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首页> 外文期刊>Proceedings of the Royal Society. Mathematical, physical and engineering sciences >A two-phase flow model for three-dimensional breaking waves over complex topography
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A two-phase flow model for three-dimensional breaking waves over complex topography

机译:复杂地形上三维破碎波的两相流模型

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A two-phase flow model has been developed to study three-dimensional breaking waves over complex topography, including the wave pre-breaking, overturning and post-breaking processes. The large-eddy simulation approach has been adopted in this study, where the model is based on the filtered Navier-Stokes equations with the Smagorinsky sub-grid model being used for the unresolved scales of turbulence. The governing equations have been discretized using the finite volume method, with the PISO algorithm being employed for the pressure-velocity coupling. The air-water interface has been captured using a volume of fluid method and the partial cell treatment has been implemented to deal with complex topography in the Cartesian grid. The model is first validated against available analytical solutions and experimental data for solitary wave propagation over constant water depth and three-dimensional breaking waves over a plane slope, respectively. Furthermore, the model is used to study three-dimensional overturning waves over three different bed topographies, with three-dimensional wave profiles and surface velocities being presented and discussed. The overturning jet, air entrainment and splash-up during wave breaking have been captured by the two-phase flow model, which demonstrates the capability of the model to simulate free surface flow and wave breaking problems over complex topography.
机译:已经开发了两相流模型来研究复杂地形上的三维破碎波,包括波浪的破裂前,倾覆和破裂后过程。本研究采用了大涡模拟方法,其中该模型基于过滤后的Navier-Stokes方程,其中Smagorinsky子网格模型用于未解决的湍流尺度。控制方程已使用有限体积法离散化,压力-速度耦合采用PISO算法。空气-水界面已使用一定体积的流体方法进行了捕获,并且已经实施了部分单元处理以处理笛卡尔网格中的复杂地形。首先针对可用的解析解和实验数据对模型进行验证,分别用于在恒定水深下的孤立波传播和在平面坡度上的三维破碎波。此外,该模型还用于研究三种不同床层地形上的三维倾覆波,并介绍和讨论了三维波剖面和表面速度。两相流模型已捕获了波浪破碎过程中的倾覆射流,空气夹带和飞溅,这证明了该模型在复杂地形上模拟自由表面流和波浪破碎问题的能力。

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