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研究生: 劉虹廷
Liu, Hong-Ting
論文名稱: 以實驗探討水下顆粒流與水下質量體運動行為
Subaqueous mass movement –Laboratory experiments of granular avalanches
指導教授: 戴義欽
Tai, Yih-Chin
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: 2015
畢業學年度: 103
語文別: 中文
論文頁數: 109
中文關鍵詞: 顆粒流顆粒速度形貌變化粒子影像分析
外文關鍵詞: Granular flow, Particle velocity, Morphology change, Particle image velocimetry
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  • 近年來滑坡災害發生頻率逐漸增加,倘若土石流或崩塌之土體向下游移動,產生大規模陸源沉積物並迅速進入水中,形成水下土石流、海底山崩等,並引發海嘯衝擊居民生命財產安全,因此水下大型質量體運動行為成為新興且急迫的研究議題,然而水下大型質量體運動因不易觀察,多以數值方法或實驗方式進行探討,但為了有效模擬其運動行為,來推估其流動特性,本文將以實驗方式探討一二維傾斜渠道顆粒流崩落運動現象,利用高速攝影機拍攝,並透過影像處理探討其顆粒流整體流動過程。在本研究中我們藉由不同釋放位置(水上、水下)、不同量體及不同顆粒大小情況下對水下質量體運動形貌變化並加以歸類,觀察記錄顆粒流之運動行為、流動速度,除了探討其顆粒流整體流動行為,我們亦發現當釋放量體越重,形貌變化越緩慢及堆積量百分比越少;有趣的是,於水下釋放時顆粒流之平均速度均快過於水上釋放,且量體越多,其最終堆積距離也較長,此外實驗最後應用粒子影像法來量測顆粒流之流況分析,希望探討其顆粒流之完整性。

    In the last few years, landslide-disasters have occurred frequently. If debris flows or downstream happened, it’ll produce huge of terrigenous sediments which moves quickly into the water, become subaqueous debris flows, submarine landslides, and so on…… It might cause tsunamis to happen and cause serious threat to the resident and their property. Therefore, subaqueous mass movement behavior has became a current and urgent research topic. However, subaqueous mass movement is difficult to observe, so we must mostly use numerical methods or experimental approaches to investigate it.
    In order to simulate effectively its movement, and forecast its likely motion. This article will investigate two dimensional slope channel, granular flow, and collapse by scientific experiment. Using high speed cameras and image processing to discuss whole of the granular flow. In the experiment, we use different factors, such as dryness, subaqueous volume, and weight to classify subaqueous mass movement and configuration change. Observing and recording granular flow performance, and speed is necessary, not only probe granular flow movement, but we also discover that the heavier weight we add, the slower the outward appearance and the smaller percentage that it deposits. Another interesting fact is, when releasing the granular flow subaqueous, its average velocity is faster than dry. Not only this, but we also discover that the more weight you apply, the longer stacked distance you get. In addition, with the experiment using Particle image velocimetry (PIV) to measure granular flow’s flow conditions, we hope we can investigate the principles of the granular flow.

    第一章 緒論1 1.1 前言1 1.2 研究動機與目的3 1.3研究方法4 1.3.1前導研究4 1.3.2 正式研究5 第二章 文獻回顧7 第三章 實驗規劃11 3.1 實驗內容11 3.1.1 實驗儀器11 3.1.2 實驗材料14 3.1.3 實驗渠道17 3.3實驗參數19 3.3.1實驗代號19 3.3.2 實驗圖示19 3.4 實驗步驟21 3.4.1水上崩落後進入水體之實驗21 3.4.2水下崩落後進入水體之實驗22 第四章 顆粒流崩落行為之探討24 4.1水上崩落後進入水體24 4.1.1黑白混合玻璃珠顆粒流24 4.1.2不同量體黑白混合玻璃珠顆粒流比較30 4.1.3標準試驗砂顆粒流39 4.1.4 不同量體標準試驗砂顆粒流比較41 4.2水下崩落後進入水體51 4.2.1黑白混合玻璃珠顆粒流51 4.2.2不同量體水下黑白混合玻璃珠顆粒流比較54 4.2.3標準試驗砂顆粒流59 4.2.4不同量體水下準試驗砂顆粒流比較61 4.3 顆粒流形貌變化之比較結論68 4.3.1黑白混合玻顆粒流形貌變化之比較68 4.3.2標準試驗砂顆粒流形貌變化之比較71 4.3.2黑白混合玻璃珠顆粒流速度變化之比較73 4.3.3標準試驗砂顆粒流速度變化之比較77 第五章 顆粒流堆積行為之探討81 5.1 顆粒流實驗下滑堆積呈現81 5.2 相同坡度之顆粒體最終堆積距離、厚度、堆積量比較89 5.2.1顆粒流實驗之堆積距離89 5.2.2顆粒流實驗之堆積厚度及堆積量91 第六章 分層流況之分析95 6.1 水上釋放量之流況分析95 6.2 水下釋放量之流況分析96 6.3 水上釋放量與水下釋放量流況分析之結論96 6.4 滑水現象96 第七章 結論105 參考文獻 107

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