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  1. National Taiwan Ocean University Research Hub
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Please use this identifier to cite or link to this item: http://scholars.ntou.edu.tw/handle/123456789/26537
DC FieldValueLanguage
dc.contributor.authorSahoo, Gaganen_US
dc.contributor.authorBehera, Harekrushnaen_US
dc.contributor.authorHsu, Tai-Wenen_US
dc.date.accessioned2026-03-12T03:49:05Z-
dc.date.available2026-03-12T03:49:05Z-
dc.date.issued2026/3/1-
dc.identifier.issn0955-7997-
dc.identifier.urihttp://scholars.ntou.edu.tw/handle/123456789/26537-
dc.description.abstractCapillary-gravity waves, influenced by both surface tension and gravity, interact strongly with marine structures, especially in the presence of uniform currents. Despite extensive studies on wave scattering by porous structures, the combined effects of surface tension, current, and porous barriers over a porous bottom remain insufficiently explored. This study examines the scattering of such waves by two thin surface-piercing porous barriers in the presence of a uniform current over a porous sea bed. A linear wave-structure interaction model is solved numerically through a hybrid Boundary Element-Finite Difference Method (BEM-FDM) and analytically through an eigenfunction expansion combined with a least-squares approach. The hybrid BEM-FDM efficiently handles higher-order boundary conditions that cannot be directly addressed by conventional BEM, while the analytical method eliminates the need for eigenfunction orthogonality and explicit mode coupling. The effects of surface tension, current velocity and direction, porous effect parameters of barriers as well as bottom, barrier length and spacing between them on reflection, transmission, and energy dissipation are analyzed. Results show that surface tension enhances reflection and dissipation while reducing transmission. Current direction strongly affects scattering: following currents enhance transmission, whereas opposing currents increase reflection and dissipation. Longer barriers and larger porous-effect parameters of both porous barriers and porous bottom enhance energy dissipation, while spacing between porous barriers induce interference driven oscillations.en_US
dc.language.isoEnglishen_US
dc.publisherELSEVIER SCI LTDen_US
dc.relation.ispartofENGINEERING ANALYSIS WITH BOUNDARY ELEMENTSen_US
dc.subjectSurface tensionen_US
dc.subjectFollowing and opposing currenten_US
dc.subjectPorous sea beden_US
dc.subjectSurface-piercing porous barriersen_US
dc.subjectResonance phenomenaen_US
dc.titleScattering of capillary-gravity waves by surface-piercing porous barriers in the presence of uniform current over a porous sea beden_US
dc.typejournal articleen_US
dc.identifier.doi10.1016/j.enganabound.2026.106646-
dc.identifier.isiWOS:001671095800001-
dc.relation.journalvolume184en_US
dc.relation.pages19en_US
dc.identifier.eissn1873-197X-
item.grantfulltextnone-
item.cerifentitytypePublications-
item.languageiso639-1English-
item.openairetypejournal article-
item.fulltextno fulltext-
item.openairecristypehttp://purl.org/coar/resource_type/c_6501-
crisitem.author.deptCollege of Engineering-
crisitem.author.deptDepartment of Harbor and River Engineering-
crisitem.author.deptNational Taiwan Ocean University,NTOU-
crisitem.author.deptCenter of Excellence for Ocean Engineering-
crisitem.author.deptDoctorate Degree Program in Ocean Engineering and Technology-
crisitem.author.deptOcean Energy and Engineering Technology-
crisitem.author.orcid0000-0003-3784-7179-
crisitem.author.parentorgNational Taiwan Ocean University,NTOU-
crisitem.author.parentorgCollege of Engineering-
crisitem.author.parentorgNational Taiwan Ocean University,NTOU-
crisitem.author.parentorgCollege of Engineering-
crisitem.author.parentorgCenter of Excellence for Ocean Engineering-
Appears in Collections:河海工程學系
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