ASSESSMENT OF GROUNDWATER POTENTIALS AT UDI LOCAL GOVERNMENT AREA, ENUGU STATE, NIGERIA

Abbey M. E, Onyebueke D. E
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引用次数: 1

Abstract

A geophysical study comprising vertical electrical soundings was carried out in four (4) locations (Udi 1, Udi 2, Udi 3 and Udi 4) in Udi L.G.A. to assess groundwater potentials. The method involves the use of resistivity equipment (ABEM Terrameter), the field data were obtained utilizing Schlumberger configuration. The WINRESIST software was utilized in the data processing. According to the study’s findings, the geological formations present in these locations contain five to seven layers. Layers 1 has resistivity values ranging from 158.1 – 418.1 m at depths of 0.6 – 1.6 m, layer 2 has resistivity values ranging from 1103.9 – 41387.3  m at depths of 0.8 – 8.9 m, layer 3 has resistivity values ranging from 313.0 – 4782.9 m at depths of 6.9 – 28.2 m, layer 4 has resistivity values ranging from 1847.9 – 6956.8 m at depths of 11.8 – 154.6 m, layer 5 has resistivity values ranging from 115.0 – 2838.4 m at depths of 101.2 – 219.2 m, layer 6 has resistivity values ranging from 51.1 – 261.7 m at a depth 190.6 m, and layer 7 have a resistivity value of 47.1 m at an unknown depth. Layer 4 from all locations shows a prolific aquifer where enormous groundwater can be explored due to its high resistivity values, depth and thickness. The aquifer is estimated to be at the depths of 90.0 – 120.0 m. The results of this geophysical examination revealed that the studied region has good groundwater potential, which if properly utilized, will go a long way toward alleviating the effects of water insufficiency in Udi L.G.A.
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尼日利亚足努古州udi地方政府地区地下水潜力评估
在Udi L.G.A.的四个地点(Udi 1、Udi 2、Udi 3和Udi 4)进行了一项包括垂直电测深的地球物理研究,以评估地下水潜力。该方法包括使用电阻率设备(ABEM Terrameter),现场数据是利用斯伦贝谢配置获得的。数据处理采用WINRESIST软件。根据这项研究的发现,这些地方的地质构造包含五到七层。1层电阻率值从158.1 - 418.1米深度为0.6 - 1.6米,二层有电阻率值从1103.9 - 41387.3米深度为0.8 - 8.9米,第三层有电阻率值从313.0 - 4782.9米深度为6.9 - 28.2米,第四层电阻率值从1847.9 - 6956.8米深度为11.8 - 154.6米、5层电阻率值从115.0 - 2838.4米深度为101.2 - 219.2米,第6层的电阻率值为51.1 - 261.7,深度为190.6 m,第7层的电阻率值为47.1,深度未知。所有位置的第4层都显示了一个多产的含水层,由于其高电阻率值,深度和厚度,可以勘探大量地下水。据估计,该含水层的深度为90.0 - 120.0米。地球物理勘探结果表明,研究区具有良好的地下水潜力,如果利用得当,将对缓解乌地地区水资源不足的影响大有帮助
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