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| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 黃宏斌(Hung-Pin Huang) | |
| dc.contributor.author | Hao-Kai Ho | en |
| dc.contributor.author | 何晧愷 | zh_TW |
| dc.date.accessioned | 2021-06-08T03:03:50Z | - |
| dc.date.copyright | 2017-07-20 | |
| dc.date.issued | 2017 | |
| dc.date.submitted | 2017-07-13 | |
| dc.identifier.citation | [1]臺灣省山地農牧局 (1982),「臺灣省防砂壩工程調查報告」。
[2]陳正炎 (1987),「投潭水作用下渠床沖刷剖面之研究」,台灣水利,35卷1期,pp.35-52。 [3]吳金洲 (1990),「堰壩溢流水舌對下游河床沖刷之研究」,逢甲大學土木及水利工程研究所碩士論文。 [4]陳正炎、郭信成、鐘文傳 (1993),「堰壩投潭沖刷特性因子之研究」,中華水土保持學報,24卷2期,pp.81-89。 [5]陳正炎、彭思顯、鐘文傳 (1993),「投潭水作用下局部沖刷之沖刷率研究堰」,中華水土保持學報,25卷3期,pp.135-141。 [6]蘇重光、連惠邦 (1993),「防砂壩下游天然河床受壩頂溢流沖刷之研究」,台灣水利,第41卷第二期,pp.35~41。 [7]陳正炎、蔡建文 (1995),「堰壩投潭水流沖擊力之研究」,中華水土保持學報,26卷2期,pp.135~144。 [8]陳聖文 (2000),「防砂壩下游帶工佈置之試驗研究」,國立中興大學土木工程學系碩士論文。 [9]李祈宏 (2000),「砂礫河床之跌水沖刷分析」,國立中央大學土木工程研究所碩士論文。 [10]水土保持手冊 (2005),「水土保持手冊-工程方法篇」,行政院農業委員會水土保持局。 [11]陳佳裕 (2007),「防砂壩下游水流沖擊力與局部沖刷現象之探討」,國立臺灣大學生物環境系統工程學系碩士論文。 [12]行政院農委會水土保持局南投分局 (2011),「彰投地區重要集水區成效評估暨構造物總體檢成果報告」。 [13]行政院農委會水土保持局南投分局 (2011),「雲嘉地區重要集水區成效評估暨構造物總體檢成果報告」。 [14]劉希羿 (2013),「坡度跌流工沖擊流場機制之研究」,國立中興大學土木工程學系博士論文。 [15]劉家齊 (2015),「應用FLOW-3D模擬橋墩周圍流場及底床沖刷之研究」,國立成功大學水利及海洋工程學系碩士論文。 [16]黃宏斌 (2016),「水土保持防砂構造物沖刷坑形成機制與防治方法之探討(1/2)」,行政院農委會水土保持局研究計畫成果報告。 [17]黃宏斌 (2016),「105年水土保持防砂構造物沖刷坑形成機制與防治方法之探討」,行政院農委會水土保持局研究計畫成果報告。 [18]Dick R. Mastbergen and Jan H. Van Den Berg. (2003). “Breaching in fine sands and the generation of sustained turbidity currents in submarine canyons.” Sedimentology. [19]Flow Science, “User Manual of FLOW-3D Version 10.1”, Flow Science. [20]Gaël Epely-Chauvin, Giovanni De Cesare, Sebastian Schwindt. (2014) “Numerical modelling of plunge pool scour evolution in non-cohesive sediments,” Engineering Applications of Computational Fluid Mechanics Vol. 8, No. 4, pp. 477-487. [21]Hoffmans Gijs J. C. M. (1998), “Jet scour in equilibrium phase”, Journal of Hydraulic Engineering, ASCE, April 1998, pp.430-437. [22]Javad Farhoudi, Kenneth V. H. Smith (1985), “Local scour profiles downstream of hydraulic jump”, Journal of Hydraulic Research, Vol.23, No.4, pp. 343-358. [23]Junke Guo. (2002). “Hunter Rouse and Shields Diagram., 1096-1098. World Scientific. [24]L. van Rijn. (1984). “Sediment transport, Part I: bed load transport.”, Journal of Hydraulic Engineering. [25]Mason, P.J. and Arumugam, K. (1985). “Free jet scour below dams and flip buckets.” Journal of Hydraulic Engineering, ASCE, Vol. 111, No. 2, pp. 220-235. [26]M. G. Kleinhans. (2000). “Sorting out sand and gravel: sediment transport and deposition in sand-gravel bed rivers.” PhD thesis, Universitaat Utrecht. [27]M. Habibi, M.J khanjani. (2012). “Scour Analysis in High Vertical Drop Shallow Using Numerical and Physical Models.” International Journal of Emerging Technology and Advanced Engineering, Volume 2, Issue 6. [28]Shahrokh Amiraslani, Jafar Fahimi, Hossein Mehdinezhad. (2010). “The Numerical Investigation of Free Falling Jet’s Effect On the Scour of Plunge Pool,” XVIII International Conference on Water Resources. [29]R. Soulsby. (1997). “Ch. 9: Bedload transport in Dynamics of Marine Sand.” Thomas Telford Publications. [30]U.S. Department of Transportation, Federal Highway Administration. (2006), Hydraulic Engineering Circular No. 14, 3rd edition. | |
| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/20793 | - |
| dc.description.abstract | 水流通過防砂壩或固床工後形成跌水,流動過程中高位能轉換成動能衝擊下游溪床形成沖刷坑,經常導致壩趾基礎淘空或是護坦受損,進而危害構造物安全。本研究藉水槽試驗探討自由射流下沖刷坑之沖刷機制與型態,並提出沖刷坑特徵之預測模式。
本研究水槽試驗之範圍為單寬流量0.00325~0.0177cms/m,跌水高0.02~0.15 m,均質粒徑1.5~7.5mm,沖刷時間2400~14400s,在清水流下經試驗數據分析與FLOW-3D模擬,得結論如下: 1.沖刷坑深度與跌水高、單寬流量成正相關,而與粒徑大小成負相關,且隨時間成冪次方遞增直到達平衡狀態為止,而沖刷坑長度約為最大沖刷坑深度之3倍(L2/hs=3)。 2.沖刷坑深度與有效跌水高比隨時間增加而趨於穩定,最終達一臨界值,其最大沖刷坑深度將不超過有效跌水高之0.7倍。 3.沖刷坑深度與壩基掏刷深度呈線性遞增,壩基掏刷深度約為最大沖刷坑深度之0.45至0.85倍間。 4.消能效率隨著相對臨界水深之降低而增加,當臨界水深與壩高之比在0.4以下,其消能效率皆可達50%以上。 5.經過水槽試驗,可得到沖刷坑深度隨時間變化模式: h_st/H=0.9560(q^2/(gH^3 ))^0.4130 (d/H)^(-0.4448) (t_t/240)^0.0345 hst為沖刷延時t時之最大沖刷坑深度(m),H為跌水高度(m),q為單寬流量(cms/m),g為重力加速度(m/s2),d為粒徑大小(m),tt為沖刷延時(min)。 6.透過FLOW-3D數值模擬垂直跌水之沖刷,以沖刷坑深度變化率為0.003cm/s來判斷是否達平衡狀態,調整流量係數(C=0.885)後其最大沖刷深度與水槽試驗有相當之吻合度。 7.藉實測資料與FLOW-3D模擬比對,模擬之沖刷坑深度將些微高估於實際情形,未來應用於預估沖刷坑規模時須注意。 | zh_TW |
| dc.description.abstract | The potential energy converted into kinetic energy by fall at check dam or ground sill always attacks the creek bed and forms a scour hole. This phenomenon results in taking out the base of hydraulic structure or damaging the apron, and even affecting the safety of the structure. This study uses flume experiments to investigate the free jet scours and does hydraulic mechanical mechanism and behavior analysis of vertical drop. The prediction models are developed and being used to predict the scour below high vertical drops.
The per unit width of discharge is between 0.00325~0.0177cms/m, the height of drop is between 0.02~0.15 m, the particle size is between 1.5~7.5mm, and the test duration time is between 2400~14400s in this flume experiment. After analyzing available data and the simulation by FLOW-3D, the principle results were as follows: 1.The depth of scour is positively correlated with the height of drop, the per unit width of discharge, and is negatively correlated with the particle size. The scour depth increases with time in an exponential rate until reaching to the equilibrium, and the length of scour is 3 times than the depth of scour(L2/hs=3). 2.The ratio of the scour depth to effective drop height increases with time and eventually reaches a critical value, and the maximum depths of scour will not exceed 0.7 times the effective drop height. 3.The depth of scour at the base of hydraulic structure is about 0.45 to 0.85 times to the maximum depth of scour and linearly increasing with it. 4.The energy dissipation efficiency increases with the relative critical water depth. The energy dissipation efficiency can reach more than 50% . while the critical water depth is equal to or less than 0.4. 5.According to the result of experiment and previous studies, we propose the module of the depth scour hole with variations of time: h_st/H=0.9560(q^2/(gH^3 ))^0.4130 (d/H)^(-0.4448) (t_t/240)^0.0345 where hst = the maximum depth of scour at time t(m), H = drop height(m), q = per unit width of discharge(cms/m), g = gravitational constant(m/s2), d = particle size(m), tt = specified time(min). 6.By using FLOW-3D software to simulate the dimension of scour holes below a vertical drop, the equilibrium of scour depths is determined by the scour depth change rate of 0.003cm/s. The maximum depth of scour is quite consistent with the result of flume experiments after adjusting the discharge coefficient(C=0.885). 7.According to the measured data and FLOW-3D simulation, the simulation of the scour depth is deeper than the field result. It should be noted in the applications of predicting scour scales in future. | en |
| dc.description.provenance | Made available in DSpace on 2021-06-08T03:03:50Z (GMT). No. of bitstreams: 1 ntu-106-R04622020-1.pdf: 3150134 bytes, checksum: 65f9410fec10826d906f70aad31c4abe (MD5) Previous issue date: 2017 | en |
| dc.description.tableofcontents | 誌謝 I
摘要 II Abstract IV 目錄 VI 表目錄 VIII 圖目錄 IX 第一章 前言 1 第二章 文獻回顧 2 一、前人文獻 2 (一)沖刷坑特徵 2 (二)沖刷時間 6 (三)水流衝擊力 7 (四)能量損失 9 (五)FLOW-3D相關文獻 10 二、文獻分析 11 第三章 研究方法 13 一、因次分析 13 二、水槽試驗 14 (一)實驗設備 14 (二)試驗規劃 17 (三)試驗步驟 19 三、FLOW-3D模擬 20 (一)數值方法 20 (二)控制方程式 21 (三)RNG (Renormalization Group)紊流傳輸模式 23 (四)泥砂沖刷模式 25 第四章 結果與討論 30 一、水槽試驗結果 30 (一)沖刷坑深度 30 (二)沖刷坑長度 37 (三)沖刷時間 40 (四)壩基掏刷 45 (五)消能設施之影響 48 (六)水流衝擊力 49 (七)能量消減 51 (八)試驗分析與各模式之比較 53 二、FLOW-3D模擬結果 58 (一)模擬條件設定 58 (二)模擬結果 63 第五章 結論 76 參考文獻 78 | |
| dc.language.iso | zh-TW | |
| dc.subject | 垂直跌水 | zh_TW |
| dc.subject | 防砂壩 | zh_TW |
| dc.subject | FLOW-3D | zh_TW |
| dc.subject | vertical drop | en |
| dc.subject | FLOW-3D | en |
| dc.subject | Check dam | en |
| dc.title | 垂直跌水之沖刷探討 | zh_TW |
| dc.title | Scour Analysis of Vertical Drop | en |
| dc.type | Thesis | |
| dc.date.schoolyear | 105-2 | |
| dc.description.degree | 碩士 | |
| dc.contributor.oralexamcommittee | 游繁結(Fan-Chieh Yu),連惠邦(Hui-Pang Lien),詹勳全(Hsun-Chuan Chan) | |
| dc.subject.keyword | 防砂壩,垂直跌水,FLOW-3D, | zh_TW |
| dc.subject.keyword | Check dam,vertical drop,FLOW-3D, | en |
| dc.relation.page | 80 | |
| dc.identifier.doi | 10.6342/NTU201701284 | |
| dc.rights.note | 未授權 | |
| dc.date.accepted | 2017-07-13 | |
| dc.contributor.author-college | 生物資源暨農學院 | zh_TW |
| dc.contributor.author-dept | 生物環境系統工程學研究所 | zh_TW |
| 顯示於系所單位: | 生物環境系統工程學系 | |
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