| 研究生: |
黃瑞昌 Huang, Jui-Chang |
|---|---|
| 論文名稱: |
土石流啟動機制之數值分析 Numerical Analysis of the Mechanism of Debris Flow Initiation |
| 指導教授: |
常正之
Charng, Jeng-Jy |
| 學位類別: |
碩士 Master |
| 系所名稱: |
工學院 - 土木工程學系 Department of Civil Engineering |
| 論文出版年: | 2003 |
| 畢業學年度: | 91 |
| 語文別: | 英文 |
| 論文頁數: | 147 |
| 中文關鍵詞: | 土石流 、啟動 、有限元素 |
| 外文關鍵詞: | FEM, Initiation, Debris Flow |
| 相關次數: | 點閱:71 下載:3 |
| 分享至: |
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本文主要針對降雨入滲過程中,滲流及地下水位變動所造成溪床堆積土體變形,進而引致土石流啟動之探討,並利用二維有限元素法來模擬土石流的啟動過程。首先,模擬不同條件下的水槽試驗,驗證此分析方法之可行性。其後,應用此分析方法在銅門與豐丘土石流上,使用降雨量滲透模式之暫態分析,結合彈塑性變形分析與Spencer & Bishop極限平衡穩定分析,探討在降雨期間,溪床堆積土體受滲流影響時,孔隙水壓、土體變形及安全係數之相對關係。
根據模擬結果顯示,銅門與豐丘兩地區在豪雨期間,孔隙水壓的上升造成溪床堆積物位移增量增大,同時,邊坡穩定之安全係數亦下降,則表示該土體正處於不穩定之狀態至破壞的發生,此一過程可視作土石流之啟動機制。此外,本研究建立銅門與豐丘地區在不同地下水位狀況下土石流啟動之臨界降雨線。由分析結果顯示,銅門地區地下水位在地表下1.5m處、豐丘地區地下水位在地表下2m處之臨界降雨線與現地迴歸分析值相當吻合,可作為土石流預警之參考。
A two-dimensional (2-D) finite element deformation analysis incorporated with transient seepage analysis was adopted to simulate the initiation of debris flow. Two limit equilibrium methods “Spencer” and “Bishop” were applied to determine the factor of safety of soil mass during precipitation. Firstly, several sets of flume experiments are examined by numerical tools to verify the appropriateness of numerical model and the validity of numerical procedures. The numerical predictions of the pore water pressure response are reasonable in agreement with the laboratory measurements for flume experiments. Subsequently, the numerical analysis was shifted to debris flow field sites in Tung-Men and Feng-Chiou for a full-scale simulation of debris flow initiation.
For numerical results in Tung-Men and Feng-Chiou Debris Flows, it can be seen that the rainfall might raise the groundwater table and in turn generate the pore water pressure. Eventually the displacement increment increases abruptly and the corresponding factor of safety dropped immediately at the moment of pore water pressure rising. This study establishes the critical rainfall line for different groundwater table conditions in Tung-Men and Feng-Chiou areas. The critical rainfall line for groundwater table at z=1.5m appears reasonably close to the regression analysis in Tung-Men area and at z=2m agrees with the regression analysis in Feng-Chiou area.
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