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研究生: 謝秉軒
Hsieh, Ping-Hsuan
論文名稱: 三維多面體個別元素法在大規模崩塌模擬之研究
Simulating the rock avalanches using 3D DEM with Polyhedrons
指導教授: 吳建宏
Wu, Jian-Hong
學位類別: 碩士
Master
系所名稱: 工學院 - 自然災害減災及管理國際碩士學位學程
International Master Program on Natural Hazards Mitigation and Management
論文出版年: 2019
畢業學年度: 107
語文別: 英文
論文頁數: 125
中文關鍵詞: 大規模崩塌新磨村南勢坑數值模擬3DEC
外文關鍵詞: Large-scale landslide, Xinmo landslide, numerical simulation, 3DEC, Nan-Shi-Keng landslide
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  • 近年來大規模邊坡破壞發生頻繁,在破壞時往往伴隨大量的土石在數十秒內滑動,造成災害。本研究利用大規模崩塌數值模擬,探討其滑動歷程以及影響範圍,期能在未來有助於劃定大規模邊坡破壞潛勢區滑動影響範圍。本研究中有兩個案例:中國茂縣新磨村邊坡破壞以及台南175縣道南勢坑地滑區。模擬中透過建構三維數值模型、不連續面切割來模擬現地地形與滑動塊體的堆疊,最後探討新磨村邊坡破壞的崩塌歷程,以及預測南勢坑地滑區崩塌後的影響範圍。
    本研究所使用的是屬於分離元素法(Distinct Element Method, DEM)的3 Dimensional Distinct Element Code (3DEC)軟體。模擬時透過給定重力以及連續面摩擦角的改變來模擬塊體滑落。新磨村邊坡破壞模擬結果顯示在數值模擬時必須考慮塊體高速滑動時會產生不連續面摩擦角降低的自潤效果;此外,新磨村上方的塊體會明顯影響塊體的行為與堆積。南勢坑地滑的模擬結果則顯示該地區若發生滑動,將歷時大約30秒左右,在南勢坑溪中堆疊岩塊的影響長度可達390公尺,堆積高度則有30公尺。

    Large-scale rock avalanche has occurred frequently in recent years. A large amount of sand and stone slide only in tens of seconds causing disasters. This study simulate the large-scale rock avalanche by using numerical simulation to explore its sliding history and its impact range. Help to delineate the impact potential area in large-scale rock avalanche in the future. There are two cases in this study: the Xinmao Landslide, which occurred in Xinmo Village, Mao County, China, and the Nan-Shi-Keng, which is located at 175 County Road in Tainan. In the simulation, a three-dimensional numerical model will be built and cut the discontinuous surfaceto simulate the stacking of the local terrain and the sliding block. Finally, discussing the landlside process of the slope of Xinmo Village, and predicting the impactrange of the Nanyukeng Landslide.
    The three Dimensional Distinct Element Code (3DEC) software belonging to the Distinct Element Method (DEM) was used in this study. During the simulation, the block slip simulate by a given gravity and a change in the different friction angle in the joints. The simulation results of the landslide damage in Xinmo Village show that it is necessary to consider the self-lubricating effect of the friction angle reduction in the simulation when the block is sliding at high speed. In addition, the block above the Xinmo Village will significantly affect the behavior and accumulation of the simulation. The simulation results of the Nan-Shi-Keng sliding show that if the sliding occurs in the area, it will take about 30 seconds, and the stacking rock in the Nan-Shi-Keng River will have a temporary dam with 390 meters long and of 30 meters height.

    Chapter 1. Introduction 1 1.1 Background 1 1.2 Motivation and objective 1 1.3 Research process 3 Chapter 2.Literature Review 6 2-1 Large-scale rock avalanche 6 2-2 Empirical method 9 2-2-1 Hong Kong 10 2-2-2 Japan 11 2-2-3 Taiwan 12 2-3 Numerical simulation of rock avalanche process 18 2-3-1 Continuum numerical analysis 19 2-3-2 Discontinuous numerical analysis 24 Chapter 3 Study Sites 28 3-1 The Xinmo Landslide 28 3-1-1 Overview 28 3-1-2 Topographic Characteristics 30 3-1-3 Landslide Mechanism 33 3-1-4 Climate and Hydrology 33 3-1-5 Post-failure simulation of a landslide 34 3-2 The Nan-Shi-Keng Landslide 36 3-2-1 Overview 36 3-2-2 Geography and Geological structures 37 3-2-3 Climate and Hydrology 39 3-2-4 Slope stability analysis 39 Chapter 4 Three-dimensional Distinct Element Method 41 4-1 Theoretical background 41 4-1-1 Aspect of Modeling a Discontinuous System 41 4-1-2 Numerical Formulation of the element method in 3D 42 4-2 Mechanical Calculations for Motion and Interaction in 3D 47 4-2-1 Calculation Step 47 4.2.2 Numerical Stability 53 Chapter 5.Code Verification and Pre-processing 54 5-1 Verification cases 54 5-1-1 Unique Shear Strength on the Sliding Surface 54 5-1-2 Different Shear Strengths on the Sliding Surface 56 5-2 The Xinmo landslide 61 5-2-1 Geometry of the landslide 61 5-2-2 Parameter setting 68 5-3 Nan-Shi-Keng Landslide 71 5-3-1 Geometry of the landslide 71 5-3-2 Parameter setting 74 Chapter 6 Computational Results 78 6-1 Xinmo landslide simulations 78 6-1-1 Sensitivity analysis on joint friction angles 78 6-2 Assessment of the Impact area based on the empirical formulas 94 6-2-1 Runout distance 94 6-2-2 Impact width 94 6-3 Nan-Shi-Keng Landslide simulation 96 6-3-1 Sensitivity analysis on the friction angle of discontinuity 96 6-3-2 Sensitivity analysis on block size 105 6-3-4 Sensitivity analysis on the retaining wall setting 109 6-3-5 The retaining wall does not penetrate the sliding surface 111 Chapter 7 Conclusions 116 7-1 Conclusions 116 7-1-1 Xinmo landslide 116 7-1-2 Nan-Shi-Keng landslide 117 7-2 Suggestions 117 References 118

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