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Application of Vertical Electric Soundings for Foundation Investigation in a Basement Complex Terrain: A case Study of Ijebu Igbo, Southwestern Nigeria

机译:垂直电测深在地下复杂地形基础调查中的应用:以尼日利亚西南部Ijebu Igbo为例

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Vertical Electrical sounding (VES) has been used to study the subsurface lithology of a site for a proposed building in Ijebu Igbo,Southwestern,Nigeria with a view to recommending the appropriate depth to which the foundation could be sited.The area extent of the site was estimated to be 2500m2.Seventeen (17) VES stations were established along three profiles.The Schlumberger electrode array was employed with current electrode spacing AB/2 of 100m.Data collected was plotted and curved matched.The result of the curved matching was used as an input for the computer iteration software.The subsurface layers resistivity,thickness and depth were calculated quantitatively.The results revealed three to four geoelectric layers.These are inferred as topsoil,sandy layer,clayey horizon and basement.The basement rocks were either fresh or weathered.The resistivity of the top soil ranges from 166.7 to 1027.7 flm with depth range of 0.6-1.2m whereas the resistivity of the fresh basement ranges from 1460.7 to 3255.8.ohm-m while that of the weathered basement ranges from 302.8- 752.8ohm-m.Clayey horizon is predominant in the entire area with varying depth of between 3.8m and 10.2m.The presence of clay in the clayey horizon are at varying depth is of concern,this is not too good as engineering materials and need to be further analyzed so as to determine the moisture contents,percentage passing to determine its clay content.The fresh basement at the central part of the site could withstand stress as there was no evidence of structural geological features such as faults which can aid subsidence.This study has provided preliminary information that could guide further studies and foundation design of the proposed building.
机译:垂直电测深(VES)已被用于研究尼日利亚西南部Ijebu Igbo拟建建筑物的场地的地下岩性,以建议基础可被安置的适当深度。估计面积为2500m2。沿着三个剖面建立了十七(17)个VES站,使用Schlumberger电极阵列,当前电极间距AB / 2为100m,绘制了数据并进行曲线匹配,并使用曲线匹配的结果作为计算机迭代软件的输入,对地下层的电阻率,厚度和深度进行了定量计算,结果揭示了三到四个地电层,推断为表层土壤,桑迪层,粘土层和基底。表层土壤的电阻率范围为166.7至1027.7 flm,深度范围为0.6-1.2m,而新鲜地下室的电阻率范围为1 460.7至3255.8ohm-m,风化的地下室的范围为302.8- 752.8ohm-m.Clayey层位在整个区域中占主导地位,深度在3.8m和10.2m之间变化。需要注意的是,在不同深度处,这不是很好的工程材料,需要进一步分析以确定含水量,通过百分比以确定其粘土含量。现场中心的新鲜地下室可以承受压力由于没有证据表明诸如断层之类的结构地质特征可以帮助沉降。本研究提供了初步信息,可以为拟议建筑物的进一步研究和基础设计提供指导。

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