Authors :
Tom Cyprian N.; Warmate Tamunonengiyeofori; Tamunosiki Dieokuma
Volume/Issue :
Volume 11 - 2026, Issue 3 - March
Google Scholar :
https://tinyurl.com/2t35m7vt
Scribd :
https://tinyurl.com/bsta59zz
DOI :
https://doi.org/10.38124/ijisrt/26mar1475
Note : A published paper may take 4-5 working days from the publication date to appear in PlumX Metrics, Semantic Scholar, and ResearchGate.
Abstract :
Hydrological estimates were derived from geophysical parameters to assess aquifer proficiency in the Borokiri
area of the Niger Delta. Schlumberger vertical electrical soundings were conducted with a maximum current electrode
spread (AB) of 400m, generating HK-type model curves. Dar Zarrouk parameters extracted from the geoelectric data
were converted to relevant hydrological properties, including hydraulic conductivity and transmissivity. The study reveals
highly prolific aquifer zones with resistivity values exceeding 1000 Ωm and modelled transmissivity values of 2125 m²/day,
classified as Krasny Class I magnitude—indicating regional groundwater importance. Formation factor analysis, based on
established porosity and cementation values within the Benin Formation, enabled quantitative estimation of hydraulic
conductivity. The geoelectric sections delineated four subsurface layers, with the third layer (18.5m thick at 24.8m depth)
identified as the primary freshwater aquifer, underlain by a fourth layer with extremely low resistivity (1.1 Ωm),
interpreted as a saline aquifer resulting from saltwater intrusion. Calculated longitudinal conductance values of less than
0.1 siemens indicate poor overburden protective capacity, rendering the aquifer vulnerable to surface contamination.
These findings demonstrate that while the Borikiri area hosts high-yield freshwater aquifers suitable for regional water
supply, the absence of protective clay layers necessitates careful contamination management. The study confirms the
efficacy of integrating Dar Zarrouk parameter analysis with conventional resistivity sounding for quantitative aquifer
evaluation in complex deltaic environments.
Keywords :
Aquifer Transmissivity; Hydraulic Conductivity; Dar Zarrouk Parameters; Schlumberger Sounding; Saline Water Intrusion; Niger Delta; Groundwater Vulnerability; Electrical Resistivity.
References :
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- Alaminokuma, G.I., Nwankwoala, H.O. and Amadi, A.N., “Petrophysical Evaluation of the Benin Formation Using Porosity and Cementation Factor Relationships in Southern Nigeria”, International Journal of Scientific & Engineering Research, 6(3), pp.112–120, 2015.
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- Inyang, G.E., Nwosu, L.I. and Ezeh, C.C., “Estimation of Aquifer Transmissivity Using Dar-Zarrouk Parameters in Layered Sedimentary Basins”, HydroResearch, 4, pp.45–56, 2021.
- Niwas, S. and Singhal, D.C., “Estimation of Aquifer Transmissivity from Dar-Zarrouk Parameters in Porous Media”, Journal of Hydrology, 50(1–4), pp.393–399, 1981.
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- Okiongbo, K.S., Akpofure, E.A. and Odubo, E., “Deermination of Groundwater Potential and Aquifer Protective Capacity Using Resistivity Method in Parts of the Niger Delta, Nigeria”, International Journal of Geosciences, 6(10), pp.1127–1140, 2015.
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Hydrological estimates were derived from geophysical parameters to assess aquifer proficiency in the Borokiri
area of the Niger Delta. Schlumberger vertical electrical soundings were conducted with a maximum current electrode
spread (AB) of 400m, generating HK-type model curves. Dar Zarrouk parameters extracted from the geoelectric data
were converted to relevant hydrological properties, including hydraulic conductivity and transmissivity. The study reveals
highly prolific aquifer zones with resistivity values exceeding 1000 Ωm and modelled transmissivity values of 2125 m²/day,
classified as Krasny Class I magnitude—indicating regional groundwater importance. Formation factor analysis, based on
established porosity and cementation values within the Benin Formation, enabled quantitative estimation of hydraulic
conductivity. The geoelectric sections delineated four subsurface layers, with the third layer (18.5m thick at 24.8m depth)
identified as the primary freshwater aquifer, underlain by a fourth layer with extremely low resistivity (1.1 Ωm),
interpreted as a saline aquifer resulting from saltwater intrusion. Calculated longitudinal conductance values of less than
0.1 siemens indicate poor overburden protective capacity, rendering the aquifer vulnerable to surface contamination.
These findings demonstrate that while the Borikiri area hosts high-yield freshwater aquifers suitable for regional water
supply, the absence of protective clay layers necessitates careful contamination management. The study confirms the
efficacy of integrating Dar Zarrouk parameter analysis with conventional resistivity sounding for quantitative aquifer
evaluation in complex deltaic environments.
Keywords :
Aquifer Transmissivity; Hydraulic Conductivity; Dar Zarrouk Parameters; Schlumberger Sounding; Saline Water Intrusion; Niger Delta; Groundwater Vulnerability; Electrical Resistivity.