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Impulsive plunging wave breaking downstream of a bump in a shallow water flume - Part II: Numerical simulations

机译:冲破浅水槽凸块下游的冲击波-第二部分:数值模拟

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Part II of this two-part paper presents the simulation results of the plunging wave-breaking generated by impulsive flow over a submerged bump fixed in a shallow water flume using the exact experimental initial and boundary conditions provided in Part I of this study. The overall plunging wave breaking process is described with major wave breaking events identified: jet plunge, oblique splash and vertical jet. These major events repeat up to four times before entering the chaotic breaking phase. The plunging wave breaking process of the simulations shows a similar time line as the experiments consisting of startup, steep wave formation, plunging wave, and chaotic wave breaking swept downstream time phases. Wave breaking profile, air entrainment, velocity, vorticity, flume bottom pressure, and energy are analyzed and compared with the experimental results. The simulations qualitatively predict all four time phases, all four plunging events and their sub-events. The wave profile and location at the maximum height is very close to the experiment results. The flume flow and velocity demonstrate the same flow trend as the experiments but with reduced velocity magnitudes. The simulations show similar bottom pressure to the experiments but with large oscillations, and the post-breaking water elevations are larger as compared to the experimental results.
机译:这份由两部分组成的论文的第二部分介绍了使用本研究第一部分中提供的确切实验初始条件和边界条件,模拟了由固定在浅水槽中的浸入式凸块上的冲击流产生的突波破坏的模拟结果。描述了整个突波破碎过程,并确定了主要的突波事件:喷射骤降,倾斜飞溅和垂直喷射。在进入混乱的破坏阶段之前,这些主要事件最多重复四次。仿真的突波破碎过程显示了与实验类似的时间线,包括启动,陡峭的波形成,突波和混沌波破碎,席卷了下游时间阶段。分析了波浪的断面,空气夹带,速度,涡旋,水槽底部压力和能量,并与实验结果进行了比较。模拟定性地预测了所有四个时间阶段,所有四个暴跌事件及其子事件。最大高度处的波轮廓和位置非常接近实验结果。水槽的流量和速度显示出与实验相同的流量趋势,但速度幅度减小。模拟显示出与实验相似的底部压力,但振荡较大,并且与实验结果相比,破裂后的水位高。

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