| 研究生: |
吳昀達 Wu, Yun-Ta |
|---|---|
| 論文名稱: |
長波與海岸結構物互制之研究 LONG WAVES INTERACTION WITH COASTAL STRUCTURES |
| 指導教授: |
蕭士俊
Hsiao, Shih-Chun |
| 學位類別: |
博士 Doctor |
| 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: | 2015 |
| 畢業學年度: | 103 |
| 語文別: | 英文 |
| 論文頁數: | 323 |
| 中文關鍵詞: | 海嘯 、孤立波 、碎波 、潛堤 、多孔介質流 、孔隙板 、紊流 、質點影像測速儀 、RANS模式 |
| 外文關鍵詞: | Tsunami, solitary wave, breaking wave, submerged breakwater, porous media flow, slotted barrier, turbulence, PIV, RANS model |
| 相關次數: | 點閱:141 下載:16 |
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本文旨在探討海嘯長波與海岸結構物互制所產生之水動力及紊流特性,並以孤立波型態之長波作為海嘯波代表。是以二式為法:物理模型量測主要利用高解析度之質點影像測速儀配合空間鑲嵌法呈現流場結構,透過重複多次相同試驗,以及利用整體平均法,遂而求出平均物理量及紊流擾動量;數值模式則是基於雷諾平均方程式以及紊流模式,求解平均物理量與紊流動能。
首先,求索如何在數值模式中重現準確且穩定之孤立波。經由不同精度之孤立波理論解加至模式中,並分別利用邊界造波與源項造波之方式,論究造波之準確性與穩定性。前者乃依準確代表輸入之波高與實際模擬之波高差異言之,後者則是代表需要多長之傳播距離使模擬之波浪可趨於穩定。另外,黏滯性對孤立波於水平底床傳遞之影響,亦利用實驗量測與數值模擬論證之。
復次,探討孤立波與透水、不透水潛堤互制之議題。根據量測與模擬結果,紊流動能最大值皆發生於結構物之上游側。再者,利用巨觀描述,亦即平均之概念,模擬透水潛堤,則可擬得大部分的流體之水動力特性,但細節之流場結構則須仰賴微觀描述,即直接模擬透水結構物之粒徑組成以得之。
繼之,剖析孤立波與板式結構物之互制。針對不透水板,明顯之紊流動能發生在碎波捲入空氣之區域,以及流場分離所形成之渦流。而模擬此配置下所產生之紊流動能,則須仰賴基於非線性之渦動滯度假設下之紊流模式近似雷諾應力。而模擬高度產生流場分離的問題,譬如孤立波通過潛沒式孔隙板,則直接求解邊界層流況可得到較準確之模擬結果。
於末,解答連續孤立波在斜坡上碎波之疑義,藉由改變相鄰兩波峰之距離,其溯升、溯降等水動力特性亦因此而改變。
本研究主要貢獻在於提供量測之長波與結構物互制過程中,平均流與紊流之特性。通過精密之實驗量測與高精度數值模擬,耙梳四個與海岸工程相關之議題,既釐清並闡述詳細之物理現象,且又證實數值模式針對不同工程問題之準確性與適用性。
This dissertation presents an investigation on the wave hydrodynamics around coastal structures under tsunami–like long waves by means of solitary waves. For each topic of interest, numerical simulations are supported by carefully conducted experiments or available data in literature. Physical modeling relies on a high-resolution particle image velocimetry to measure velocity properties due to wave-structure interaction. By repeating sufficient times of identical experiment, meaningful turbulence information can be evaluated through the ensemble-averaged method for the mean velocities and the Reynolds-decomposition method for the velocity fluctuations. Numerical simulations are computed by a depth- and phase-resolving wave model based on the Reynolds-averaged Navier-Stokes equations with an appropriate turbulence model to relate the Reynolds–Stress.
Propagation of solitary waves in a constant water depth is first investigated. Both the Dirichlet boundary condition and the internal mass source are utilized to generate desired solitary waves with the implementations of various solitary wave theories in the numerical model. The purpose of this attempt is to examine how to generate stable and accurate solitary wave in the first place. Accurate solitary waves are examined by means of relative error of the wave height between the input signal and the realistic generated wave while stable solitary waves are examined by means of how much distance is necessary to stabilize the waves. Attenuation of solitary waves propagating over a significant traveling distance due to viscous effect is then studied experimentally and numerically.
Next, interactions between solitary waves and submerged permeable/impermeable breakwaters are investigated. Maximum magnitude of turbulent intensity is always observed at the leading edge of the obstacle for both obstacle scenarios. It is found that the macroscopic approach for porous media flow can predict the overall velocity and turbulence fields but the detailed physics need to be achieved by means of the microscopic description for the flow within the porous structure.
Thirdly, we concern the wave hydrodynamics around an environmental-friendly coastal defense by means of submerged solid/slotted barrier under solitary waves. For the solid case, strong turbulence has been created by large amplitude of solitary wave and wave breaking occurred during wave–structure interaction. It is found that the non-linear eddy viscosity model to approximate the Reynolds-Stress is indeed important for the prediction of turbulent kinetic energy. For the slotted case, a complicated flow pattern due to flow separation and interactions between induced vortices has been observed by laboratory observation and later confirmed by simulation.
Last topic focuses on successive solitary wave breaking on a sloping beach. By varying the time separation between two neighboring crests of solitary waves, significant difference on the run-up and run-down processes has been observed through numerical simulation. It should be devoted to experimental effort in order to verify the numerical findings.
This study mainly contributes to provide reliable measured data in terms of velocity and turbulence due to wave-structure interaction. Such data is then used to compare with numerical simulation in order to ensure that the present wave model can provide meaningful physics on coastal engineering related applications.
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