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Application of Surface Geophysics to Groundwater Investigations: A Case Study of Rural Area in Ilorin, Northcentral Nigeria.

机译:地面地球物理学在地下水调查中的应用 - 以伊洛林,尼日利亚州伊洛林农村案例研究。

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This study was carried out to determine groundwater potential in Ilorin, Northcentral Nigeria using Vertical Electrical Sounding (VES). The VES data was generated from twenty (20) locations in the study area and was later processed and analyzed using IPI2 WIN software. The underlying geo-electric sections comprises of topsoil, laterites, weathered basement, fractured basement, and fresh basement.The topsoil has resistivity and thickness ranges between 44.1- 862?m and 0.5 – 3.52m. The second layer which is laterites possess resistivity and thickness between 16.3 - 2001 ?m and 0.62 – 10.3m, The third layer is weathered basement having resistivity and thickness ranges from 11.0 – 755 ?m and 3.1 – 52.0m. The fourth layer considered as fractured basement has resistivity and thickness between 93.1 - 3247 ?m and 14.8 – 71.1m and final layer is fresh basement which possess resistivity ranges between 73.7 – 8444 ?m.The interpretation from the resistivity log of regolith rocks shows different curve types which include HA, HKH, QH, H and A – type curves. About 55% of the regolith in the area possesses aquifer potential value of 10.5 which shows optimum weathering and groundwater potential, therefore, any future borehole should be sited in these locations which are 3, 4, 8, 9, 10, 12, 13, 14, 16, 18, and 20. This study will provide a baseline hydrogeophysical data bank for prospective scientists, agriculturalists and relevant agencies that may be concerned with rural water supply and food security.
机译:本研究进行了使用垂直电气探测(VES)来确定ILorin的地下水潜力。 VES数据是从研究区域的二十(20)个位置生成的,并且稍后使用IPI2 Win软件进行处理和分析。底层的地质电路包括甲醛,肤质,风化的地下室,裂缝地下室和新鲜地下室。表土的电阻率和厚度范围在44.1-862Ω·m和0.5-3.52m之间。第二层是横向于16.3-2001×m和0.62-103m的电阻率和厚度,第三层是受风化的基底,电阻率和厚度范围为11.0-755Ωm和3.1-52.0m。被认为是裂缝地下室的第四层具有93.1-2247μm和14.8 - 71.1米和最终层的电阻率和厚度是新的基础,其具有73.7-8444Ω·m的电阻率范围。从岩石岩石的电阻率测量的解释显示不同曲线类型包括HA,HKH,QH,H和A型曲线。该地区约有55%的石油石具有10.5的含水层潜在值,其显示出最佳的风化和地下水潜力,因此,任何未来的钻孔都应该在这些位置占据3,4,8,9,10,12,13,本研究将为可能涉及农村供水和粮食安全的前瞻性科学家,农业学家和有关机构提供基线水文学科数据库。

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