Geophysical and Geotechnical Site Characterization at Lagos Central Area of Lagos State, Nigeria

R. B. Adegbola, K. Oyedele, Elizabeth Abidoye
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Abstract

Introduction: Geophysical characterization refers to the collection of information associated with subsurface features. Geotechnical involves engineering structural performance studies which are used to obtain information on the physical properties of soil and rock around a site to design earthworks and foundations for proposed structures and for repair of distress to earthworks and structures caused by subsurface conditions. Aim: The study was aimed at characterizing the subsurface formations for the purpose of determining its capacity to withstand engineering structures. Materials and Methods: Geophysical techniques involving eight (8) vertical electrical sounding (VES) and Wenner array were carried out with two (2) traverses. Geotechnical investigation involving cone penetration test (CPT) was also carried out. Results: The results obtained were presented as 1D resistivity profiles and Pseudo-sections of 2-D. Three (3) geo-electric layers were delineated within the study area and these comprise of topsoil, peat or clay and silty sand. The CPT results were used in the calculation of bearing capacity using Bustamante and Gianeselli equation for pile foundations and Meyehorf equation to determine the maximum load the materials can withstand respectively. Conclusion: The shallow subsurface geology was adjudged to be mechanically unstable with low penetration resistance values up to the depth of 11m. The methods conformed and confirmed that shallow foundation was considered unsuitable for the intended engineering structure. Keywords: Meyehorf, Bustamante and Gianeselli, Subsurface, Geology, Unstable, Foundation.
尼日利亚拉各斯州拉各斯中部地区的地球物理和岩土工程场地特征
简介:地球物理表征是指与地下特征相关的信息的收集。岩土工程涉及工程结构性能研究,用于获取场地周围土壤和岩石的物理特性信息,以设计拟议结构的土方工程和基础,以及修复由地下条件引起的土方工程和结构的损坏。目的:本研究旨在表征地下地层,以确定其承受工程结构的能力。材料和方法:地球物理技术包括8个垂直电测深(VES)和温纳阵列(Wenner array),并进行了2次穿越。岩土工程勘察包括锥贯试验(CPT)也进行了。结果:得到的结果以一维电阻率剖面和二维伪剖面的形式呈现。在研究区内圈定了3个地电层,包括表土、泥炭或粘土和粉砂。将CPT结果用于承载力计算,分别采用桩基础的Bustamante和Gianeselli方程和Meyehorf方程确定材料所能承受的最大荷载。结论:判定浅层地下地质力学不稳定,直至11m深度的穿透阻力值较低。结果表明,浅基础不适合工程结构。关键词:Meyehorf, Bustamante和Gianeselli,地下,地质,不稳定,基础
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