Mapping a spatial salinity flow from seawater to groundwater using electrical resistivity topography techniques

In this work, the spatial salinity flow of surface water (ocean) into coastal groundwater (wells and boreholes water) in Okun-Ajah and its environ is reported using Electrical Resistivity Tomography (ERT) to show the interaction of surface water with the aquifer of the adjoining coastal communities....

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Main Author: Adeatyo Femi Folorunso
Format: Article
Language:English
Published: Elsevier 2021-09-01
Series:Scientific African
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S2468227621002611
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spelling doaj-228f3557544e448f942546600bd7daf02021-10-03T04:43:39ZengElsevierScientific African2468-22762021-09-0113e00957Mapping a spatial salinity flow from seawater to groundwater using electrical resistivity topography techniquesAdeatyo Femi Folorunso0Department of Marine Science and Technology, The Federal University of Technology, Akure, NigeriaIn this work, the spatial salinity flow of surface water (ocean) into coastal groundwater (wells and boreholes water) in Okun-Ajah and its environ is reported using Electrical Resistivity Tomography (ERT) to show the interaction of surface water with the aquifer of the adjoining coastal communities. The ERT data were supported with measurements of in situ hydro-physical parameters for confirmation. Eight (8) ERT traverses were established in the area, and nineteen (19) shallow wells, eight (8) deep wells (boreholes) and eight (8) surface water samples were analysed in situ in the work. The ERT model inversion show underground aquifer with very low resistivity all through the profiles established parallel to the coast while the very low resistivity region thin out under the traverses established perpendicular or tangential to the coast. Hydro-physical parameters such as electrical conductivity (EC), total dissolved solids (TDS). pH and temperature were also measured for all categories of water sampled (wells, boreholes and ocean). The results show that the concentrations of EC and TDS, agents of salinity, reduce away from the ocean, while aquifers with clear proximity to the ocean show elevated values. The correlation of all data clearly indicated the underground flow path of the ocean into the coastal aquifers. The integrated techniques have proven to be veritable tools to map saline water intrusion into coastal aquifers.http://www.sciencedirect.com/science/article/pii/S2468227621002611Coastal aquiferGroundwaterHydro-physicalSalinityFlowpath
collection DOAJ
language English
format Article
sources DOAJ
author Adeatyo Femi Folorunso
spellingShingle Adeatyo Femi Folorunso
Mapping a spatial salinity flow from seawater to groundwater using electrical resistivity topography techniques
Scientific African
Coastal aquifer
Groundwater
Hydro-physical
Salinity
Flowpath
author_facet Adeatyo Femi Folorunso
author_sort Adeatyo Femi Folorunso
title Mapping a spatial salinity flow from seawater to groundwater using electrical resistivity topography techniques
title_short Mapping a spatial salinity flow from seawater to groundwater using electrical resistivity topography techniques
title_full Mapping a spatial salinity flow from seawater to groundwater using electrical resistivity topography techniques
title_fullStr Mapping a spatial salinity flow from seawater to groundwater using electrical resistivity topography techniques
title_full_unstemmed Mapping a spatial salinity flow from seawater to groundwater using electrical resistivity topography techniques
title_sort mapping a spatial salinity flow from seawater to groundwater using electrical resistivity topography techniques
publisher Elsevier
series Scientific African
issn 2468-2276
publishDate 2021-09-01
description In this work, the spatial salinity flow of surface water (ocean) into coastal groundwater (wells and boreholes water) in Okun-Ajah and its environ is reported using Electrical Resistivity Tomography (ERT) to show the interaction of surface water with the aquifer of the adjoining coastal communities. The ERT data were supported with measurements of in situ hydro-physical parameters for confirmation. Eight (8) ERT traverses were established in the area, and nineteen (19) shallow wells, eight (8) deep wells (boreholes) and eight (8) surface water samples were analysed in situ in the work. The ERT model inversion show underground aquifer with very low resistivity all through the profiles established parallel to the coast while the very low resistivity region thin out under the traverses established perpendicular or tangential to the coast. Hydro-physical parameters such as electrical conductivity (EC), total dissolved solids (TDS). pH and temperature were also measured for all categories of water sampled (wells, boreholes and ocean). The results show that the concentrations of EC and TDS, agents of salinity, reduce away from the ocean, while aquifers with clear proximity to the ocean show elevated values. The correlation of all data clearly indicated the underground flow path of the ocean into the coastal aquifers. The integrated techniques have proven to be veritable tools to map saline water intrusion into coastal aquifers.
topic Coastal aquifer
Groundwater
Hydro-physical
Salinity
Flowpath
url http://www.sciencedirect.com/science/article/pii/S2468227621002611
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