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首页> 外文期刊>International Journal of Geosciences >Integrated Landsat Imagery and Geophysical Exploration for Groundwater Potential Evaluation of Okene and Its Environs, Southwestern Nigeria
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Integrated Landsat Imagery and Geophysical Exploration for Groundwater Potential Evaluation of Okene and Its Environs, Southwestern Nigeria

机译:尼日利亚西南部Okene及其周围地区地下水潜力的综合Landsat影像和地球物理勘探

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摘要

In this study, an integrated remote sensing and geophysical (aeromagnetic and geo-electric) methods was employed to assess the potential of groundwater in a basement complex terrain of Okene and its environs, Southwestern, Nigeria. Landsat imagery acquired over the study area was processed in the Geographic Information Systems (GIS) environment to delineate the surface lineaments, drainage networks and their orientations. Aeromagnetic data over the area were analyzed and its derivative maps were interpreted to further map the structures and the geology in the subsurface; depths to magnetic sources were determined using spectral analysis. Vertical Electrical Sounding (VES) of geo-electric method was interpreted to map the subsurface geology layers. The results of the integrated data were correlated with borehole yield data of the area for effective interpretation. Delineated lineaments from the azimuth, frequency plot showed dominant trends in the NE-SW and NNE-SSW directions. Radial average power spectrum revealed the depth to magnetic sources between 100 and 2500 m and the interpreted VES data characterized the area into three to four subsurface layers. In correlating the results with borehole yield data, the zones with high lineament density and lowegative magnetic anomaly were categorized as high groundwater potential zones while areas with low lineament density and high/positive magnetic anomaly as low groundwater potential zones. This study will guide efficiently subsequent groundwater drilling program in the study area.
机译:在这项研究中,采用了一种综合的遥感和地球物理(航空磁和地球电)方法来评估尼日利亚西南部的奥肯及其周围地区地下复杂地形中的地下水潜力。在地理信息系统(GIS)环境中处理了在研究区域内获取的Landsat影像,以描绘出地表轮廓,排水网络及其方向。分析了该地区的航空磁数据,并解释了其导数图,以进一步绘制地下的结构和地质图。使用频谱分析确定到磁源的深度。解释了地电方法的垂直电测深(VES)来绘制地下地质层的图。综合数据的结果与该地区的钻孔产量数据相关联,以进行有效解释。从方位角,频率图上划定的线条显示出NE-SW和NNE-SSW方向的主要趋势。径向平均功率谱揭示了在100至2500 m之间的磁源深度,解释的VES数据将区域划分为3至4个地下层。在将结果与井眼产量数据进行关联时,将具有高线面密度和低/负磁异常的区域分类为高地下水位区域,而将具有低线面密度和高/正磁异常的区域分类为低地下水位区域。这项研究将有效地指导研究区域的后续地下水钻探计划。

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