Land satellite imagery and integrated geophysical investigations of highway pavement instability in southwestern Nigeria

IF 0.4 Q4 ENVIRONMENTAL SCIENCES Geology, Geophysics and Environment Pub Date : 2020-10-16 DOI:10.7494/geol.2020.46.2.135
O. Ademila, A. I. Olayinka, M. Oladunjoye
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引用次数: 9

Abstract

The high global numbers of road accidents due to bad roads and the failure of other engineering structures have necessitated this study, particularly as road transport accounts for a higher percentage of cargo movement in African countries. The geophysical investigation was carried out on six failed and two stable sections along the Ibadan-Iwo-Osogbo highway to examine the geological factors responsible for highway failure in the area. A Landsat ETM+ (Enhanced Thematic Mapper Plus) imagery of the study area and its environs was acquired and processed for lineaments analyses. Magnetic, Very Low Frequency Electromagnetic (VLF-EM) and electrical resistivity methods involving Schlumberger Vertical Electrical Sounding (VES) and 2-D imaging using a dipole- dipole array were utilized. Lineaments were identified across failed localities. Lateral magnetic variations in the near-surface geological materials characterized the study area. The 2-D VLF-EM models generated showed conductive zones corresponding to fractured zones of conductive clay materials within the basement rocks. Subgrade soils below the highway pavement along the failed sections are typical of incompetent clayey and sandy clay/clayey sand formations with resistivity values between 20–475 Ω∙m. In comparison, the subgrade soil beneath the stable sections has moderate to high resistivity values of 196–616 Ω∙m. 2-D resistivity structures across the failed segments identified low resistivity water-absorbing clay and lithological contacts. Water absorbing, clay enriched subgrade soils and the identified near-surface linear conductive features are the major geologic factors, and poor drainage network resulted in the highway failure. Remote sensing and geophysical investigations of the geological sequence and structures underlying the highway should be carried out before construction to effectively complement the routine geotechnical studies to ensure the sustainability of road  nfrastructure.
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尼日利亚西南部公路路面不稳定性的陆地卫星图像和综合地球物理调查
由于道路状况不佳和其他工程结构损坏造成的全球道路事故数量众多,因此有必要进行这项研究,特别是因为公路运输在非洲国家的货物运输中所占的百分比较高。对伊巴丹-伊沃-奥索博高速公路沿线的6段破坏路段和2段稳定路段进行了地球物理调查,以研究造成该地区公路破坏的地质因素。获取了研究区及其周边地区的Landsat ETM+ (Enhanced Thematic Mapper Plus)图像,并对其进行了处理以进行地形分析。利用斯伦贝谢垂直电测深(VES)和利用偶极子-偶极子阵列进行二维成像的磁性、甚低频电磁(VLF-EM)和电阻率方法。在失败的地方确定了轮廓。研究区近地表地质物质的横向磁性变化特征。建立的二维VLF-EM模型显示,导电带对应于基底岩石内导电粘土材料的断裂带。沿破坏路段的公路路面以下路基土为典型的不合格粘土和砂质粘土/粘土砂层,电阻率在20-475 Ω∙m之间。稳定断面下的路基土电阻率为196 ~ 616 Ω∙m,为中高电阻率。破坏段的二维电阻率结构确定了低电阻率吸水粘土和岩性接触层。吸水性强、富含粘土的路基土和已识别的近地表线状导电特征是导致公路破坏的主要地质因素,排水网络不良是导致公路破坏的主要原因。在施工前应对公路的地质层序和结构进行遥感和地球物理调查,以有效补充常规的岩土工程研究,以确保道路基础设施的可持续性。
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