本研究進行礫石型土石流之渠槽實驗，以高速攝影機及影像分析堆積顆粒受到上游供水的壓力與滲流作用下產生破壞行為及運動特性。本研究採用Voronoï Patterns 方法分析顆粒流中顆粒的速度向量及其流動特性。在顆粒流體化的過程中，前端龍頭與水非均勻混合，且顆粒在前端有集中隆起的情況。顆粒流中滲流線前後段的顆粒速度及顆粒濃度也有所差異，這些現象與現地土石流之流況相近。 本研究改變上游的供水量以及渠槽角度進行不同的實驗，並分析顆粒流上視及側視的速度剖面，與前人的數值及實驗結果進行比較。結果顯示實驗中的顆粒運動較符合Bagnold速度剖面的條件，並與礫石型土石流有相同的流動特性。 This research carries out granular flow experiments, by using high-speed camera to observe the role of particle movements caused by runoff. The flow behavior of accumulation of particles by the upstream water supply pressure and seepage, are examined and the image analysis technology to analyze the characteristics of granular flow. In this study, we use Voronoï Patterns method to analyze the velocity vector and flow characteristics of granular flow. In the process of fluidization, the combining of the particle and water is non-uniform in the snout. The particles accumulated in the snout are not saturated and the wave front becomes a bulb.
