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Evaluation of Aquifer Potentials for IrrigationPractice in Parts of the Basement Complex ofNorth-Central Nigeria

机译:尼日利亚中北部地下室综合体部分地区灌溉实践的含水层潜力评估

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A Geoelectric survey involving Vertical Electrical Sounding was carried out with the aim of using the results to delineate aquifer and assess its sustenance for adequate water supply for irrigation work in Fadama parts of some villages in Igabi Local Government Area, Kaduna state, Nigeria. The data were acquired with symmetric Schlumberger configuration at stations chosen across the study area. The acquired data were inverted with 1D Earth Imager iterative software. The interpreted results suggest four geoelectric layers. From their equivalent geologic/lithologic units, the weathered and the underlain fractured basement, which are characterized with relatively low resistivity values (14 to 217a?|m), were considered as the aquiferous layers of the study area. Suitable sites for construction of pump-fitted wells were suggested based on thickness of the aquiferous layers. On assessment of the groundwater from estimated aquifer parameters, the well yield will serve the intended irrigation purpose.
机译:进行了一次涉及垂直电测深的地电调查,目的是用结果描绘出含水层,并评估其在尼日利亚卡杜纳州伊加比地方政府地区一些村庄的Fadama地区的灌溉工作所需的充足供水。数据是在研究区域内选定的站点通过对称斯伦贝谢配置获取的。使用1D Earth Imager迭代软件反转获取的数据。解释结果表明有四个地电层。从它们等效的地质/岩性单位来看,被认为具有相对较低的电阻率值(14至217a?| m)的风化和地下裂隙基底被认为是研究区域的含水层。根据含水层的厚度,建议建造合适的泵井位置。根据估计的含水层参数评估地下水后,井的产量将达到预期的灌溉目的。

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