Model Experimental Study on Stress Transfer and Redistribution in a Clay Landslide under Surcharge Load

Stress transfer and redistribution always accompany with the evolution of landslides. However, previous literature studies have mainly focused on stages of stress variation, and far too little attention has been paid to detailed transfer and redistribution process analysis on stress variation. In th...

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Main Authors: Heng-Jun Hou, Bo Wang, Quan-Xiang Deng, Zheng-Wei Zhu, Feng Xiao
Format: Article
Language:English
Published: Wiley 2020-01-01
Series:Advances in Materials Science and Engineering
Online Access:http://dx.doi.org/10.1155/2020/4269043
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author Heng-Jun Hou
Bo Wang
Quan-Xiang Deng
Zheng-Wei Zhu
Feng Xiao
author_facet Heng-Jun Hou
Bo Wang
Quan-Xiang Deng
Zheng-Wei Zhu
Feng Xiao
author_sort Heng-Jun Hou
collection DOAJ
description Stress transfer and redistribution always accompany with the evolution of landslides. However, previous literature studies have mainly focused on stages of stress variation, and far too little attention has been paid to detailed transfer and redistribution process analysis on stress variation. In this paper, a large-scale clay model slope with masonry slide bed and prefabricated cambered slip surface was constructed. Earth pressure cells were embedded into slip mass to monitor vertical and horizontal stresses in different parts of the test soils under the set load sequence. Stress transfer efficiency (STE) indicators based on qualified stress monitoring datasets (tested by Shapiro-Wilk method) were established to quantify the stress transfer process. Staged development of stress inside the clay slope was analyzed through extracting slopes of stress curves and limit loads. The stress redistribution process was analyzed using STE and deflection of stress isolines derived from numerical simulation. Moreover, to study the influence of loading position on stress variation, geometry partitioning has also been discussed. Results showed that vertical and horizontal stresses had different growth trends on both sides of 80 kN and 60 kN, respectively. Horizontal stress growth has two stages; vertical stress growth has two stages in soils close to slope surface and shear outlet, while there are three stages in other soils. Vertical stress transfer efficiency (VSTE) and horizontal stress transfer efficiency (HSTE) are recommended to quantify stress transfer and redistribution process. Based on VSTEs and HSTEs, the slip mass could be partitioned into three parts: loading zone, transfer zone, and free zone. Deflecting amplitudes of stress isolines were in consistency with the results revealed by STEs.
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spelling doaj-art-455d03c7daee427989408debeeaf4afa2025-08-20T03:36:44ZengWileyAdvances in Materials Science and Engineering1687-84341687-84422020-01-01202010.1155/2020/42690434269043Model Experimental Study on Stress Transfer and Redistribution in a Clay Landslide under Surcharge LoadHeng-Jun Hou0Bo Wang1Quan-Xiang Deng2Zheng-Wei Zhu3Feng Xiao4School of Civil Engineering of Chongqing University, Chongqing 400045, ChinaSchool of Civil Engineering of Chongqing University, Chongqing 400045, ChinaSchool of Civil Engineering of Chongqing University, Chongqing 400045, ChinaSchool of Civil Engineering of Chongqing University, Chongqing 400045, ChinaSchool of Civil Engineering of Chongqing University, Chongqing 400045, ChinaStress transfer and redistribution always accompany with the evolution of landslides. However, previous literature studies have mainly focused on stages of stress variation, and far too little attention has been paid to detailed transfer and redistribution process analysis on stress variation. In this paper, a large-scale clay model slope with masonry slide bed and prefabricated cambered slip surface was constructed. Earth pressure cells were embedded into slip mass to monitor vertical and horizontal stresses in different parts of the test soils under the set load sequence. Stress transfer efficiency (STE) indicators based on qualified stress monitoring datasets (tested by Shapiro-Wilk method) were established to quantify the stress transfer process. Staged development of stress inside the clay slope was analyzed through extracting slopes of stress curves and limit loads. The stress redistribution process was analyzed using STE and deflection of stress isolines derived from numerical simulation. Moreover, to study the influence of loading position on stress variation, geometry partitioning has also been discussed. Results showed that vertical and horizontal stresses had different growth trends on both sides of 80 kN and 60 kN, respectively. Horizontal stress growth has two stages; vertical stress growth has two stages in soils close to slope surface and shear outlet, while there are three stages in other soils. Vertical stress transfer efficiency (VSTE) and horizontal stress transfer efficiency (HSTE) are recommended to quantify stress transfer and redistribution process. Based on VSTEs and HSTEs, the slip mass could be partitioned into three parts: loading zone, transfer zone, and free zone. Deflecting amplitudes of stress isolines were in consistency with the results revealed by STEs.http://dx.doi.org/10.1155/2020/4269043
spellingShingle Heng-Jun Hou
Bo Wang
Quan-Xiang Deng
Zheng-Wei Zhu
Feng Xiao
Model Experimental Study on Stress Transfer and Redistribution in a Clay Landslide under Surcharge Load
Advances in Materials Science and Engineering
title Model Experimental Study on Stress Transfer and Redistribution in a Clay Landslide under Surcharge Load
title_full Model Experimental Study on Stress Transfer and Redistribution in a Clay Landslide under Surcharge Load
title_fullStr Model Experimental Study on Stress Transfer and Redistribution in a Clay Landslide under Surcharge Load
title_full_unstemmed Model Experimental Study on Stress Transfer and Redistribution in a Clay Landslide under Surcharge Load
title_short Model Experimental Study on Stress Transfer and Redistribution in a Clay Landslide under Surcharge Load
title_sort model experimental study on stress transfer and redistribution in a clay landslide under surcharge load
url http://dx.doi.org/10.1155/2020/4269043
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