4.7 Article

A SPH numerical wave flume with non-reflective open boundary conditions

Journal

OCEAN ENGINEERING
Volume 163, Issue -, Pages 483-501

Publisher

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.oceaneng.2018.06.034

Keywords

Smoothed particle hydrodynamics; Numerical wave flume; Open boundary condition; Wave generation; Wave absorption; Non-reflection

Funding

  1. Scientific Research Program of Zhejiang Institute of Hydrsaulics Estuary [A17001]
  2. National Natural Science Foundation of China [51279055, 51709091]
  3. Jiangsu Natural Science Foundation of China [BK20170874]
  4. State Key Laboratory of Satellite Ocean Environment Dynamics (SOED) [SOED1609]
  5. Key laboratory of coastal Marine resources development and environmental safety in Jiangsu Province [JSCE5060]
  6. Central high education fundamental research funding [2017B00514]

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In this paper, a numerical wave flume with full functions of wave generation and absorption is proposed under the framework of Weakly Compressible Smoothed Particle Hydrodynamics (WCSPH). In contrast to the conventional SPH numerical wave flumes using wave paddles and sponge layers, the wave generation and absorption in this paper are implemented using non-reflective open boundary conditions, which are capable of generating multiple types of waves, including solitary waves, linear and second-order regular waves. Passive and active wave absorption are available for transmitting incident waves and preventing secondary reflections. Steady or unsteady flows can also be defined during wave generation and absorption to set up numerical wave-flow flumes. The results on a series of validation cases indicate that this SPH numerical wave flume not only performs satisfactorily in conventional wave generation and absorption and nonlinear wave-structure interaction simulations but also has the following three advantages: 1) It avoids using the sponge layers to shorten the flumes, which improves the efficiency; 2) it keeps the mean water level steady and prevents water level shifting; and 3) it implements steady/unsteady flow and wave-flow interactions to model a wider range of hydrodynamic problems.

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