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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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 |
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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.
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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 |
work_keys_str_mv |
AT hungenchen developmentandexaminationofrainfalltriggeredshallowlandslidemodel AT chénhóngēn developmentandexaminationofrainfalltriggeredshallowlandslidemodel AT hungenchen jiàngyǔyǐnfāpōdeqiǎnbēngtāmóshìzhījiànlìyǔtàntǎo AT chénhóngēn jiàngyǔyǐnfāpōdeqiǎnbēngtāmóshìzhījiànlìyǔtàntǎo |
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