| 研究生: |
賴貞方 Lai, Cheng-Fang |
|---|---|
| 論文名稱: |
地震作用下土壤液化之有限元素分析 Finite Element Analyses with Soil Liquefaction under Seismic Loads |
| 指導教授: |
朱聖浩
Ju, Shen-Haw |
| 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: | 2013 |
| 畢業學年度: | 101 |
| 語文別: | 英文 |
| 論文頁數: | 81 |
| 中文關鍵詞: | 帽蓋模式 、有限元素法 、土壤液化 、流固耦合系統 、Newmark 法 、Zienkiewicz |
| 外文關鍵詞: | cap model, finite element method, soil liquefaction, solid-water coupled system, Newmark method, Zienkiewicz |
| 相關次數: | 點閱:159 下載:12 |
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台灣位處於地震帶上,頻繁的地震所造成的土壤液化是無法避免的。但是,土壤液化會使得土壤強度減少,造成支撐建築物和橋梁的能力降低,導致他們傾斜或滑動因而被破壞。本論文之主要目的是發展三維有限元素方法並用於模擬液化土壤受力後之行為。所發展之有限元素程式是採用Zienkiewnicz等人所推導之流固耦合系統理論做為控制方程式; 使用Newmark法求解微分方程; 土壤之非線性行為遵循帽蓋模式,為非線性彈塑性分析。並使用有限元素程式建立簡單之液化土壤模型計算例題,其分析之結果與前人之研究結果相當符合,因此本程式之正確性應可證明。由於此領域之研究內容相當廣泛複雜,本論文僅有初步分析之結果,其更進一步之研究持續進行中。
Taiwan is located at the intersection of the Philippines Sea Plate and the Euraisian Plate, where are part of the circum-Pacific volcano and seismic zone. The soil liquefaction caused by frequent earthquake thus cannot be avoided. When liquefaction occurs, the strength of the soil decreases, and the ability of a soil deposit to support foundations for buildings and bridges is reduced. That can cause them to tilt or slide and this movement can cause destruction of structures. The main purpose of this study is to establish the three dimensional finite element program, which can be used to analyze the behavior of soil liquefaction under seismic loads. The governing equation implemented in the program is coupled soil skeleton and pore fluid interaction, which were derived by Zienkiewicz et al; use Newmark method of numerical integration to solve differential equations; and the nonlinear soil behavior is represented by the nonlinear kinematic cap model based on classic theory of elastoplasticity. This study builds the fundamental model of soil liquefaction to analyze examples by the finite element program. The results are similar to the other thesis. Therefore, the program is validated and it is able to successfully analyze the system that coupled soil and water. This study only presented with initial achievement on soil liquefaction because the content of this field is quite extensive and complex, and further analysis will be continued.
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