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Hybridization of the Wave Propagation Model SWASH and the Meshfree Particle Method SPH for Real Coastal Applications

机译:波浪传播模型SWASH与无网格粒子方法SPH的混合,用于实际沿海应用

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摘要

Two computational models, Simulating WAve till SHore (SWASH) and DualSPHysics, with different computational costs and capabilities have been hybridized in this work. SWASH is a time-domain wave model based on a finite difference method for simulating nonhydrostatic, free-surface and rotational flow while DualSPHysics is a Lagrangian meshless model based on the Smoothed Particle Hydrodynamics (SPH) technique. SWASH is a reliable model to generate and propagate waves in large domains, whereas DualSPHysics is normally used in areas close to the coastline to provide a detailed description of the interaction between sea waves and coastal structures. The presented technique is a one-way coupling, with a hybridization point where the information from SWASH is passed to DualSPHysics. SWASH is used to propagate waves along the fluid domain and to calculate velocities at different depths at the position of the hybridization point. Waves in DualSPHysics are generated by means of a moving boundary (MB) whose displacement in time is reconstructed using the velocities provided by SWASH. Each particle that forms the MB is displaced with its correspondent velocity that depends on its depth. The hybridization technique is validated with experimental data and the resulting model is proved to reproduce accurately wave heights and orbital velocities. Thus, the hybrid model preserves the flexibility and capabilities of DualSPHysics with important improvements in efficiency. In addition, it simulates wave propagation even more accurately than DualSPHysics taking advantage of SWASH strengths.
机译:这项工作混合了两种计算模型,它们具有不同的计算成本和功能,分别是“模拟波浪至SHore(SWASH)”和“ DualSPHysics”。 SWASH是基于时域波动模型的时域波动模型,用于模拟非静水,自由表面和旋转流,而DualSPHysics是基于平滑粒子流体动力学(SPH)技术的拉格朗日无网格模型。 SWASH是在大范围内生成和传播海浪的可靠模型,而DualSPHysics通常用于海岸线附近的区域,以详细描述海浪与沿海结构之间的相互作用。提出的技术是一种单向耦合,具有一个混合点,其中将来自SWASH的信息传递到DualSPHysics。 SWASH用于沿流体域传播波并计算杂交点位置不同深度处的速度。 DualSPHysics中的波是通过移动边界(MB)​​生成的,移动边界的时间位移是使用SWASH提供的速度重建的。形成MB的每个粒子都以取决于其深度的相应速度位移。实验数据验证了该杂交技术的有效性,并证明了所得模型可精确再现波高和轨道速度。因此,混合模型保留了DualSPHysics的灵活性和功能,并在效率上有重要改进。此外,它利用SWASH的优势,比DualSPHysics更精确地模拟波传播。

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