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請用此 Handle URI 來引用此文件: http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/78695
完整後設資料紀錄
DC 欄位值語言
dc.contributor.advisor戴璽恆(Xi-Heng Dai)
dc.contributor.authorChun-Hao Liangen
dc.contributor.author梁淳皓zh_TW
dc.date.accessioned2021-07-11T15:12:48Z-
dc.date.available2024-01-01
dc.date.copyright2020-10-20
dc.date.issued2020
dc.date.submitted2020-10-12
dc.identifier.citation1.Abramowitz, M., Stegun, I. A. (1972). Handbook of Mathematical Functions with Formulas, Graphs, and Mathematical Tables. National Bureau of Standards Applied Mathematics Series 55. Tenth Printing, 887-888.
2.Adrian, R. J. (2007). Hairpin vortex organization in wall turbulence. Physics of Fluids, 19(4), 041301.
3.Benjamin, T. B. (1968). Gravity currents and related phenomena. Journal of Fluid Mechanics, 31(2), 209-248.
4.Bonometti, T., Balachandar, S. (2008). Effect of Schmidt number on the structure and propagation of density currents. Theoretical and Computational Fluid Dynamics, 22(5), 341-361.
5.Brooke, J. W., Hanratty, T. J. (1992). Origin of turbulence‐producing eddies in a channel flow. Physics of Fluids A: Fluid Dynamics, 5(4), 1011-1022.
6.Cantero, M. I., Balachandar, S., García, M. H., Bock, D. (2008). Turbulent structures in planar gravity currents and their influence on the flow dynamics. Journal of Geophysical Research: Oceans, 113(C8), 1-22.
7.Cantero, M. I., Lee, J. R., Balachandar, S., Garcia, M. H. (2007). On the front velocity of gravity currents. Journal of Fluid Mechanics, 586, 1-39.
8.Canuto, C., Hussaini, M. Y., Quarteroni, A., Thomas Jr, A. (2012). Spectral methods in fluid dynamics. Springer Science Business Media.
9.Cebeci, T. (2012). Analysis of turbulent boundary layers. Elsevier 127-134.
10.Chakraborty, P., Balachandar, S., Adrian, R. J. (2005). On the relationships between local vortex identification schemes. Journal of Fluid Mechanics, 535, 189-214.
11.Dai, A. (2013). Gravity currents propagating on sloping boundaries. Journal of Hydraulic Engineering, 139(6), 593-601.
12.Dai, A., Ozdemir, C. E., Cantero, M. I., Balachandar, S. (2012). Gravity currents from instantaneous sources down a slope. Journal of Hydraulic Engineering, 138(3), 237-246.
13.Durran, D. R. (2013). Numerical methods for wave equations in geophysical fluid dynamics (Vol. 32). Springer Science Business Media.
14.Espath, L. F. R., Pinto, L. C., Laizet, S., Silvestrini, J. H. (2015). High-fidelity simulations of the lobe-and-cleft structures and the deposition map in particle-driven gravity currents. Physics of Fluids, 27(5), 056604.
15.Härtel, C., Carlsson, F., Thunblom, M. (2000). Analysis and direct numerical simulation of the flow at a gravity-current head. Part 2. The lobe-and-cleft instability. Journal of Fluid Mechanics, 418, 213-229.
16.Härtel, C., Meiburg, E., Necker, F. (2000). Analysis and direct numerical simulation of the flow at a gravity-current head. Part 1. Flow topology and front speed for slip and no-slip boundaries. Journal of Fluid Mechanics, 418, 189-212.
17.Maxworthy, T., Leilich, J., Simpson, J. E., Meiburg, E. H. (2002). The propagation of a gravity current into a linearly stratified fluid. Journal of Fluid Mechanics, 453, 371-394.
18.Necker, F., Härtel, C., Kleiser, L., Meiburg, E. (2005). Mixing and dissipation in particle-driven gravity currents. Journal of Fluid Mechanics, 545, 339-372.
19.Simpson, J. E. (1972). Effects of the lower boundary on the head of a gravity current. Journal of Fluid Mechanics, 53(4), 759-768.
20.Williamson, J. H. (1980). Low-storage runge-kutta schemes. Journal of Computational Physics, 35(1), 48-56.
21.李奇展 (2019). 異重流前端的葉型和裂口特性. 國立台灣大學工程科學及海洋工程研究所碩士學位論文.
dc.identifier.urihttp://tdr.lib.ntu.edu.tw/jspui/handle/123456789/78695-
dc.description.abstract當異重流隨時間向前流動時,在異重流前端位置可明顯觀測到由頻繁聚合及分裂行為所產生的凹凸不規則結構,在此不規則結構當中,我們將凸起結構稱為葉(Lobe)、凹陷結構稱為裂口(Cleft),葉及裂口(Lobe-and-Cleft)結構為對異重流前端形貌造成變化的重要因素之一。
本研究主要目的有二,第一在過往研究當中亦有針對異重流之流動行為進行分析,然而大部分皆為低雷諾數部分,因此於本研究中我們將針對高雷諾數的部分進行分析,並比較高低雷諾數可能之差異性。第二則是過往文獻中亦較缺乏分析的異重流前端分裂聚合產生葉及裂口結構之原因,在本研究中我們將使用異重流內部渦度場分析分裂聚合行為時渦旋之變化,並將以渦旋解釋造成分裂聚合之起因。
研究之方法我們則使用數值方法求解統御方程式模擬重流體在一長形水槽中與環境流體混合而形成之雷諾數分別為1788、3450、8950、13000、17000之三維異重流,並求解包含濃度場、速度場、渦度場等三維流場中之相關重要參數進行分析比對。
本研究所針對五組不同雷諾數案例結果則顯示,我們除了成功拓展高雷諾數方面之研究資料,在各項雷諾數前端流場資料分析也都符合過往研究中之趨勢。此外,我們也能夠合理的利用渦度強度標準λ_ci呈現齒狀(Tooth-like)結構分裂聚合過程中之行為。而藉由解析有關渦度時變率變化之渦度方程式,包含方程式中對於總體時變率變化最具貢獻之傾斜項分析,以及子母渦旋(Parent and offspring vortex)之交互作用行為皆能有效針對裂口之生成及分裂前進之方向進行合理之解釋。
在我們的研究貢獻當中,除了成功拓展異重流由低雷諾數至高雷諾數下之流動行為分析,並能解釋不穩定渦度場變化對於異重流前端形貌之影響作用。
zh_TW
dc.description.abstractWhile the gravity current flows, it splits and merges frequently at the leading edge of the gravity current, leading to some protrusion and depression structure. In these irregular structures, the protrusion part is called lobe and the depression one is called cleft, both of which are the key points affecting the topology of gravity current. There were two main objectives in our study, the first one was to explore the high-Reynolds-number regime, which was analysed insufficiently in previous studies, and this provided us the access to compare the difference of gravity currents at high and low Reynolds numbers. The other was to determine the causes influencing the splits and merges, both of which lead to the generation and dissipation of lobe-and-cleft structure. The analysis of splits and merges was also relatively lacking in the previous research. In our research, we analysed the variation of vorticity field in the gravity current and concluded the generation and dissipation of lobe-and-cleft structure with the variation of the vortex. The Numerical methods were conducted to solve the governing equations in order to simulate the three-dimensional gravity current, which happens between the interface of high-concentration fluid and ambient fluid, at Reynolds number of 1788, 3450, 8950, 13000, 17000, respectively. Some important parameters such as concentration, velocity, vorticity, and so forth were analysed. Results revealed that we successfully expanded the information from low-Reynolds number to high-Reynolds number, and the tendency of the statistical results at different Reynolds number were also similar to the results in the previous study. Furthermore, the swirling parameter of λ_ci was used to represent the variation of vortex when the lobe-and-cleft structure split and merged. Both the analysis of vorticity equation, including the observation of tilting term whose contribution was greatest in the equation, and the analysis of the interactions between the parent and offspring vortex, all provided the physical supports that the vortex has great influence on the generation and the evolution of the new cleft. It provides the evidence that the study can help us to compare the difference of gravity current from low to high Reynolds number, and the unstable turbulence structure has influence on the topology of gravity current.en
dc.description.provenanceMade available in DSpace on 2021-07-11T15:12:48Z (GMT). No. of bitstreams: 1
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Previous issue date: 2020
en
dc.description.tableofcontents國立臺灣大學碩士學位論文口試委員會審定書 I
致謝 II
摘要 III
Abstract IV
目錄 VI
圖目錄 VIII
表目錄 XI
第一章 緒論 1
1.1 前言 1
1.2 文獻回顧 2
1.3 研究目的及論文架構 6
第二章 研究方法 7
2.1 統御方程式 7
2.2 數值模擬方法 9
2.3 數值模擬資料的積分型態 10
2.4 壁面定律(The law of the wall) 11
第三章 結果與分析 13
3.1 異重流前端流場分析 17
3.1.1 異重流濃度場與速度場分析 17
3.1.2 前端速度分析 18
3.1.3 異重流前端環境流體流進裂口之流量分析 21
3.1.4 異重流前端雷諾數〖Re〗_F與葉尺寸b ̅之關係 25
3.2 異重流前端分裂聚合分析 29
3.2.1 雷諾數3450及13000分裂過程中濃度場、速度場、渦度場之變化情形分析 33
3.2.2 雷諾數3450及13000聚合過程中濃度場、速度場、渦度場之變化情形分析 42
3.3 異重流前端輪廓分裂與渦度方程式之關係 51
3.3.1 渦度方程式 52
3.3.2 雷諾數3450異重流前端輪廓分裂與傾斜項之關係 54
3.3.3 雷諾數13000異重流前端輪廓分裂與傾斜項之關係 58
3.4 異重流前端輪廓分裂與子母渦旋之關係 62
3.4.1 雷諾數3450異重流前端輪廓分裂與子母渦旋之關係 64
3.4.2 雷諾數13000異重流前端輪廓分裂與子母渦旋之關係 72
第四章 結論與建議 81
4.1 結論 81
4.2 建議與未來工作 84
參考文獻 85
dc.language.isozh-TW
dc.subject不穩定紊流結構zh_TW
dc.subject異重流zh_TW
dc.subject葉及裂口結構zh_TW
dc.subject分裂zh_TW
dc.subject聚合zh_TW
dc.subjectLobe-and-Cleft structureen
dc.subjectGravity currenten
dc.subjectUnstable turbulenceen
dc.subjectMergeen
dc.subjectSpliten
dc.title異重流前端葉及裂口的分裂與聚合zh_TW
dc.titleThe Splits and Merges of the Lobe-and-Cleft Structure at the Leading Edge of Gravity Currenten
dc.typeThesis
dc.date.schoolyear109-1
dc.description.degree碩士
dc.contributor.oralexamcommittee羅弘岳(Hong-Yue Luo),吳清森(Qing-Sen Wu)
dc.subject.keyword異重流,葉及裂口結構,分裂,聚合,不穩定紊流結構,zh_TW
dc.subject.keywordGravity current,Lobe-and-Cleft structure,Split,Merge,Unstable turbulence,en
dc.relation.page87
dc.identifier.doi10.6342/NTU202004256
dc.rights.note有償授權
dc.date.accepted2020-10-13
dc.contributor.author-college工學院zh_TW
dc.contributor.author-dept工程科學及海洋工程學研究所zh_TW
dc.date.embargo-lift2024-01-01-
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