Integrated Geophysical Methods for Post Construction Studies: Case study of Omuo Comprehensive High School, Omuo Ekiti, Southwestern, Nigeria

Article ID

GUOS1

Integrated Geophysical Methods for Post Construction Studies: Case study of Omuo Comprehensive High School, Omuo Ekiti, Southwestern, Nigeria

A.O. Adelusi
A.O. Adelusi
A.A. Akinlalu
A.A. Akinlalu
B .W. Daramola
B .W. Daramola
DOI

Abstract

An integrated geophysical survey was carried out within the Precambrian Basement Complex of Omuo Comprehensive High School and its environ in Omuo-Ekiti, Ekiti State, South-west Nigeria to assess buildings in the area that are intensively affected by cracks resulting in structural instability. The geophysical methods adopted for the investigation are the Very Low Frequency Electromagnetic (VLF-EM), Magnetic, 2-D electrical resistivity profiling using the dipole-dipole array and Vertical Electrical Soundings (VES) using the Schlumberger array. The traverses were established E – W direction cutting across geologic strike. A total of five traverses were established with length ranging from 130 – 200m and of varying inter-traverse spacing. The station interval is 10m. Also, a total of thirty-five (35) VES stations were occupied covering the entire study area. The acquired data were processed and interpreted integrally to elucidate the shallow subsurface geology of the study area. The results were qualitatively and quantitatively interpreted and are presented as sounding curves and geo-electric sections. The magnetic interpretation shows relatively uneven bedrock topography with variable overburden thicknesses of between 5m – 15m. However, the VLF-EM results reveal ten (10) conductive zones which manifest as low resistivity zones in the generated geo-electric sections. The characteristic sounding curves obtained from the study area are H, HA, KH, HK, KHK, HAK and QH. The geo-electric sections reveal four subsurface layers which include: The topsoil, with resistivity values ranging from 104 – 4656 ohm-m and thickness of between 0.4 – 1.6 m. The weathered layer is characterized by resistivity values varying from 57 – 381 ohm-m and thicknesses of between 0.2 – 9.0 m. The fractured basements were identified beneath traverses 1, 2 and 5 with resistivity values of 109 – 709 ohm-m and depth range of 5.5 – 15.8m. The fresh basement has resistivity values of betwe

Integrated Geophysical Methods for Post Construction Studies: Case study of Omuo Comprehensive High School, Omuo Ekiti, Southwestern, Nigeria

An integrated geophysical survey was carried out within the Precambrian Basement Complex of Omuo Comprehensive High School and its environ in Omuo-Ekiti, Ekiti State, South-west Nigeria to assess buildings in the area that are intensively affected by cracks resulting in structural instability. The geophysical methods adopted for the investigation are the Very Low Frequency Electromagnetic (VLF-EM), Magnetic, 2-D electrical resistivity profiling using the dipole-dipole array and Vertical Electrical Soundings (VES) using the Schlumberger array. The traverses were established E – W direction cutting across geologic strike. A total of five traverses were established with length ranging from 130 – 200m and of varying inter-traverse spacing. The station interval is 10m. Also, a total of thirty-five (35) VES stations were occupied covering the entire study area. The acquired data were processed and interpreted integrally to elucidate the shallow subsurface geology of the study area. The results were qualitatively and quantitatively interpreted and are presented as sounding curves and geo-electric sections. The magnetic interpretation shows relatively uneven bedrock topography with variable overburden thicknesses of between 5m – 15m. However, the VLF-EM results reveal ten (10) conductive zones which manifest as low resistivity zones in the generated geo-electric sections. The characteristic sounding curves obtained from the study area are H, HA, KH, HK, KHK, HAK and QH. The geo-electric sections reveal four subsurface layers which include: The topsoil, with resistivity values ranging from 104 – 4656 ohm-m and thickness of between 0.4 – 1.6 m. The weathered layer is characterized by resistivity values varying from 57 – 381 ohm-m and thicknesses of between 0.2 – 9.0 m. The fractured basements were identified beneath traverses 1, 2 and 5 with resistivity values of 109 – 709 ohm-m and depth range of 5.5 – 15.8m. The fresh basement has resistivity values of betwe

A.O. Adelusi
A.O. Adelusi
A.A. Akinlalu
A.A. Akinlalu
B .W. Daramola
B .W. Daramola

No Figures found in article.

Akinlalu,A.A. 2014. “. Global Journal of Science Frontier Research – H: Environment & Environmental geology GJSFR-H Volume 14 (GJSFR Volume 14 Issue H1): .

Download Citation

Journal Specifications

Crossref Journal DOI 10.17406/GJSFR

Print ISSN 0975-5896

e-ISSN 2249-4626

Issue Cover
GJSFR Volume 14 Issue H1
Pg. 31- 41
Classification
Not Found
Article Matrices
Total Views: 4531
Total Downloads: 2309
2026 Trends
Research Identity (RIN)
Related Research
Our website is actively being updated, and changes may occur frequently. Please clear your browser cache if needed. For feedback or error reporting, please email [email protected]

Request Access

Please fill out the form below to request access to this research paper. Your request will be reviewed by the editorial or author team.
X

Quote and Order Details

Contact Person

Invoice Address

Notes or Comments

This is the heading

Lorem ipsum dolor sit amet, consectetur adipiscing elit. Ut elit tellus, luctus nec ullamcorper mattis, pulvinar dapibus leo.

High-quality academic research articles on global topics and journals.

Integrated Geophysical Methods for Post Construction Studies: Case study of Omuo Comprehensive High School, Omuo Ekiti, Southwestern, Nigeria

A.O. Adelusi
A.O. Adelusi
A.A. Akinlalu
A.A. Akinlalu
B .W. Daramola
B .W. Daramola

Research Journals