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Coupling methodology for smoothed particle hydrodynamics modelling of non-linear wave-structure interactions

机译:非线性波结构相互作用的平滑粒子流体动力学建模的耦合方法

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摘要

A two-way coupling methodology for wave propagation and wave-structure interaction with SPH is hereby presented. The methodology consists of combining a fast, fully non-linear wave propagation model, OceanWave3D, with an accurate Smoothed Particle Hydrodynamics (SPH) solver, DualSPHysics. At the coupling interface in the SPH zone, moving dynamic boundary particles are applied, which move according to the horizontal velocity calculated in the wave propagation model. The surface elevation is registered in the SPH zone and transferred back to the wave propagation model. Using this coupling methodology, a large domain can be simulated with the wave propagation model, with small, discrete SPH zones embedded to locally obtain higher accuracies. The communication between the solvers is implemented using OpenMPl. Three connected processes are run: OceanWave3D, DualSPHysics and Python. The latter is used to monitor the data transfer and manipulate the data in an efficient manner. The coupling methodology is validated by simulating wave propagation of linear and non-linear waves, and comparing the surface elevations and orbital velocities to a theoretical solution. Comparison with two experimental datasets is performed as well. The coupling methodology proofs that it is able to accurately propagate waves and shows a good agreement with theoretical and experimental results.
机译:因此,提出了一种用于波传播和与SPH相互作用的波结构的双向耦合方法。该方法包括将快速,完全非线性的波传播模型OceanWave3D与精确的平滑粒子流体动力学(SPH)求解器DualSPHysics相结合。在SPH区域的耦合界面处,应用了移动的动态边界粒子,该粒子根据在波传播模型中计算的水平速度移动。地表高程记录在SPH区域中,并传回波传播模型。使用这种耦合方法,可以使用波传播模型模拟大域,并嵌入小的离散SPH区域以局部获得更高的精度。求解器之间的通信是使用OpenMP1实现的。运行三个连接的进程:OceanWave3D,DualSPHysics和Python。后者用于监视数据传输并以有效方式处理数据。通过模拟线性和非线性波的波传播,并将表面标高和轨道速度与理论解进行比较,验证了耦合方法的有效性。还与两个实验数据集进行了比较。耦合方法论证明它能够精确地传播波,并且与理论和实验结果显示出良好的一致性。

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