GEOPHYSICAL INVESTIGATION FOR POST-FOUNDATION ASSESSMENT WITHIN EKITI STATE UNIVERSITY, ADO EKITI, SOUTHWESTERN NIGERIA

Ilugbo Stephen Olubusola, Ajayi Christopher Ayodele, Madukwe Henry Yemagu, A. Babatunde A., Talabi Abel Ojo, O. Akinola, O. Felix, Ajisafe Yemisi Christianah, Talabi Joseph Ifeoluwa
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Abstract

This study has evaluated the post-construction subsoil integrity of a distressed building in Ado-Ekiti, Southwestern Nigeria, to decipher the in-situ lithology and structural disposition. Four traverses of 100 m length were established in approximately E-W direction with an inter-station spacing of 10 m. Two Geophysical methods were deployed including the ground magnetic method using Proton Precession Magnetometer and Electrical Resistivity method utilizing 2D Electrical Imaging and Vertical Electrical Sounding (VES) techniques. Twelve (20) VES station points were acquired within the investigated area using Schlumberger configuration which gave relevant information on layer stratification and geoelectric parameters. The obtained results from the VES showed four geo-electric layers comprises topsoil, clayey layer, weathered layer, fractured bedrock, and fresh basement. Low apparent resistivity was delineated from the 2D imaging exhibiting unfit materials at distance between 50 to 75 m and 80 to 100m. The magnetic results showed a series of bedrock ridges and depressions. The integration of results revealed that the majority of the study areas are unsuitable except for central parts which indicate appreciable competence and stability.
尼日利亚西南部ado ekiti ekiti州立大学地基后评价的地球物理调查
本研究评估了尼日利亚西南部Ado-Ekiti一座废弃建筑的施工后底土完整性,以破译原位岩性和结构配置。在大约东西向建立了4条长度为100 m的导线,站间间距为10 m。采用了两种地球物理方法,包括利用质子进动磁强计的地磁法和利用二维电成像和垂直电测深(VES)技术的电阻率法。利用斯伦贝谢的配置,在调查区域内获得了12(20)个VES测点,提供了地层分层和地电参数的相关信息。结果表明:地电层分为表土层、黏性层、风化层、破碎基岩层和新鲜基底层。二维成像显示50 ~ 75 m和80 ~ 100m之间的不适宜材料的视电阻率较低。磁测结果显示出一系列基岩脊和洼地。综合分析结果表明,除中心区域具有较强的竞争力和稳定性外,其余区域均不适宜。
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