跳到主要內容

臺灣博碩士論文加值系統

(18.97.14.84) 您好!臺灣時間:2024/12/14 16:00
字體大小: 字級放大   字級縮小   預設字形  
回查詢結果 :::

詳目顯示

: 
twitterline
研究生:賴奕君
研究生(外文):Yi-Chun Lai
論文名稱:黏彈性褶皺生成機制及數值模擬技術探討
論文名稱(外文):Folding of Single Visco-elastic Layer — Numerical Simulation
指導教授:鄧茂華鄧茂華引用關係鄭富書鄭富書引用關係
指導教授(外文):Mao-Hua TengFu-Shu Jeng
學位類別:碩士
校院名稱:國立臺灣大學
系所名稱:地質學研究所
學門:自然科學學門
學類:地球科學學類
論文種類:學術論文
論文出版年:2000
畢業學年度:88
語文別:中文
中文關鍵詞:褶皺數值模擬應變速率黏彈性有限元素法
外文關鍵詞:foldingnumerical simulationstrain ratevisco-elasticFEM
相關次數:
  • 被引用被引用:7
  • 點閱點閱:280
  • 評分評分:
  • 下載下載:18
  • 收藏至我的研究室書目清單書目收藏:0
本文以力學方法及數值方法模擬、分析與討論黏彈性岩層產生褶皺的力學機制及控制因素。數值分析採用有限元素法程式ABAQUS。考量之控制因素包括:岩層之材料性質、應變速率、模擬技術等。
由分析結果得知:(1) 褶皺生成之波形受到應變速率的影響:當應變速率較快之時,岩層之波形由彈性阻抗比所決定,形成之波長為臨界波長;(2) 當應變速率較慢時,褶皺之波形由初始幾何外形擾動所控制。
為了將初始幾何外形對褶皺構造的影響排除,本研究另外採用了一種不需要初始幾何外形缺陷的擾動方法來進行模擬。同樣的,當應變速率較快時,褶皺波形由岩層的彈性性質所控制。當擠壓外力大於一特定值時,形成之褶皺具有一雙頻波形;當擠壓外力小於一特定值時,褶皺之波形為一單一且具振幅衰減行為之波形。
當岩層受到兩階段不同應變速率擠壓時,由分析結果得知:第一階段應變速率較快時所形成之褶皺波形可在應變速率較慢的第二階段維持。相反的,第一階段應變速率較慢時所形成之褶皺波形會受到應變速率較快之第二階段壓縮的影響而改變。
This thesis aims to identify the mechanisms associated with folding of a single visco-elastic layer based on a series of numerical analyses, using finite element program, ABAQUS. The factors, including material properties, strain rate as well as simulation skill were considered.
The analyzed results indicate that: (1) The waveform is dominated by the compressing rate, namely the strain rate. As the layer is compressed under fast strain rate the waveform of the yielded fold is dominated by the elastic competence contrast R, and has a critical wave length; (2) As the strain rate is slow, the waveform is controlled by the initial geometrical perturbation.
To exclude the influence of initial perturbation, this research develops a perturbation method without introducing the geometry imperfection. Again, when compressed under fast strain rate, the waveform is controlled by the elastic properties. When the applied force F is greater then a certain value , the waveform comprises of two frequencies. When F is less then a certain value , the waveform has only one frequency with decreasing amplitudes away from the perturbed end.
As the layer is two-stage compressed with a fast and a slow strain rates, we found the waveform yielded at initial stage with fast strain rate can be maintained to later stage regardless the slow strain rate. On the other hand, the waveform yielded at initial stage with slow strain rate can be altered by the later fast strain rate.
誌謝I
摘要II
AbstractIII
目錄IV
圖目錄VI
表目錄IX
第一章 前言1
1-1 研究動機1
1-2 研究目地與方法2
1-3 本文內容2
第二章 前人研究4
2-1 褶皺的分類4
2-2 褶皺的發育過程4
2-3 彈性材料的褶皺理論6
2-4 黏性材料的褶皺理論8
2-5 褶皺的物理模型研究11
2-6 褶皺的數值模型研究11
第三章 研究方法15
3-1 分析方法簡介15
3-2 數值分析模型介紹16
3-3 數值分析模型規劃16
3-4 Maxwell黏彈性材料驗證17
第四章 數值模擬技術比較27
4-1 數值模型介紹27
4-2 預壓縮-擾動法27
4-3 初始幾何外形擾動法29
4-4 討論30
第五章 應變速率對褶皺構造之影響38
5-1 初始幾何外形擾動法38
5-2 預壓縮-擾動法41
5-3 褶皺產狀成因之力學分析 — 彈性材料44
5-4 褶皺產狀之影響 — 黏性阻抗比及應變速率48
5-5 討論53
第六章 結論與建議74
6-1 結論74
6-2 進一步研究進建議75
參考文獻76
附錄A 有限元素法簡介80
附錄B 黏彈性材料參數輸入說明89
附錄C 分析案例總列表91
林啟文、楊昭男(1991),簡介褶皺形成的理論,地質,11卷1期,第47-65頁。
楊昭男(1995),臺灣的地質構造現象,經濟部中央地質調查所,台北。張國楨(1998),台灣西部基盤高區對鄰近主要新構造影響之三模擬,國立台灣大學碩士論文,台北。
張迺楨(1999),褶皺之數值模擬與力學機制初探,國立台灣大學碩士論文,台北。
蕭銘璽(1996),北港高區附近新構造運動之數值模擬,國立台灣大學碩士論文,台北。
Abbassi, M.R. and N.S. Mancktelow (1990). “The effect of initial perturbation shape and symmetry on fold development,” Journal of Structural Geology 12: 273 - 282.
Bijlaard, P.P. (1946). “On the Elastic Stability of Thin Plates Supported by a Continuous Medium,” Proc. K. Ned. Akad. Wet. 49: 1189 - 1199.
Biot, M. A. (1937). “Bending of an Infinite Beam on an Elastic Foundation,” Trans. Am. Soc. Mech. Eng. 55: A1 - A7.
Biot, M. A. (1939). “Non-linear theory of elasticity and the linearized case for a body under initial stress,” Philos. Mag. 28:468 - 489.
Biot, M. A. (1957). “Folding Instability of a Layered Viscoelastic Medium Under Compuession,” Proc. R. Soc. London. Ser. A 242: 444 - 454.
Biot, M. A. (1957). “Theory of Folding of Stratified Viscoelastic Media and Its Implocations in Tectonics and Orogenesis,” Geol. Soc. Am. Bull. 72: 1595 - 1620.
Biot, M. A. (1959). “On the instability of folding deformation of a layered viscoelastic medium under compression,” J. Appl. Mech. 26: 393 - 400.
Biot, M. A. (1960). “Instability of a continuously inhomogeneous viscoelastic half-space under initial stress,” J. Franklin Inst. 270: 190 - 201.
Biot, M. A. (1961). “Theory of folding of stratified viscoelastic media and its implications in tectonics and orogenesis,” Geol. Soc. Am. Bull. 72: 1595 - 1620.
Biot, M. A. (1964). “Theory of Internal Buckling of a Confined Mutilayered Structure,” Geol. Soc. Am. Bull. 75: 563 — 568.
Biot, M. A. (1965). “Further Development of the Theory of Internal Buckling of Mutilayers,” Geol. Soc. Am. Bull. 76: 833 — 840.
Chapple, W. M. (1968), “A Mathematical Theory of Finite- Amplitude Rock-Folding,” Geol. Soc. Am. Bull. 79: 47 -68.
Cobbold, P. R. (1977), “Finite-element Analysis of Fold Propagation — a Problematic Application ?” Tectonophysics 38: 339 - 353.
Currie, J. B., A. W. Patnode and R. P. Trump (1962). “Development of Folds in Sedimentary Strata,” Geol. Soc. Am. Bull. 73: 461 — 472.
Dieterich, J. H. and N. L. Carter (1969), “Stress — History of Folding,” American Journal of Sciences 267: 129 — 154.
Hunt, G. W., M. K. Wadee and N. Shiacolas (1993), “Localized Elasticae for the Strut on the Linear Foundation,” Journal of Applied Mechanics 60: 1033 — 1038.
Hunt, G. W., H. B. Mühlhaus and A. I. M. Whiting (1996), “Evolution of Localized Folding for a Thin Elastic Layer in a Softening Visco-elastic Medium,” Pure and applied Geophysics 146: 229 — 252.
Johns, M. K. and S. Mosher (1996). “Physical Models of Regional Fold Superposition: the Role of Competence Contrast,” Journal of Structural Geology. 18: 475 — 492.
Johnson, A. M. (1970). Physical Processes in Geology, Freeman, Cooper & Company, California.
Johnson, A. M. (1977). Styles of Folding, Elsevier Scientific Publishing Company, Amsterdam — Oxford — New York.
Johnson, A. M. and R. C. Fletcher (1994). Folding of Viscous Layers, Columbia University Press, New York.
Lan, L. and P. J. Hudleston (1991), “Finite-element moduls of buckle folds in non-linear materials,” Tectonophysics 199: 1 - 12.
Mancktelow, N. S. and M. R. Abbassi (1991), “Single layer buckle folding in non-linear materials--II. Comparison between theory and experiment,” Journal of structral geology 14: 105 - 120.
Mancktelow, N. S. (1999), “Finite-element modelling of single- layer folding in elasto-viscous materials: the effect of initial perturbation geometry,” Journal of structral geology 21: 161-177.
Ramberg, H. (1959). “Evoltion of Ptygmatic Folding,” Nor. Geol. Tidsskr., 39: 99 - 151.
Sherwin, J. A. and W. M. Chapple (1968). “Wavelengths of Single Layer Folds : A Comparison Between Theory and Observation,” Am. J. Sci., 266: 167-179.
Smoluchowski, M. (1909), “Uber Ein Gewisses Stabilitatsproblem Der Elastizitatslehre Und Der Beziehungen Zur Entstehung Von Faltenbitgen,” Anz. Akad. Wiss. Krakau, Math. Naturw., 2: 3 and 727.
Strayer, L. M. and P. J. Hudleston (1997), “Numerical Modeling of Fold Initiaion at Thrust Ramps,” Journal of Structural Geology. 19: 551 - 566.
Susan, H. Treagus (1973), “Buckling Stability of a Viscous Single-Layer System, Oblique to the Principal Compression,” Tectonophysics 19: 271 - 289.
Toshihiko, Shimamoto and Ikuo Hara (1975), “Geometry and Strain Distribution of Single — Layer Folds,” Tectonophysics, 30: 1 - 34.
Zhang, Y., B. E. Hobbs, A. Ord and H. B. Muhlhaus (1996). “Computer Simulation of Single — Layer Buckling,” Journal of Structural Geology. 18: 643 — 655.
Zhang, Y., B. E. Hobbs and M. W. Jessell (1993), “Crystallographic preferred orientation development in a buckled single layer : a computer simulation,” Journal of Structural Geology. 15: 265 — 276.
QRCODE
 
 
 
 
 
                                                                                                                                                                                                                                                                                                                                                                                                               
第一頁 上一頁 下一頁 最後一頁 top