| 研究生: |
黃蘭貴 Huang, Lan-Kuei |
|---|---|
| 論文名稱: |
慣性效應對彈性波在多孔介質內含兩相非混合流體傳波影響之數值研究 A Numerical Evaluation of Inertial Effect on Elastic Wave Propagation and Attenuation through a Poroelastic Medium Containing Two Immiscible Fluids |
| 指導教授: |
羅偉誠
Lo, Wei-Cheng |
| 學位類別: |
碩士 Master |
| 系所名稱: |
工學院 - 水利及海洋工程學系 Department of Hydraulic & Ocean Engineering |
| 論文出版年: | 2010 |
| 畢業學年度: | 98 |
| 語文別: | 英文 |
| 論文頁數: | 79 |
| 中文關鍵詞: | 彈性波 、孔隙介質 、慣性 、有限差分顯式法 |
| 外文關鍵詞: | Dilatational waves, Porous media, inertial, Explicit Finite Difference Method |
| 相關次數: | 點閱:136 下載:4 |
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彈性波於未飽和彈性孔隙介質中傳遞及衰退的特性是目前水文地質方面重要的研究課題。在工程應用上,孔彈性力學理論可以精確地分析兩種非混合流體在孔隙介質中受彈性波之影響及變化。然而,在孔彈性力學理論中,其慣性阻力項、黏滯阻力項及應力項皆為互制(coupling)且為影響彈性波傳遞及衰退程度因子之一,因此在理論模式中無法直接求得邊界值問題之解析解。本研究利用有限差分法對孔彈性力學理論之偏微分方程式中各互制項進行離散化並數值模擬分析彈性波在未飽和孔隙介質中之傳波特性,進而觀察慣性項對孔彈性理論中之固體及兩項非混合孔隙流體的影響。
本文主要探討彈性波在拘限含水層傳遞時之動力行為的變化,經由數值模擬後可以獲得總應力及兩個孔隙非混合流體之壓力值。假設在振盪頻率為1 Hz、10 Hz、100 Hz的情況下,頻率越大,隨著距離傳遞之彈性波衰退程度也越大;比較不同起始孔隙流體飽和度的條件下(例如:非潤濕流體飽和度 =0.3、0.6、0.7、0.8、0.9),其衰退程度隨著 飽和度增大而越大;然慣性項除了對特定範圍(震盪頻率8Hz~80Hz, =0.8~0.84)之近邊界處有明顯之影響外,對其他系統造成之效應較不顯著。
The study on the behavior of elastic wave propagation and attenuation through a fluid-containing porous medium is a central topic in hydrogeophysics. It has been demonstrated recently that the behavior can be well described by the theory of poroelasticity precisely. However, due to the fact that the model equations are decoupled in inertial and viscous coupling terms so that it is impossible to obtain exact analytical solutions for boundary problems, except in few special cases. In the current study, we utilize the finite difference method to disperse the governing partial difference equations and then numerically examine the characteristics of wave propagation and attenuation to gain physical insight on the influence of inertial effect on the pore pressure of two immiscible fluids and the stress of solid.
As an illustrative example, a semi-infinite Columbia Fine Sandy Loam containing two immiscible fluids (water-oil) subject to a stress-excitation boundary on the left side and an impermeable boundary on the up and down sides is investigated at seismic frequencies (1Hz, 10Hz, and 100Hz). Our numerical results show that the decay degree of the stress and pore fluid pressures increase with an increase in travel distance of elastic waves, excitation frequencies, and relative saturation of the non-wetting fluid. Most importantly, it is noted that as relative saturation of the non-wetting fluid takes the value from 0.8 to 0.84 and excitation frequency ranges 8Hz to 80Hhz, the total stress in the dynamic model (with inertial terms) yield a cyclic response while this attribute can not be observed in the diffusive model (inertial terms neglected).
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