Stability analyses of residual soil slope under different rainfall conditions

Climate change contributes to the changes in rainfall patterns. Many areas are experiencing a larger amount of rainfall with a higher intensity. It results in an increase in the frequency of rainfall-induced slope failures. In geotechnical engineering practice, the rainfall loading can be considered...

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Main Author: Jing, Yannan
Other Authors: Harianto Rahardjo
Format: Final Year Project
Language:English
Published: Nanyang Technological University 2019
Subjects:
Online Access:https://hdl.handle.net/10356/136534
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Institution: Nanyang Technological University
Language: English
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spelling sg-ntu-dr.10356-1365342019-12-26T05:07:04Z Stability analyses of residual soil slope under different rainfall conditions Jing, Yannan Harianto Rahardjo School of Civil and Environmental Engineering CHRAHARDJO@ntu.edu.sg Engineering Engineering::Civil engineering::Geotechnical Climate change contributes to the changes in rainfall patterns. Many areas are experiencing a larger amount of rainfall with a higher intensity. It results in an increase in the frequency of rainfall-induced slope failures. In geotechnical engineering practice, the rainfall loading can be considered as a parameter in triggering slope failure. However, limited studies have been conducted to identify the influence of the increase in rainfall intensity and rainfall duration due to climate change on the stability of residual soil slopes. Therefore, the objective of this project is to study the stability of residual soil slopes with different soil-water characteristic curves (SWCCs) and unsaturated shear strengths under different rainfall conditions. The scope of the project involved measurements of SWCC, saturated permeability, saturated and unsaturated shear strength of residual soils from Old Alluvium and Jurong Formation. In addition, 2-D seepage and stability analyses of unsaturated residual soil slopes were performed to investigate the variations of Factor of Safety (FoS) with respect to different rainfall conditions. The results of the study indicated the decreasing rate in FoS of the slope from Old Alluvium was higher as compared to the rate of decrease in FoS of the slope from sedimentary Jurong Formation. This was attributed to the higher permeability of the residual soil from Old Alluvium. In addition, the rate of recovery in FoS of the slope from sedimentary Jurong Formation was lower than that of the slope from Old Alluvium after rainfall stopped. Bachelor of Engineering (Civil) 2019-12-26T05:07:04Z 2019-12-26T05:07:04Z 2019 Final Year Project (FYP) https://hdl.handle.net/10356/136534 en application/pdf Nanyang Technological University
institution Nanyang Technological University
building NTU Library
country Singapore
collection DR-NTU
language English
topic Engineering
Engineering::Civil engineering::Geotechnical
spellingShingle Engineering
Engineering::Civil engineering::Geotechnical
Jing, Yannan
Stability analyses of residual soil slope under different rainfall conditions
description Climate change contributes to the changes in rainfall patterns. Many areas are experiencing a larger amount of rainfall with a higher intensity. It results in an increase in the frequency of rainfall-induced slope failures. In geotechnical engineering practice, the rainfall loading can be considered as a parameter in triggering slope failure. However, limited studies have been conducted to identify the influence of the increase in rainfall intensity and rainfall duration due to climate change on the stability of residual soil slopes. Therefore, the objective of this project is to study the stability of residual soil slopes with different soil-water characteristic curves (SWCCs) and unsaturated shear strengths under different rainfall conditions. The scope of the project involved measurements of SWCC, saturated permeability, saturated and unsaturated shear strength of residual soils from Old Alluvium and Jurong Formation. In addition, 2-D seepage and stability analyses of unsaturated residual soil slopes were performed to investigate the variations of Factor of Safety (FoS) with respect to different rainfall conditions. The results of the study indicated the decreasing rate in FoS of the slope from Old Alluvium was higher as compared to the rate of decrease in FoS of the slope from sedimentary Jurong Formation. This was attributed to the higher permeability of the residual soil from Old Alluvium. In addition, the rate of recovery in FoS of the slope from sedimentary Jurong Formation was lower than that of the slope from Old Alluvium after rainfall stopped.
author2 Harianto Rahardjo
author_facet Harianto Rahardjo
Jing, Yannan
format Final Year Project
author Jing, Yannan
author_sort Jing, Yannan
title Stability analyses of residual soil slope under different rainfall conditions
title_short Stability analyses of residual soil slope under different rainfall conditions
title_full Stability analyses of residual soil slope under different rainfall conditions
title_fullStr Stability analyses of residual soil slope under different rainfall conditions
title_full_unstemmed Stability analyses of residual soil slope under different rainfall conditions
title_sort stability analyses of residual soil slope under different rainfall conditions
publisher Nanyang Technological University
publishDate 2019
url https://hdl.handle.net/10356/136534
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