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首页> 外文期刊>International Journal of Environmental Monitoring and Analysis >2D Electrical Resistivity Imaging (ERI) for Subsurface Evaluation of a Pre-engineering Construction Site in Akure, Southwestern Nigeria
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2D Electrical Resistivity Imaging (ERI) for Subsurface Evaluation of a Pre-engineering Construction Site in Akure, Southwestern Nigeria

机译:2D电阻率成像(ERI)用于尼日利亚西南部教育前工程施工现场的地下评估

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2D electrical resistivity imaging (ERI) and vertical electrical sounding (VES) were integrated to map the subsurface lithology at a pre-engineering construction site in Akure, southwestern Nigeria, in order to ascertain the competence and suitability of the site for engineering structures. Four 2D horizontal profiling (Wenner array) was used to qualitatively study and interprete the geoinformation of the lithological nature of each geoelectric layer within the study site. Four vertical electrical sounding were also conducted using Schlunberger configuration. The VES data were processed and inverted using master curves and WinResist computer software, while the 2D inversion was done using Diprowin. The results of the 2D horizontal profiling revealed that the study area is composed of four subsurface geo-electric layers with resistivities ranging between 6.91Ωm to 93.6Ωm. These results revealed an expansive clay formation to the depth probed. While the VES results showed a three subsurface geo-electric layers with resistivities ranging between 8.4Ωm to 640Ωm with the second layers where the foundation is supposed to be laid confirmed the presence of clay with resistivities ranging between 8.4Ωm to 13.0Ωm with depth ranging between 4.9m to 7.9m. The results revealed the site to be an expansive clay formation and showed that shallow foundation may not be feasible or advisable for massive engineering structures because of the presence of clay materials in the area. But small or light engineering structures may be recommended.
机译:2D电阻率成像(ERI)和垂直电气探测(VES)集成在尼日利亚西南部的Akure预工程建筑工地上映射地下岩性,以确定现场为工程结构的能力和适用性。四个2D水平分析(Wenner阵列)用于定性地研究和解释研究部位内每个地电层的岩性性质的地理信息。还使用Schlunberger配置进行了四种垂直电气探测。使用主曲线和WinResist计算机软件处理和反转VES数据,而使用Diprowin完成2D反演。 2D水平分析的结果显示,研究区域由四个地下地质电层组成,电阻率在6.91Ωm至93.6Ωm之间。这些结果揭示了深度探测的膨胀性粘土形成。虽然VES结果显示了具有电阻性的三个地下地质电层,其电阻率在8.4Ωm至640Ωm之间,第二层被铺设的第二层确认了在8.4Ωm至13.0Ωm之间的电阻率的粘土的存在,深度范围4.9m至7.9m。结果表明,该部位是一种膨胀的粘土形成,并表明由于该地区存在粘土材料,浅基础可能是不可行的或可取的巨大工程结构。但是可能推荐小或轻的工程结构。

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