Progressive Formation of Retrogressive Landslide and the Lateral Length of Instability
Retrogressive landslide is caused by the lower rock mass sliding, so that the upper part loses support, is deformed, and starts to slide. In the process of highway construction, the incised slope often leads to retrogressive landslide, and the determination of the damage range of retrogressive lands...
Main Authors: | , , , , , , , |
---|---|
Format: | Article |
Language: | English |
Published: |
MDPI AG
2023-01-01
|
Series: | Applied Sciences |
Subjects: | |
Online Access: | https://www.mdpi.com/2076-3417/13/2/799 |
_version_ | 1797446706028085248 |
---|---|
author | Xiongpeng Zhu Linglin Xie Yi Tang Yifan Chen Huihua Hu Guangyin Lu Changfu Chen Hang Lin |
author_facet | Xiongpeng Zhu Linglin Xie Yi Tang Yifan Chen Huihua Hu Guangyin Lu Changfu Chen Hang Lin |
author_sort | Xiongpeng Zhu |
collection | DOAJ |
description | Retrogressive landslide is caused by the lower rock mass sliding, so that the upper part loses support, is deformed, and starts to slide. In the process of highway construction, the incised slope often leads to retrogressive landslide, and the determination of the damage range of retrogressive landslide is of great significance for the control of the slope. Taking a highway retrogressive landslide in Hunan Province as the research object, the particle flow discrete element is used to numerically simulate the entire failure process of the slope. According to the complex geological conditions of the slope, the rock mass of each part of the slope model is divided, the displacement of key parts of the landslide is monitored, the whole failure process of the retrogressive landslide is simulated, and the lateral length of traction instability is calculated through the stability theory of the sliding pull-crack failure slope. The research shows that the incised slope is the root cause of the retrogressive landslide, and the rainfall is the direct cause. When the retrogressive landslide is treated in engineering practice, the lateral length of traction instability can be obtained according to the stability theory of the sliding pull-crack failure slope, to realize the accurate judgment of the traction failure range of the sliding body. |
first_indexed | 2024-03-09T13:45:25Z |
format | Article |
id | doaj.art-a6148da9f34c4c7b97363aab13add275 |
institution | Directory Open Access Journal |
issn | 2076-3417 |
language | English |
last_indexed | 2024-03-09T13:45:25Z |
publishDate | 2023-01-01 |
publisher | MDPI AG |
record_format | Article |
series | Applied Sciences |
spelling | doaj.art-a6148da9f34c4c7b97363aab13add2752023-11-30T21:01:36ZengMDPI AGApplied Sciences2076-34172023-01-0113279910.3390/app13020799Progressive Formation of Retrogressive Landslide and the Lateral Length of InstabilityXiongpeng Zhu0Linglin Xie1Yi Tang2Yifan Chen3Huihua Hu4Guangyin Lu5Changfu Chen6Hang Lin7School of Resources and Safety Engineering, Central South University, Changsha 410083, ChinaHunan Provincial Communications Planning, Survey and Design Institute, Changsha 410200, ChinaSchool of Resources and Safety Engineering, Central South University, Changsha 410083, ChinaSchool of Resources and Safety Engineering, Central South University, Changsha 410083, ChinaSchool of Resources and Safety Engineering, Central South University, Changsha 410083, ChinaSchool of Geosciences and Info-Physics, Central South University, Changsha 410083, ChinaSchool of Civil Engineering, Hunan University, Changsha 410082, ChinaSchool of Resources and Safety Engineering, Central South University, Changsha 410083, ChinaRetrogressive landslide is caused by the lower rock mass sliding, so that the upper part loses support, is deformed, and starts to slide. In the process of highway construction, the incised slope often leads to retrogressive landslide, and the determination of the damage range of retrogressive landslide is of great significance for the control of the slope. Taking a highway retrogressive landslide in Hunan Province as the research object, the particle flow discrete element is used to numerically simulate the entire failure process of the slope. According to the complex geological conditions of the slope, the rock mass of each part of the slope model is divided, the displacement of key parts of the landslide is monitored, the whole failure process of the retrogressive landslide is simulated, and the lateral length of traction instability is calculated through the stability theory of the sliding pull-crack failure slope. The research shows that the incised slope is the root cause of the retrogressive landslide, and the rainfall is the direct cause. When the retrogressive landslide is treated in engineering practice, the lateral length of traction instability can be obtained according to the stability theory of the sliding pull-crack failure slope, to realize the accurate judgment of the traction failure range of the sliding body.https://www.mdpi.com/2076-3417/13/2/799retrogressive landslideprogressive formationrock slopelateral length of instability |
spellingShingle | Xiongpeng Zhu Linglin Xie Yi Tang Yifan Chen Huihua Hu Guangyin Lu Changfu Chen Hang Lin Progressive Formation of Retrogressive Landslide and the Lateral Length of Instability Applied Sciences retrogressive landslide progressive formation rock slope lateral length of instability |
title | Progressive Formation of Retrogressive Landslide and the Lateral Length of Instability |
title_full | Progressive Formation of Retrogressive Landslide and the Lateral Length of Instability |
title_fullStr | Progressive Formation of Retrogressive Landslide and the Lateral Length of Instability |
title_full_unstemmed | Progressive Formation of Retrogressive Landslide and the Lateral Length of Instability |
title_short | Progressive Formation of Retrogressive Landslide and the Lateral Length of Instability |
title_sort | progressive formation of retrogressive landslide and the lateral length of instability |
topic | retrogressive landslide progressive formation rock slope lateral length of instability |
url | https://www.mdpi.com/2076-3417/13/2/799 |
work_keys_str_mv | AT xiongpengzhu progressiveformationofretrogressivelandslideandthelaterallengthofinstability AT linglinxie progressiveformationofretrogressivelandslideandthelaterallengthofinstability AT yitang progressiveformationofretrogressivelandslideandthelaterallengthofinstability AT yifanchen progressiveformationofretrogressivelandslideandthelaterallengthofinstability AT huihuahu progressiveformationofretrogressivelandslideandthelaterallengthofinstability AT guangyinlu progressiveformationofretrogressivelandslideandthelaterallengthofinstability AT changfuchen progressiveformationofretrogressivelandslideandthelaterallengthofinstability AT hanglin progressiveformationofretrogressivelandslideandthelaterallengthofinstability |