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首页> 外文期刊>Journal of water resource and protection >Assessment of Groundwater Potential and Aquifer Characteristics in the Vicinity of Igun, Eku and Oria in Delta State, Nigeria
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Assessment of Groundwater Potential and Aquifer Characteristics in the Vicinity of Igun, Eku and Oria in Delta State, Nigeria

机译:尼日利亚三角州伊贡,伊库和奥里亚附近的地下水潜力和含水层特征评估

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This study was carried out to investigate the groundwater potential and aquifer characteristics of locations in Igun, Eku and Oria in Delta State, Nigeria. Nine vertical electrical soundings using the Schlumberger configuration were conducted to assess the geoelectric properties of the subsurface, while down-hole loggings and pumping test were employed to evaluate the aquifer characteristics of the area. The geoelectric data were interpreted by partial curve matching and computer iteration techniques to determine the resistivity, thickness and depth of the subsurface formations. The result revealed the presence of four geoelectric layers comprising of lateritic/loamy topsoil, clay, fine-medium grain sand, and coarse sand. Analysis of the geoelectric interpretation indicates that the third and fourth layers are water bearing horizons. Result further indicates that the fourth layer with a resistivity range of 2212 to 7148 Ωm and depth range of 24.7 to 31.9 m is more prolific than the third layer aquifer. The result of hydrogeological investigation showed that the electrical conductivity of the groundwater aquifer in Igun, Eku and Oria are 0.028, 0.032 and 0.024 mS/m respectively, while their corresponding total dissolved solid are 91.08, 95.92 and 79.53 mg/m~3. The result also showed that the transmissivity of the groundwater in Igun, Eku and Oria are 0.0728, 0.0873 and 0.0679 m~2/min respectively while their corresponding storativity were obtained as 3.21 × 10~(-4), 4.71 × 10~(-4), and 2.87 × 10~(-4). These results obtained from the three locations have shown that the groundwater aquifer is reliable in terms of quality and yield as they conform to international standards.
机译:这项研究的目的是调查尼日利亚三角州伊贡,伊库和奥里亚各地区的地下水潜力和含水层特征。使用斯伦贝谢配置进行了9次垂直电测深,以评估地下的地电特性,同时采用井下测井和抽水试验评估该地区的含水层特征。通过部分曲线匹配和计算机迭代技术解释了地电数据,以确定地下岩层的电阻率,厚度和深度。结果表明存在四个地电层,包括红土/壤质表层土,粘土,中细粒度砂和粗砂。对地电解释的分析表明,第三层和第四层是含水层。结果进一步表明,电阻率范围为2212至7148Ωm且深度范围为24.7至31.9 m的第四层比第三层含水层的产多。水文地质调查结果表明,伊贡,伊库和奥里亚地下水含水层的电导率分别为0.028、0.032和0.024 mS / m,而它们相应的总溶解固体为91.08、95.92和79.53 mg / m〜3。结果还表明,伊贡,伊库和奥里亚的地下水透过率分别为0.0728、0.0873和0.0679 m〜2 / min,而相应的渗透率分别为3.21×10〜(-4),4.71×10〜(- 4)和2.87×10〜(-4)。从这三个地点获得的结果表明,地下水蓄水层符合国际标准,因此在质量和产量方面都是可靠的。

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