Development of Quasi-3D Slope Stability Model Associated with Groundwater Level Variations

碩士 === 國立交通大學 === 土木工程系所 === 101 === The purpose of this study is to develop a quasi-three-dimensional slope stability model based on limit equilibrium method for overcoming the huge computational effort and taking realistic conditions into consideration. The rainfall infiltration and groundwater le...

Full description

Bibliographic Details
Main Authors: Hwang, Ya-Wen, 黃亞雯
Other Authors: Yang, Jinn-Chuang
Format: Others
Language:zh-TW
Published: 2013
Online Access:http://ndltd.ncl.edu.tw/handle/2ns936
id ndltd-TW-101NCTU5015068
record_format oai_dc
spelling ndltd-TW-101NCTU50150682019-05-15T21:13:33Z http://ndltd.ncl.edu.tw/handle/2ns936 Development of Quasi-3D Slope Stability Model Associated with Groundwater Level Variations 考慮地下水位變化之擬似三維邊坡穩定模式之建立 Hwang, Ya-Wen 黃亞雯 碩士 國立交通大學 土木工程系所 101 The purpose of this study is to develop a quasi-three-dimensional slope stability model based on limit equilibrium method for overcoming the huge computational effort and taking realistic conditions into consideration. The rainfall infiltration and groundwater level variation were simulated by solving the Green-Ampt theory and the one-dimensional Boussinesq equation for sloping aquifer simultaneously. The three-dimensional system was divided into several two-dimensional layers. The stability of each layer was analyzed by using the simplified Bishop method. The three-dimensional stability condition with rainfall infiltration over time was therefore calculated by employing a weighted procedure where weighting was based upon arc-length or area of each layer. Under neglecting lateral flows, the effects of soil permeability, rainfall characters, rainfall patterns, inclined angle of rock layer, topography and soil properties on slope stability were discussed. Yang, Jinn-Chuang Chiang, Shih-Wei 楊錦釧 姜世偉 2013 學位論文 ; thesis 62 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 === 101 === The purpose of this study is to develop a quasi-three-dimensional slope stability model based on limit equilibrium method for overcoming the huge computational effort and taking realistic conditions into consideration. The rainfall infiltration and groundwater level variation were simulated by solving the Green-Ampt theory and the one-dimensional Boussinesq equation for sloping aquifer simultaneously. The three-dimensional system was divided into several two-dimensional layers. The stability of each layer was analyzed by using the simplified Bishop method. The three-dimensional stability condition with rainfall infiltration over time was therefore calculated by employing a weighted procedure where weighting was based upon arc-length or area of each layer. Under neglecting lateral flows, the effects of soil permeability, rainfall characters, rainfall patterns, inclined angle of rock layer, topography and soil properties on slope stability were discussed.
author2 Yang, Jinn-Chuang
author_facet Yang, Jinn-Chuang
Hwang, Ya-Wen
黃亞雯
author Hwang, Ya-Wen
黃亞雯
spellingShingle Hwang, Ya-Wen
黃亞雯
Development of Quasi-3D Slope Stability Model Associated with Groundwater Level Variations
author_sort Hwang, Ya-Wen
title Development of Quasi-3D Slope Stability Model Associated with Groundwater Level Variations
title_short Development of Quasi-3D Slope Stability Model Associated with Groundwater Level Variations
title_full Development of Quasi-3D Slope Stability Model Associated with Groundwater Level Variations
title_fullStr Development of Quasi-3D Slope Stability Model Associated with Groundwater Level Variations
title_full_unstemmed Development of Quasi-3D Slope Stability Model Associated with Groundwater Level Variations
title_sort development of quasi-3d slope stability model associated with groundwater level variations
publishDate 2013
url http://ndltd.ncl.edu.tw/handle/2ns936
work_keys_str_mv AT hwangyawen developmentofquasi3dslopestabilitymodelassociatedwithgroundwaterlevelvariations
AT huángyàwén developmentofquasi3dslopestabilitymodelassociatedwithgroundwaterlevelvariations
AT hwangyawen kǎolǜdexiàshuǐwèibiànhuàzhīnǐshìsānwéibiānpōwěndìngmóshìzhījiànlì
AT huángyàwén kǎolǜdexiàshuǐwèibiànhuàzhīnǐshìsānwéibiānpōwěndìngmóshìzhījiànlì
_version_ 1719110336169115648