Numerical Simulations on the Landslide Motions of an Inclined Soil Layer Caused by Rain Infiltration and Bedrock Exfiltration

碩士 === 國立成功大學 === 水利及海洋工程學系 === 104 === Landslides are the mass movement caused by gravity down the slope on hillsides, and can threaten people's lives and properties. Landslides and its movement mainly are controlled by change in internal the pore water pressure. Rain infiltration and bedrock...

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Main Authors: Shin-LinChen, 陳新霖
Other Authors: Chyan-deng Jan
Format: Others
Language:zh-TW
Published: 2016
Online Access:http://ndltd.ncl.edu.tw/handle/bn3rnd
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spelling ndltd-TW-104NCKU50830932019-05-15T22:54:10Z http://ndltd.ncl.edu.tw/handle/bn3rnd Numerical Simulations on the Landslide Motions of an Inclined Soil Layer Caused by Rain Infiltration and Bedrock Exfiltration 降雨入滲和岩盤出滲引發土體崩塌之數值模擬 Shin-LinChen 陳新霖 碩士 國立成功大學 水利及海洋工程學系 104 Landslides are the mass movement caused by gravity down the slope on hillsides, and can threaten people's lives and properties. Landslides and its movement mainly are controlled by change in internal the pore water pressure. Rain infiltration and bedrock exfiltration can change pore water pressure within the soil layer, thereby causing the soil slides. In this study, we developed a model that describe the velocity of block sliding down an inclined plane governed by Newton’s equation of motion and diffusion equation, considering the dilatancy angle and friction coefficient could vary with block displacement. Then we can use this model to analyze the soil layer motion along an infinite slope influenced by rainfall infiltration or bedrock exfiltration, respectively. Results show that the sources of excess pore pressure that control the types of landslide motion. Under rainfall infiltration conditions, the motion of landslide can be categorized into stationary and rapid sliding, and that into stationary, rapid sliding and intermittent slipping caused by bedrock exfiltration conditions. In addition, this study extended infinite slope theory that soil layers can slide a certain distance on a slope to a horizontal plane, further using this model to clarify the relationships between the displacement of block, rainfall infiltration and bedrock exfiltration. Results show that when the block occurs rapid sliding, horizontal sliding distance could be a linear relationship with respect to the intensities of rainfall infiltration and bedrock exfiltration. Also, when the block occurs intermittent slipping, the displacement of intermittent slipping will be a linear relationship with respect to the amount and intensity of bedrock exfiltration. The model develop in this study can provide useful information and thereby refined the prediction, prevention and mitigation of geological disasters. Chyan-deng Jan 詹錢登 2016 學位論文 ; thesis 73 zh-TW
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description 碩士 === 國立成功大學 === 水利及海洋工程學系 === 104 === Landslides are the mass movement caused by gravity down the slope on hillsides, and can threaten people's lives and properties. Landslides and its movement mainly are controlled by change in internal the pore water pressure. Rain infiltration and bedrock exfiltration can change pore water pressure within the soil layer, thereby causing the soil slides. In this study, we developed a model that describe the velocity of block sliding down an inclined plane governed by Newton’s equation of motion and diffusion equation, considering the dilatancy angle and friction coefficient could vary with block displacement. Then we can use this model to analyze the soil layer motion along an infinite slope influenced by rainfall infiltration or bedrock exfiltration, respectively. Results show that the sources of excess pore pressure that control the types of landslide motion. Under rainfall infiltration conditions, the motion of landslide can be categorized into stationary and rapid sliding, and that into stationary, rapid sliding and intermittent slipping caused by bedrock exfiltration conditions. In addition, this study extended infinite slope theory that soil layers can slide a certain distance on a slope to a horizontal plane, further using this model to clarify the relationships between the displacement of block, rainfall infiltration and bedrock exfiltration. Results show that when the block occurs rapid sliding, horizontal sliding distance could be a linear relationship with respect to the intensities of rainfall infiltration and bedrock exfiltration. Also, when the block occurs intermittent slipping, the displacement of intermittent slipping will be a linear relationship with respect to the amount and intensity of bedrock exfiltration. The model develop in this study can provide useful information and thereby refined the prediction, prevention and mitigation of geological disasters.
author2 Chyan-deng Jan
author_facet Chyan-deng Jan
Shin-LinChen
陳新霖
author Shin-LinChen
陳新霖
spellingShingle Shin-LinChen
陳新霖
Numerical Simulations on the Landslide Motions of an Inclined Soil Layer Caused by Rain Infiltration and Bedrock Exfiltration
author_sort Shin-LinChen
title Numerical Simulations on the Landslide Motions of an Inclined Soil Layer Caused by Rain Infiltration and Bedrock Exfiltration
title_short Numerical Simulations on the Landslide Motions of an Inclined Soil Layer Caused by Rain Infiltration and Bedrock Exfiltration
title_full Numerical Simulations on the Landslide Motions of an Inclined Soil Layer Caused by Rain Infiltration and Bedrock Exfiltration
title_fullStr Numerical Simulations on the Landslide Motions of an Inclined Soil Layer Caused by Rain Infiltration and Bedrock Exfiltration
title_full_unstemmed Numerical Simulations on the Landslide Motions of an Inclined Soil Layer Caused by Rain Infiltration and Bedrock Exfiltration
title_sort numerical simulations on the landslide motions of an inclined soil layer caused by rain infiltration and bedrock exfiltration
publishDate 2016
url http://ndltd.ncl.edu.tw/handle/bn3rnd
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