Evaluation of Aquifer Protective Capacity and Groundwater Potential in Part of Iju, Akure-North, Ondo State, Nigeria

Authors

  • A. Olajide Department of Applied Geophysics, Federal University of Technology Akure, Ondo State, Nigeria
  • S. Bayode Department of Applied Geophysics, Federal University of Technology Akure, Ondo State, Nigeria
  • T. Fagbemigun Department of Geophysics, Federal University, Oye Ekiti, Ekiti State, Nigeria
  • A. Oyebamiji Department of Geology, Federal University, Oye Ekiti, Ekiti State, Nigeria
  • J. Amosun Department of Geophysics, Federal University, Oye Ekiti, Ekiti State, Nigeria
  • A. Owasanoye Department of Physics, Federal University, Oye Ekiti, Ekiti State, Nigeria

Keywords:

Vertical Electrical Sounding, Very Low Frquency Electromagnetic, Groundwater Potential, Aquifer Protective Capacity

Abstract

Groundwater potential and aquifer protective capacity of the overburden unit was evaluated in part of Iju, Akure North, Ondo State using integrated geophysical methods involving Very Low Frequency Electromagnetic (VLF-EM) profiling and Vertical Electrical Sounding (VES). Four major traverses were established of varying length extents. The VLF-EM measurements were taken along the four major profiles of 10 m station interval.
Forty two (42) Vertical Electrical Soundings were also conducted with half electrode spacing varying between 1 and 100 m and interpretation was done using the partial curve matching techniques and computer aided iteration. Five subsurface geological units were identified from geoelectric sections, consisting of the top soil, lateritic, weathered, partly weathered and fresh basement layers consecutively. For the first layer, resistivity
ranges between 23 and 323 ?m with values of thickness ranging between 0.5 and 2.2 m. The resistivity and thickness of the second (lateritic) layer range from 132 to 430 ?m and 1.6 to 4 m respectively. The resistivity of the weathered layer ranges from 4 to 94 ?m and variable thickness between 10 and 24.4 m. The fourth layer has a resistivity value range of 65 to 120 ?m and thicknesses between 20 and 30 m. The basement bedrock (fifth layer) has resistivity values between 770 and 820 ?m. The depth to bedrock ranges from 1.8 to 31 m. The geophysical data and the basement aquifer delineated were then used to evaluate the hydrogeological setting and aquifer protective capacity of the study area. The observation from the results shows that close to 70 % of the study area falls within the zones of low groundwater potential, 25 % falls within medium potential zones while only 5 % make up the high potential zones. 75 % of the study area constituted the weak to poor protective capacity zones.

 

Author Biographies

A. Olajide, Department of Applied Geophysics, Federal University of Technology Akure, Ondo State, Nigeria

 

 

S. Bayode, Department of Applied Geophysics, Federal University of Technology Akure, Ondo State, Nigeria

 

 

T. Fagbemigun, Department of Geophysics, Federal University, Oye Ekiti, Ekiti State, Nigeria

 

 

A. Oyebamiji, Department of Geology, Federal University, Oye Ekiti, Ekiti State, Nigeria

 

 

J. Amosun, Department of Geophysics, Federal University, Oye Ekiti, Ekiti State, Nigeria

 

 

A. Owasanoye, Department of Physics, Federal University, Oye Ekiti, Ekiti State, Nigeria

 

 

Dimensions

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Published

2020-08-01

How to Cite

Evaluation of Aquifer Protective Capacity and Groundwater Potential in Part of Iju, Akure-North, Ondo State, Nigeria. (2020). Journal of the Nigerian Society of Physical Sciences, 2(3), 197-204. https://doi.org/10.46481/jnsps.2020.32

Issue

Section

Original Research

How to Cite

Evaluation of Aquifer Protective Capacity and Groundwater Potential in Part of Iju, Akure-North, Ondo State, Nigeria. (2020). Journal of the Nigerian Society of Physical Sciences, 2(3), 197-204. https://doi.org/10.46481/jnsps.2020.32