The effects of internal erosion on granular soils used in transport embankments

IF 3.3 2区 工程技术 Q2 ENGINEERING, GEOLOGICAL
I. Johnston , W. Murphy , J. Holden
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Abstract

The flooding of embankments used for rail and other infrastructure has the potential to cause lasting weakening of slopes via the movement of fine particles induced by seepage. In laboratory experiments, internal erosion was induced in granular soil samples, with properties consistent with those used to construct transportation embankments, to assess how particle migration through, and out of, samples caused shear wave velocity, strength, stiffness and permeability changes. Shear wave velocity changes, measured using horizontal bender elements, of up to 19 % were observed following fine particle removal of up to 1 % of initial sample mass. Shear wave velocity change was found to be an indicator for identifying the development of permeability change during seepage-induced particle migration. Median measured permeability changes were +5 % and −34 % for samples containing 15 % and 30 % fines, respectively. The largest directly observed permeability and shear wave velocity changes occurred during the initial stages of seepage. Negative correlation was observed between mass of material removed from samples and peak friction angle. Following seepage, soils displayed a dual stiffness behaviour. Stiffness and strength changes were attributed to redistribution of fine particles and opening of pore spaces. Our results have implications for the monitoring of earthworks affected by flooding and seepage as the associated redistribution of fine particles may lead to large changes in slope properties.

内侵蚀对用于运输路堤的颗粒土的影响
用于铁路和其他基础设施的路堤被水淹没后,细颗粒可能会因渗流引起的移动而导致斜坡的持久削弱。在实验室实验中,我们在颗粒土样本中诱导了内部侵蚀,这些样本的性质与用于建造运输路堤的样本一致,目的是评估颗粒在样本中的迁移如何引起剪切波速度、强度、刚度和渗透性的变化。使用水平弯管元件测量剪切波速,观察到细颗粒移出后的剪切波速变化高达 19%,而移出的细颗粒占初始样品质量的 1%。研究发现,剪切波速度变化是确定渗流诱导颗粒迁移过程中渗透性变化发展的一个指标。对于含有 15% 和 30% 细颗粒的样品,测得的渗透率变化中值分别为 +5% 和 -34%。直接观测到的最大渗透率和剪切波速度变化发生在渗流的初始阶段。从样本中移除的材料质量与摩擦角峰值之间呈负相关。渗流后,土壤显示出双重刚度行为。刚度和强度的变化归因于细颗粒的重新分布和孔隙的打开。我们的研究结果对监测受洪水和渗水影响的土方工程具有重要意义,因为相关的细颗粒重新分布可能会导致边坡特性发生巨大变化。
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来源期刊
Soils and Foundations
Soils and Foundations 工程技术-地球科学综合
CiteScore
6.40
自引率
8.10%
发文量
99
审稿时长
5 months
期刊介绍: Soils and Foundations is one of the leading journals in the field of soil mechanics and geotechnical engineering. It is the official journal of the Japanese Geotechnical Society (JGS)., The journal publishes a variety of original research paper, technical reports, technical notes, as well as the state-of-the-art reports upon invitation by the Editor, in the fields of soil and rock mechanics, geotechnical engineering, and environmental geotechnics. Since the publication of Volume 1, No.1 issue in June 1960, Soils and Foundations will celebrate the 60th anniversary in the year of 2020. Soils and Foundations welcomes theoretical as well as practical work associated with the aforementioned field(s). Case studies that describe the original and interdisciplinary work applicable to geotechnical engineering are particularly encouraged. Discussions to each of the published articles are also welcomed in order to provide an avenue in which opinions of peers may be fed back or exchanged. In providing latest expertise on a specific topic, one issue out of six per year on average was allocated to include selected papers from the International Symposia which were held in Japan as well as overseas.
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