Use of Geoelectric Method for Groundwater Assessment in  Awe Brine Area, Awe Nasarawa Nigeria

Authors

  • Mohammed Aliyu Kaura
    Department of Geology, Federal University of Lafia, Nasarawa state, Nigeria
    https://orcid.org/0000-0001-6372-7125
  • Abdullahi Ahmed Sule
    Department of Physics, Federal University of Lafia, Nasarawa state, Nigeria
  • Umar Nuhu Degree
    Department of Geology, Federal University of Lafia, Nasarawa state, Nigeria
  • Saidu Bello Mamudu
    National Biotechnology Research and Development Agency, Bioresources Development Center Billiri Gombe State, Nigeria
  • Yohannah Andrawus
    Department of Geology, Federal University of Lafia, Nasarawa state, Nigeria
  • Badamisi Muhammad Maina
    Department of Geology, Federal University of Lafia, Nasarawa state, Nigeria
  • Abdulrafiu Sherif
    Department of Geology, Federal University of Lafia, Nasarawa state, Nigeria
  • Aliyu Salihu
    Department of Geology, Federal University of Lafia, Nasarawa state, Nigeria

Keywords:

Array, Array, Array, Array, Array, Array, Array

Abstract

A total of Forty-five vertical electrical soundings (VES) were conducted using Schlumberger electrode configuration to map the groundwater condition in the Awe Brine Field, Nasarawa, Nigeria. The result of the study exhibited significant variations in resistivity across the area, which allowed the generation of iso-resistivity contour maps for four distinct geoelectric layers. The first layer, consisting of a thin top layer of unconsolidated material, displayed resistivity values ranging from 85 Ωm to 2437.8 Ωm. The second layer, composed of shale-sandstone, has a resistivity between 1.2 Ωm to 785 Ωm. The third layer showed resistivity ranging from 1.2 Ωm to 430.5 Ωm. it was observed that a thick layer of sandy clay contained fresh water, with resistivity levels ranging from 27 Ωm to 1825.9 Ωm. The Dar Zarrouk parameters were calculated to evaluate the protective attributes of the aquifers. The analysis revealed that the longitudinal conductance (Sc) ranged from 0.06 to 3.86 S, the longitudinal resistivity (ρL)) ranged from 71.66 to 3830.4 Ωm, and the transverse resistance (TR) ranged between 2.55 and 1102.18 Ω. Based on the resistivity values and thickness of the geoelectric layers, the researchers identified four distinct aquifer zones labelled A, B, C, and D. Notably, the third layer, referred to as the C horizon, displayed significantly lower resistivity and higher salinity compared to the other layers. This layer corresponds to the Awe Formation, renowned for its brine deposits. Consequently, the study suggests that exploring freshwater resources near New Awe is more promising than the Old Awe area

Dimensions

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Published

2024-06-08

How to Cite

Use of Geoelectric Method for Groundwater Assessment in  Awe Brine Area, Awe Nasarawa Nigeria. (2024). Lafia Journal of Scientific and Industrial Research, 2(2), 29-39. https://doi.org/10.62050/ljsir2024.v2n2.245

Issue

Volume 2, Issue 2 (October, 2024), Lafia Journal of Scientific and Industrial Research (LJSIR)

Section

Physical Sciences
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How to Cite

Use of Geoelectric Method for Groundwater Assessment in  Awe Brine Area, Awe Nasarawa Nigeria. (2024). Lafia Journal of Scientific and Industrial Research, 2(2), 29-39. https://doi.org/10.62050/ljsir2024.v2n2.245

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