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dc.contributor.authorEl Rahi, Joe
dc.contributor.authorMartinez Estevez, Iván 
dc.contributor.authorTagliafierro, Bonaventura
dc.contributor.authorDomínguez Alonso, José Manuel 
dc.contributor.authorCabrera Crespo, Alejandro Jacobo 
dc.contributor.authorStratigaki, Vasiliki
dc.contributor.authorSuzuki, Tomohiro
dc.contributor.authorTroch, Peter
dc.date.accessioned2024-05-23T08:33:20Z
dc.date.available2024-05-23T08:33:20Z
dc.date.issued2023-10-01
dc.identifier.citationOcean Engineering, 285. (1): 115227 (2023)spa
dc.identifier.issn00298018
dc.identifier.urihttp://hdl.handle.net/11093/6856
dc.description.abstractVegetation meadows in coastal waters are a key constituent of a future green defense package due to the ecosystem services they provide and the potential to attenuate wave energy. To numerically describe the vegetation dynamics under wave action, this paper presents a novel application of a numerical coupling for solving fluid–elastic structure interactions (FSI) problems involving ultra-thin elements in a 3-D environment. The extended two-way coupling employed in this work combines the mesh-free Smoothed Particle Hydrodynamics (SPH) method in the DualSPHysics code to solve the fluid flow, and the Finite Element Analysis (FEA) structural solver in Project Chrono to solve the structural dynamics. To represent the vegetation, a flexible structure based on the Euler–Bernoulli beam model is used. The beam element is embedded into the SPH domain using an envelope subdomain that is discretized using dummy boundary particles. As such, this dummy envelope serves as a decoupling interface for the geometrical properties of the structure, allowing for ultra-thin structures smaller than the initial inter-particle distance (dp). The numerical approach is validated against an experimental setup including a flexible blade swaying under the action of an oscillatory flow. The results demonstrate that the numerical model is able to resolve the wave–vegetation interaction problem. Furthermore, additional insights into the blade dynamics reveal that the swaying velocity increases linearly along the length, with the upper part swaying at a speed comparable to the fluid velocity while the stem remains relatively stationary. Additionally, the findings indicate that rigid vegetation experiences higher forces per unit length, and in systems with substantial swaying motion, energy dissipation predominantly occurs around the lower base of the vegetationen
dc.language.isoengspa
dc.publisherOcean Engineeringspa
dc.rightsAtribución 4.0 Internacional
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/
dc.titleNumerical investigation of wave-induced flexible vegetation dynamics in 3D using a coupling between DualSPHysics and the FEA module of Project Chronoen
dc.typearticlespa
dc.rights.accessRightsclosedAccessspa
dc.identifier.doi10.1016/j.oceaneng.2023.115227
dc.identifier.editorhttps://linkinghub.elsevier.com/retrieve/pii/S0029801823016116spa
dc.publisher.departamentoFísica aplicadaspa
dc.publisher.grupoinvestigacionEphysLabspa
dc.subject.unesco22 Físicaspa
dc.subject.unesco3301.12 Hidrodinámicaspa
dc.subject.unesco2299 Otras Especialidades Físicasspa
dc.date.updated2023-10-23T14:55:39Z
dc.computerCitationpub_title=Ocean Engineering|volume=285|journal_number=1|start_pag=115227|end_pag=spa


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    Atribución 4.0 Internacional
    Except where otherwise noted, this item's license is described as Atribución 4.0 Internacional