Groundwater Vulnerability Assessment using Electrical Resistivity Method in the Northern part of Ado-Ekiti, Southwestern Nigeria

被引:1
|
作者
Olaseeni, O. G. [1 ]
Oladapo, M., I [2 ]
Olayanju, G. M. [2 ]
Dada, O. J. [1 ]
Oyebamiji, A. R. [1 ]
机构
[1] Fed Univ Oye Ekiti, Oye Ekiti, Ekiti State, Nigeria
[2] Fed Univ Technol Akure, Akure, Ondo State, Nigeria
来源
3RD INTERNATIONAL CONFERENCE ON SCIENCE AND SUSTAINABLE DEVELOPMENT (ICSSD 2019): SCIENCE, TECHNOLOGY AND RESEARCH: KEYS TO SUSTAINABLE DEVELOPMENT | 2019年 / 1299卷
关键词
geo-electric; resistivity; thickness; contamination;
D O I
10.1088/1742-6596/1299/1/012068
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Over the years, the demand for clean and safe water has skyrocketed globally in response to rising population. Since groundwater is a more reliable source of potable water, assessment of aquifer vulnerability becomes a necessity. This research therefore aimed at delineating geo-electric parameters inform of layer resistivity and thickness, towards generating a second order geo-electric section. This study employed the use of electrical resistivity method to evaluate the vulnerability of aquifers to contamination in the northern part of Ado-Ekiti, southwestern Nigeria. Forty Vertical Electrical Sounding (VES) locations were studied using the Schlumberger array with current electrodes spacing (AB/2) of 150m. ABEM SAS 300 Resistivity Meter was useful for collecting the VES data which were presented as VES curves and quantitatively interpreted through partial curve matching and Computer Assisted 1-D forward modeling using the WinResist software. Geo-electric section along five (5) traverses, iso-resistivity map of the weathered layer and an isopach map showing the depth to aquifer were generated. Seven (7) different types of VES curves were identified, namely A, H, K, KA, HA, QA and KH types. The four geo-electric layers delineated include the topsoil (resistivity values between 29 - 1176 Omega m; thickness from 0.5 - 4.4 m), lateritic layer (resistivity values between 138- 3787 Omega m; thickness between 1.0 - 63.6m), weathered layer (resistivity values between 6 - 298 Omega m; thickness between 0.7 - 17.8 m), and fresh basement (resistivity values between 331 - 7479 Omega m). The total longitudinal unit conductance (S) values obtained range from 0.009 to 2.972 mhos. This suggests that most parts (northern, central, western and eastern portions of the area) have medium to high protective capacity rating; except the eastern portion. Therefore, most parts (80%) of the study area appear to be less vulnerable to contamination.
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页数:20
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