In the Niger Delta region of Nigeria, specifically in Ughelli and its surrounding areas,
the VES geophysical method was employed to investigate groundwater potential and
aquifer vulnerability. The Schlumberger array, utilized for the conduction of Vertical
Electrical Sounding (VES), facilitated the selection of ten specific VES locations. The
maximum spacing of the current electrodes (AB/2) reached 100 meters while utilizing
the ABEM Terrameter SAS 1000. Data interpretation was carried out using IX1D
software, which incorporated a partial curve matching technique alongside a
computer iteration method. The analysis of the estimated parameters revealed ranges
for longitudinal conductance (S) between 9 and 379.09, transverse unit resistance (Tr)
between 2.79Ω/m² and 5344.14Ω/m², longitudinal resistance (ρL) from 1.88 Ω-m to
544.8 Ω-m, and transverse resistance values ranging from 2 to 538.74. The
investigation identified the existence of four to five distinct layers of curve types,
with curve HK and HKA being the predominant types. Analysis of the VES layers
indicated a range of four to five layers. Furthermore, the findings from the Tr values
demonstrated that the area surrounding VES 9 exhibited greater groundwater
potential in comparison to other regions within the study area.
Keywords: Resistivity, Depth, Thickness, Curve type
