Evaluation of lithostratigraphic units and groundwater potential using the resolution capacities of two different electrical tomographic electrodes at dual-spacing

  • Adedibu Sunny AKINGBOYE Universiti Sains Malaysia, 11800 Pulau Pinang, Malaysia
  • Andy Anderson BERY Universiti Sains Malaysia, 11800 Pulau Pinang, Malaysia
Keywords: Electrical resistivity tomography (ERT), induced polarisation (IP) tomography, copper and stainless-steel electrodes, lithostratigraphy, groundwater, Penang Malaysia

Abstract

The selection of a choice electrode is pertinent to attenuating noise and improving geophysical tomographic inversion results. Besides, the detailed understanding of the geodynamic condition of subsurface formation is crucial to sustainable potable groundwater abstraction. Hence, the subsurface lithostratigraphic units and groundwater potential of two sites (i.e., Site 1 and Site 2) within the Universiti Sains Malaysia were evaluated using borehole-constrained electrical resistivity tomography (ERT) and induced polarisation (IP) tomography. Both methods employed the resolution capacities of stainless-steel and copper electrodes at dual-spacing. The ERT and IP field data and inversion results for copper electrodes were generally robust due to the generated higher positive data points and lower RMS errors, percentage relative differences, and mean absolute percentage errors (MAPE) than the stainless-steel electrodes, especially at Site 1 with a profile length of 200 m and an electrode spacing of 5 m. However, both electrodes tend to produce inversion models with almost the same parameters at Site 2, using half the profile length and electrode spacing of Site 1, i.e., 100 m and 2.5 m, respectively. Thus, the sensitivities and resolution capacities of the tomographic electrodes are heavily influenced by electrode spacing, profile length, amount of injected current, and depth of investigation. The borehole lithostratigraphic units, typically sandy silt, sand, and silty sand, have good correlations with the ERT and IP inversion results. The variability in observed resistivity and chargeability values were due to heterogeneous weathered materials and saturating water fills within the fractured and deeply-weathered granitic bedrock, with <200 Ωm and a chargeability of >1.8 msec. The models' median depth of >40 m mapped for the weathered and/or fractured sections was suggestive of high groundwater-yielding capacity in boreholes to sustain a part of the university community. 

Author Biographies

Adedibu Sunny AKINGBOYE, Universiti Sains Malaysia, 11800 Pulau Pinang, Malaysia

Geophysics Unit, School of Physics

Andy Anderson BERY, Universiti Sains Malaysia, 11800 Pulau Pinang, Malaysia

Geophysics Unit, School of Physics

Published
2021-12-22
How to Cite
AKINGBOYE, A. S., & BERY, A. A. (2021). Evaluation of lithostratigraphic units and groundwater potential using the resolution capacities of two different electrical tomographic electrodes at dual-spacing. Contributions to Geophysics and Geodesy, 51(4), 295-320. https://doi.org/10.31577/congeo.2021.51.4.1
Section
original research papers