Javascript must be enabled to continue!
Subsurface Corrosivity Assessment Using Subsoil Resistivity in a Typical Basement Terrain: A Case Study of the Adebowale Area in Akure, Southwestern Nigeria
View through CrossRef
The aim of this study is to investigate and map the subsurface corrosivity of soils at various depths (0.5 - 3.0 m) within the Adebowale community in Akure, Southwestern Nigeria, and to identify safe zones for the burial of metallic objects based on soil resistivity measurements. Sixty vertical electrical sounding (VES) data points were acquired using the Schlumberger electrode array with half-current (AB/2) spacing ranging from 1 - 150/225 m. The VES survey delineated 3 - 5 subsurface layers across the study area, corresponding to topsoil, weathered layer, partially weathered basement, fractured basement, and fresh basement. Maps of longitudinal conductance, longitudinal resistivity, and iso-resistivity depth slices (0.5, 0.75, 1.0, and 3.0 m) were generated. The corrosivity of the subsoil in the study area was categorized into five types: very high corrosivity (< 50 ?m), high corrosivity (50 - 100 ?m), moderate corrosivity (100 - 150 ?m), low corrosivity (150 - 200 ?m), and negligible corrosivity (> 200 ?m). At 1.0 m and 3.0 m depth surfaces, the areas of negligible to low corrosivity are about 70% and 85%, respectively, suggesting that corrosivity decreases with depth within the shallow subsurface of the study area. The longitudinal conductance and longitudinal resistivity maps of Adebowale indicated that the areas of negligible to low corrosivity are about 85% and 75%, respectively, corroborating the depth slice resistivity maps. In these areas, buried metallic utilities are safe; conversely, any metallic utilities buried within the moderate to very high corrosivity zones of the study area must be adequately protected to avoid corrosion.
Title: Subsurface Corrosivity Assessment Using Subsoil Resistivity in a Typical Basement Terrain: A Case Study of the Adebowale Area in Akure, Southwestern Nigeria
Description:
The aim of this study is to investigate and map the subsurface corrosivity of soils at various depths (0.
5 - 3.
0 m) within the Adebowale community in Akure, Southwestern Nigeria, and to identify safe zones for the burial of metallic objects based on soil resistivity measurements.
Sixty vertical electrical sounding (VES) data points were acquired using the Schlumberger electrode array with half-current (AB/2) spacing ranging from 1 - 150/225 m.
The VES survey delineated 3 - 5 subsurface layers across the study area, corresponding to topsoil, weathered layer, partially weathered basement, fractured basement, and fresh basement.
Maps of longitudinal conductance, longitudinal resistivity, and iso-resistivity depth slices (0.
5, 0.
75, 1.
0, and 3.
0 m) were generated.
The corrosivity of the subsoil in the study area was categorized into five types: very high corrosivity (< 50 ?m), high corrosivity (50 - 100 ?m), moderate corrosivity (100 - 150 ?m), low corrosivity (150 - 200 ?m), and negligible corrosivity (> 200 ?m).
At 1.
0 m and 3.
0 m depth surfaces, the areas of negligible to low corrosivity are about 70% and 85%, respectively, suggesting that corrosivity decreases with depth within the shallow subsurface of the study area.
The longitudinal conductance and longitudinal resistivity maps of Adebowale indicated that the areas of negligible to low corrosivity are about 85% and 75%, respectively, corroborating the depth slice resistivity maps.
In these areas, buried metallic utilities are safe; conversely, any metallic utilities buried within the moderate to very high corrosivity zones of the study area must be adequately protected to avoid corrosion.
Related Results
Stratigraphic studies of Ganymede’s tectonic activity in the bright terrain: results from the Byblus Sulcus and Harpagia Sulcus regions
Stratigraphic studies of Ganymede’s tectonic activity in the bright terrain: results from the Byblus Sulcus and Harpagia Sulcus regions
The Jovian satellite Ganymede experienced a pronounced period of tectonic resurfacing forming the extended bright or light terrain the so-called Sulci, which cover about 2/3 of Gan...
Preliminary study of a new-style terrain disturbance method based on gradient inhomogeneity in convection-allowing scale ensemble prediction system
Preliminary study of a new-style terrain disturbance method based on gradient inhomogeneity in convection-allowing scale ensemble prediction system
<p>Terrain with different shapes and ground surface properties has extremely complex impacts on atmospheric motion, and the forecast uncertainty and complexity caused...
Subsurface Investigation of Basement Structures Using Electrical Resistivity Methods at Zainawa Village Kano, Nigeria
Subsurface Investigation of Basement Structures Using Electrical Resistivity Methods at Zainawa Village Kano, Nigeria
Electrical Resistivity Methods involving Schlumberger Vertical Electrical Sounding (VES) and Wenner Electrical Profiling (EP) were carried out to map the Geological features of the...
Hydatid Disease of The Brain Parenchyma: A Systematic Review
Hydatid Disease of The Brain Parenchyma: A Systematic Review
Abstarct
Introduction
Isolated brain hydatid disease (BHD) is an extremely rare form of echinococcosis. A prompt and timely diagnosis is a crucial step in disease management. This ...
An Integrated Approach to Calculate Vertical and Horizontal Resistivity Utilizing Conventional Logs in Low Resistivity Pay Reservoirs in Gulf of Suez: Case Study
An Integrated Approach to Calculate Vertical and Horizontal Resistivity Utilizing Conventional Logs in Low Resistivity Pay Reservoirs in Gulf of Suez: Case Study
The occurrence of Low Resistivity Pay (LRP) have been widely reported. The conventional induction resistivity log does not recognized LRP, because this phenomenon affects the conve...
Estimating subsoil diffusivity and respiration by inverse modelling: results from first case studies
Estimating subsoil diffusivity and respiration by inverse modelling: results from first case studies
Soils are important terrestrial biological reactors and play a central role in the global carbon (C) and nitrogen (N ) cycle. Soils can store large amounts of C and N, but they als...
Crater on Ganymede emplaced at the border of the dark and bright terrain – view into the subsurface properties
Crater on Ganymede emplaced at the border of the dark and bright terrain – view into the subsurface properties
Two major terrain units dominate Ganymede’s surface: 1) the ancient heavily cratered dark terrain and 2) the tectonically resurfaced bright or light terrain (Collins et a...
Preliminary study on terrain uncertainty and its perturbing scheme
Preliminary study on terrain uncertainty and its perturbing scheme
<p>1.Introduction</p><p>A key issue in developing the ensemble prediction technique is the recognition of uncertain factors in numerical f...

