Development and Examination of Rainfall-Triggered Shallow Landslide Model

碩士 === 國立交通大學 === 土木工程系所 === 93 === In this study, based on Richards equation and infinite slope stability theory, a rainfall-triggered shallow landslide model is developed and examined. After the developed model is verified, the type and mechanism of failure in steep and mild slopes are investigate...

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Main Authors: Hung-En Chen, 陳弘恩
Other Authors: Jinn-Chuang Yang
Format: Others
Language:zh-TW
Published: 2005
Online Access:http://ndltd.ncl.edu.tw/handle/13664461361833997077
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spelling ndltd-TW-093NCTU50150742016-06-06T04:10:54Z http://ndltd.ncl.edu.tw/handle/13664461361833997077 Development and Examination of Rainfall-Triggered Shallow Landslide Model 降雨引發坡地淺崩塌模式之建立與探討 Hung-En Chen 陳弘恩 碩士 國立交通大學 土木工程系所 93 In this study, based on Richards equation and infinite slope stability theory, a rainfall-triggered shallow landslide model is developed and examined. After the developed model is verified, the type and mechanism of failure in steep and mild slopes are investigated first. The influences of rainfall characters including intensity, duration, and pattern on shallow landslide are then examined. The results show that the failure of steep slope could happen when the soils are unsaturated or saturated. However, the failure of mild slope seems to occur in saturated soils only. Both the decrease of soil suction and the rise of groundwater table caused by rainfall could trigger landslide. The intensity, duration, and pattern of rainfall have significantly influence not only on the occurrence of shallow landslide but also on the depth and time of soil failure. In addition, the sufficient condition of landslide caused by the rise of groundwater table is derived and it could be used in engineering practices. Jinn-Chuang Yang Tung-Lin Tsai 楊錦釧 蔡東霖 2005 學位論文 ; thesis 56 zh-TW
collection NDLTD
language zh-TW
format Others
sources NDLTD
description 碩士 === 國立交通大學 === 土木工程系所 === 93 === In this study, based on Richards equation and infinite slope stability theory, a rainfall-triggered shallow landslide model is developed and examined. After the developed model is verified, the type and mechanism of failure in steep and mild slopes are investigated first. The influences of rainfall characters including intensity, duration, and pattern on shallow landslide are then examined. The results show that the failure of steep slope could happen when the soils are unsaturated or saturated. However, the failure of mild slope seems to occur in saturated soils only. Both the decrease of soil suction and the rise of groundwater table caused by rainfall could trigger landslide. The intensity, duration, and pattern of rainfall have significantly influence not only on the occurrence of shallow landslide but also on the depth and time of soil failure. In addition, the sufficient condition of landslide caused by the rise of groundwater table is derived and it could be used in engineering practices.
author2 Jinn-Chuang Yang
author_facet Jinn-Chuang Yang
Hung-En Chen
陳弘恩
author Hung-En Chen
陳弘恩
spellingShingle Hung-En Chen
陳弘恩
Development and Examination of Rainfall-Triggered Shallow Landslide Model
author_sort Hung-En Chen
title Development and Examination of Rainfall-Triggered Shallow Landslide Model
title_short Development and Examination of Rainfall-Triggered Shallow Landslide Model
title_full Development and Examination of Rainfall-Triggered Shallow Landslide Model
title_fullStr Development and Examination of Rainfall-Triggered Shallow Landslide Model
title_full_unstemmed Development and Examination of Rainfall-Triggered Shallow Landslide Model
title_sort development and examination of rainfall-triggered shallow landslide model
publishDate 2005
url http://ndltd.ncl.edu.tw/handle/13664461361833997077
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