FOUNDATION CHARACTERIZATION IN IKATE AREA SOUTHWESTERN NIGERIA USING ELECTRICAL RESISTIVITY TOMOGRAPHY AND CONE PENETRATION TEST

O. E. Faseki, Anthony, O. Ademeso, Kehinde, I. Adebayo, Oladapo Olasunkanmi, Thomas, B. Omoyajowo
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Abstract

The establishments of the nexus between the underlying geology and engineering properties are fundamentals to the safe, economic and serviceable designs of civil engineering structures. Cone Penetration Test (CPT) and Electrical Resistivity Tomography (ERT) are critical tools in foundation parameterization especially within Quaternary sediments serving as foundation of engineering structures. Both techniques were used to obtained point data and lateral continuity of geologic units within Ikate Area of Lagos Metropolis for foundation parameterization. Measurements which comprising 4 profiles of 2D resistivity imaging using the Wenner electrode configuration; 1 borehole and 12 cone penetration tests (CPT) were taken with Pasi Terrameter, percussion rig and the 10.0 tons penetrometer respectively. The ERT results interpreted using Dipro software were presented in Pseudo-sections while the cone penetration test results analysed with Microsoft Excel were represented as resistance curves. Interpretation from the two methods integrated with the borehole results reveals the presence clay, peat and sand of varying properties. The uppermost layer consists of medium dense sand followed by clay/peat of very low resistivity (< 3.5 ohm-meter) covering about 6. 0 – 8.0m in depth and terminating in another layer of sand (8.0 – 15.0m). The last sandy layer with cone resistance range between 30 – 120kg/cm2 is considered a suitable layer upon which deep foundation may be founded. Shallow foundation capacity estimates at depths 0.2 – 4.0m derived from direct CPT data using three different computation techniques gives value range from 1.7 – 49.4kg/cm2, 0.7 – 15.2kg/cm2 and 0.4 – 12.6kg/cm2 respectively. Deep foundation for skyscrapers within the area are advised to be founded within the competent layer encountered beyond 10.m depth.
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利用电阻率层析成像和锥形穿透测试在尼日利亚西南部ikate地区进行地基表征
建立基础地质和工程特性之间的联系是土木工程结构安全、经济和使用设计的基础。圆锥贯入试验(CPT)和电阻率层析成像(ERT)是基础参数化的重要工具,特别是在作为工程结构基础的第四纪沉积物中。利用这两种技术获取了拉各斯大都市Ikate地区的点数据和地质单元的横向连续性,用于基础参数化。测量包括使用温纳电极配置的4个二维电阻率成像剖面;分别用Pasi Terrameter、冲击钻机和10.0吨贯深仪进行了1个孔和12个锥体贯深试验。用Dipro软件解释的ERT结果用伪截面表示,用Microsoft Excel分析的锥突测试结果用阻力曲线表示。结合钻孔结果,两种方法的解释表明存在不同性质的粘土、泥炭和砂。最上层由中密度砂组成,其次是极低电阻率(< 3.5欧姆-米)的粘土/泥炭,覆盖约6。深度为0 - 8.0m,止于另一层砂(8.0 - 15.0m)。圆锥阻力在30 - 120kg/cm2之间的最后一层砂质层被认为是建立深基础的合适层。根据直接CPT数据,使用三种不同的计算技术估算深度为0.2 - 4.0m的浅基础承载力,其取值范围分别为1.7 - 49.4kg/cm2、0.7 - 15.2kg/cm2和0.4 - 12.6kg/cm2。区域内摩天大楼的深地基建议建立在超过10层的主管层内。米深度。
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