期刊
EUROPEAN JOURNAL OF MECHANICS B-FLUIDS
卷 94, 期 -, 页码 246-262出版社
ELSEVIER
DOI: 10.1016/j.euromechflu.2022.03.006
关键词
Sediment transport; Sea waves; Oscillatory boundary layer; Direct numerical simulations
资金
- Ministero dell'Istruzione dell'Univers ita e della Ricerca -MIUR, Italy [PRIN 20172B7MY]
- Office of Naval Research (U.S.A.) [12292911, N62909-17-1-2144]
- CINECA [2017174199]
- ISCRA (class B) project MOSTSEAP [HP10BEHEPJ]
- ISCRA (class C) project TURBOSEA [HP10C5SXK5]
The dynamics of sediment grains picked-up from the seabed and dragged by the oscillatory flow induced by wind waves close to the bottom is investigated. Particle-resolved direct numerical simulations are used to analyze the flow field and trajectories of spherical particles mimicking the sediment grains. The study reveals the presence of turbulent regime and explicit computation of interaction between turbulent eddies and small vortex structures shed by sediment particles.
The dynamics of sediment grains picked-up from the seabed and dragged by the oscillatory flow induced by wind waves close to the bottom is investigated for moderate values of the Shields parameter. The results of particle-resolved direct numerical simulations are analysed, which consist of the flow field and the trajectories of spherical particles mimicking the dynamics of the sediment grains. The Reynolds number of the flow is large enough to observe the turbulent regime. Moreover, the interaction between the turbulent eddies and the small vortex structures shed by the sediment particles is explicitly computed. The trajectories of the moving grains are determined by means of Newton's laws and the evaluation of the force and torque that the fluid exerts on the surface of each sediment grain.(C) 2022 Elsevier Masson SAS. All rights reserved.
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