Open AccessEvaluation of Lithological Effect on Aquifer Transmissivity and Conductivity in Parts of Rivers State, Nigeria using Vertical Electrical Sounding (VES)
Author(s) -
Chukwu C Ben,
AUTHOR_ID,
Ovua D. Hope
Publication year - 2021
Publication title -
journal of earth and environmental science research
Language(s) - English
Resource type - Journals
ISSN - 2634-8845
DOI - 10.47363/jeesr/2021(3)161
Subject(s) - aquifer , vertical electrical sounding , lithology , geology , borehole , depth sounding , groundwater , hydraulic conductivity , hydrology (agriculture) , groundwater flow , electrical resistivity and conductivity , soil science , geotechnical engineering , petrology , soil water , oceanography , electrical engineering , engineering
Vertical Electrical Sounding (VES) was used to evaluate the effect of lithology on aquifer transmissivity and conductivity in parts of Rivers State, Nigeria. A total of 10 Vertical Electrical Sounding were conducted at ten locations. The VES data were collected using ABEM terrameter SAS 300B and processed using Win-Resist Software and Microsoft Excel Sheet. The effect of the lithology on aquifer transmissivity and conductivity were analyzed. Result from the Vertical Electrical Sounding revealed a four to six geoelectric layers. The aquifer resistivity values range from 39.40Ωm to 17290.7Ωm. Results of the aquifer conductivity values range from 0.005 to 2.538cm/s with the highest value dominating in the central part of the study area suggesting large grain sands that can permeate groundwater flow while the transmissivity values range from 0.22587cm/s2 to 132.487 cm/s2 with average of 19.1587cm/s2. Area with high transmissivity is identified with high groundwater potential permeable with groundwater flow is seen in the central part of the study area with range of 110 to 135 cm/s2 indicating a thick sandy aquifer. Result from the nearby borehole in correlation with the VES point showed an agreement with the VES data at Ogale Eleme and Elelenwo location. The result of the study can be applied in ground water resources management, hydrological studies and provides valuable information for town planner.