Deformation and failure mechanism of colluvial landslide under sustained rainfall-a case study of Xinzhan landslide in Tongzi County, China

The failure mechanism of Xinzhan landslide were investigated systematically based on multiple-integrated geotechniques, including field investigations, monitoring, and numerical simulations. Xinzhan landslide is a typical colluvial landslide, composed of gravelly soil in upper part and sandstone int...

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Main Authors: Zhou Ke, Wang Hong, Liao Jianxing, Zhang Yuguang, Chen Fangping, Yang Zhengjun
Format: Article
Language:English
Published: Elsevier 2023-05-01
Series:Alexandria Engineering Journal
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S1110016823002065
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author Zhou Ke
Wang Hong
Liao Jianxing
Zhang Yuguang
Chen Fangping
Yang Zhengjun
author_facet Zhou Ke
Wang Hong
Liao Jianxing
Zhang Yuguang
Chen Fangping
Yang Zhengjun
author_sort Zhou Ke
collection DOAJ
description The failure mechanism of Xinzhan landslide were investigated systematically based on multiple-integrated geotechniques, including field investigations, monitoring, and numerical simulations. Xinzhan landslide is a typical colluvial landslide, composed of gravelly soil in upper part and sandstone interbedded with mudstone in underlying part. The sliding surface is closing to the soil-rock interface with average depth about 8 m and the main sliding direction 287°. The occurrence of Xinzhan landslide is attributed to its unique geological environment and sustained rainfall. The hydro-mechanical coupling results indicate that under sustained rainfall, the rainwater infiltrates into gravelly soil, rising the pressure and forming transient saturation zone near the soil-rock interface, where the strength parameter is weakened under effect of water. As a consequence, the plastic deformation is intensified. Additionally, the deformation evolution trend of landslide under different rainfall intensities is also studied. The results show that the greater rainfall intensity, the shorter rainfall duration required for the landslide to produce accelerated deformation. The rainfall intensity-duration curve is used to construct the critical rainfall early warning criterion of Xinzhan landslide. The R2 of the fitting formula is 0.971, which indicates that the formula can effectively serve the early warning and provide convenience for highway safety construction.
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spelling doaj.art-3e7a467d79584f379bb358f1590ad27b2023-03-25T05:10:26ZengElsevierAlexandria Engineering Journal1110-01682023-05-017189103Deformation and failure mechanism of colluvial landslide under sustained rainfall-a case study of Xinzhan landslide in Tongzi County, ChinaZhou Ke0Wang Hong1Liao Jianxing2Zhang Yuguang3Chen Fangping4Yang Zhengjun5Guizhou Transportation Planning Survey & Design Academe CO.LTD, Guiyang, Guizhou 550081, ChinaGuizhou Transportation Planning Survey & Design Academe CO.LTD, Guiyang, Guizhou 550081, China; College of Civil Engineering, Guizhou University, Guiyang, Guizhou 550025, China; Corresponding author at: Guizhou Transportation Planning Survey & Design Academe CO.LTD, Guiyang, Guizhou 550081, China.College of Civil Engineering, Guizhou University, Guiyang, Guizhou 550025, ChinaGuizhou Transportation Planning Survey & Design Academe CO.LTD, Guiyang, Guizhou 550081, ChinaGuizhou Transportation Planning Survey & Design Academe CO.LTD, Guiyang, Guizhou 550081, ChinaMeteorological Bureau of Tongzi County, Zunyi, Guizhou 563000, ChinaThe failure mechanism of Xinzhan landslide were investigated systematically based on multiple-integrated geotechniques, including field investigations, monitoring, and numerical simulations. Xinzhan landslide is a typical colluvial landslide, composed of gravelly soil in upper part and sandstone interbedded with mudstone in underlying part. The sliding surface is closing to the soil-rock interface with average depth about 8 m and the main sliding direction 287°. The occurrence of Xinzhan landslide is attributed to its unique geological environment and sustained rainfall. The hydro-mechanical coupling results indicate that under sustained rainfall, the rainwater infiltrates into gravelly soil, rising the pressure and forming transient saturation zone near the soil-rock interface, where the strength parameter is weakened under effect of water. As a consequence, the plastic deformation is intensified. Additionally, the deformation evolution trend of landslide under different rainfall intensities is also studied. The results show that the greater rainfall intensity, the shorter rainfall duration required for the landslide to produce accelerated deformation. The rainfall intensity-duration curve is used to construct the critical rainfall early warning criterion of Xinzhan landslide. The R2 of the fitting formula is 0.971, which indicates that the formula can effectively serve the early warning and provide convenience for highway safety construction.http://www.sciencedirect.com/science/article/pii/S1110016823002065Colluvial landslideSustained rainfallFailure mechanismNumerical simulations
spellingShingle Zhou Ke
Wang Hong
Liao Jianxing
Zhang Yuguang
Chen Fangping
Yang Zhengjun
Deformation and failure mechanism of colluvial landslide under sustained rainfall-a case study of Xinzhan landslide in Tongzi County, China
Alexandria Engineering Journal
Colluvial landslide
Sustained rainfall
Failure mechanism
Numerical simulations
title Deformation and failure mechanism of colluvial landslide under sustained rainfall-a case study of Xinzhan landslide in Tongzi County, China
title_full Deformation and failure mechanism of colluvial landslide under sustained rainfall-a case study of Xinzhan landslide in Tongzi County, China
title_fullStr Deformation and failure mechanism of colluvial landslide under sustained rainfall-a case study of Xinzhan landslide in Tongzi County, China
title_full_unstemmed Deformation and failure mechanism of colluvial landslide under sustained rainfall-a case study of Xinzhan landslide in Tongzi County, China
title_short Deformation and failure mechanism of colluvial landslide under sustained rainfall-a case study of Xinzhan landslide in Tongzi County, China
title_sort deformation and failure mechanism of colluvial landslide under sustained rainfall a case study of xinzhan landslide in tongzi county china
topic Colluvial landslide
Sustained rainfall
Failure mechanism
Numerical simulations
url http://www.sciencedirect.com/science/article/pii/S1110016823002065
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