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Integrated approach for pavement deterioration assessments in a low latitude crystalline basement of south-western Nigeria

机译:尼日利亚西南部低纬度结晶基底中路面劣化评估的综合方法

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An integrated approach involving electrical resistivity (ER) technique and geotechnical analysis was employed to assess the deterioration of pavement along Iwo-Osogbo road in south-western Nigeria underlain by quartzo-syenite, migmatite gneiss, and pegmatite crystalline rocks. The ER involved the use of two-dimensional (2D) electrical resistivity tomography and one-dimensional (1D) vertical electrical sounding (VES) to provide an overview of the ground conditions and probe the subsurface profile, respectively. Geotechnical analysis involving compaction, Atterberg limits, grain-size distribution (GSD), and California bearing ratio (CBR) were also carried out on the recovered samples from four test pits, two pits each dug at the smooth and deteriorated pavement portion. Whilst moisture-related distresses originating beneath the pavement were investigated through suction distribution determined from estimated soil-water characteristic curves (SWCC) employing physico-empirical model approach. At the deteriorated pavement segment; the 2D pseudosection indicated the material at and nearsurface (depth less than 2.49 m) was of low resistivity values ranging between 69 and 153 Xm, with upper bound values near surface. The resistivity further decreases with depth indicating increase in proportion of clay and or water content. The other half of the pseudosection is characterized by relatively high resistive material whose resistivity values ranged between 103 and 227 Xm at and near surface (depth less than 1.27 m) as well as alternating bands of low (20 to 70 Xm) and relatively high resistivity (103 to 337 Xm) materials of varied thickness at greater depths. Conversely, the pseudosection obtained from the smooth pavement segment was characterised by high resistivity ([ 212 Xm) at and near surface (depth B3.5 m) over the entire length. Iterative interpretation of 1D VES data indicated three to four layers earth model without association or relationship between a particular apparent resistivity curve type and deteriorated or stable portion of the road. The moisture content and Atterberg limit parameters namely plastic limit and liquid limit plots against depth suggest the soil environment beneath the pavement as unsaturated. The GSD curves indicate the soils are gapgraded comprising sand-sized and coarse particle and corroborated by GSD curve fitting. The CBR under soaked condition ranged from 16.5 to 41.1 % indicating that the subbase soil could not withstand much load. The CBR varied between 20.8 and 72.0 % indicating that the subgrade soils have a relatively medium strength whilst the subbase soil has a very high strength. The SWCCs generally indicated that the moisture content decreases with increasing matric suction resulting in suction gradient capable of generating flow. Thus, the pavement deterioration could be attributed to improper handling of the flow initiated by the suction gradient.
机译:采用包括电阻率(ER)技术和岩土工程分析的综合方法来评估尼日利亚西南部Iwo-Osogbo公路沿线的路面变质情况,其中石英-石英岩,硅镁铁矿片麻岩和伟晶岩晶体岩石在其中。急诊室涉及使用二维(2D)电阻率层析成像和一维(1D)垂直电测深(VES)来分别提供地面状况的概述和探测地下剖面。还对从四个试验坑中回收的样品进行了压实,Atterberg极限,粒度分布(GSD)和加利福尼亚承载比(CBR)的岩土分析,其中两个坑均在光滑且恶化的路面部分挖出。同时通过物理经验模型方法通过从估计的土壤-水特征曲线(SWCC)确定的吸力分布来研究源自人行道下方的与水分有关的困扰。在恶化的人行道段; 2D假剖面表明,在地表及其附近(深度小于2.49 m)的材料的电阻率值范围在69至153 Xm之间,在地表附近具有上限。电阻率随深度进一步降低,表明粘土和/或水含量的比例增加。伪截面的另一半的特点是电阻率较高的材料,其在和靠近表面(深度小于1.27 m)的电阻率值在103至227 Xm之间,并且交替出现低电阻率带(20至70 Xm)和较高的电阻率(103至337 Xm)厚度更大的材料。相反,从光滑的路面段获得的假剖面的特征是在整个长度范围内和近表面(深度B3.5 m)处具有高电阻率([212 Xm])。一维VES数据的迭代解释表明,三至四层地球模型在特定的视电阻率曲线类型与道路的恶化或稳定部分之间没有关联或关系。水分含量和阿特伯格极限参数,即塑性极限和液体极限曲线与深度的关系图表明,人行道下方的土壤环境为非饱和土壤。 GSD曲线表明土壤是由砂级和粗颗粒组成的间隙梯度,并通过GSD曲线拟合得到了证实。浸泡条件下的CBR为16.5%至41.1%,这表明基础土壤不能承受很大的载荷。 CBR在20.8%至72.0%之间变化,表明路基土壤具有相对中等的强度,而路基土壤具有非常高的强度。 SWCC通常指示水分含量随着基质吸力的增加而降低,从而导致能够产生流量的吸力梯度。因此,路面劣化可能归因于对吸力梯度引发的流量的不正确处理。

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