,排水和斜坡的地理图或GIS层建造的。根据对地下水的保留,存储和传播中相当多的因素的比较,给出了每一层的权重。电势是通过GIS环境中的分析过程层次结构(AHP)创建的,该过程包括五个主题图,其因素带有导致地下水发生和使用加权覆盖的运动。我们分配了影响地下水前景的因素的重量,以便岩性最高(43%),其次是谱系密度(33%)。坡度称重(13%)和排水密度(7%)。在研究区域中的地下水最少的贡献者,{是}土地使用/土地覆盖率分配了4%。对于此分析,AHP一致性比率为0.04,小于阈值一致性值为0.10。该研究的结果表明,高地下水潜力占3818.57公里〜2(21%),低潜力区域占研究区域的1022.50 km2(6%)。中等和非常低的电势占最高覆盖范围,分别构成约5530.63 km2(31%)和7725.37 km2(42%)。 VES对含水层的验证表明,地下水电位的GIS分析图对应于现场结果。但是,建议将更详细的VES数据,井数据/泵送测试添加到GPZ地图中,以进行准确的验证。

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