Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/118736
DC FieldValueLanguage
dc.contributorDepartment of Civil and Environmental Engineeringen_US
dc.creatorRahmani, Aen_US
dc.creatorStocchino, Aen_US
dc.date.accessioned2026-05-15T06:05:05Z-
dc.date.available2026-05-15T06:05:05Z-
dc.identifier.issn0272-7714en_US
dc.identifier.urihttp://hdl.handle.net/10397/118736-
dc.language.isoenen_US
dc.publisherAcademic Pressen_US
dc.subjectDispersion regimesen_US
dc.subjectEulerian–Lagrangianen_US
dc.subjectInertial particleen_US
dc.subjectMicroplasticsen_US
dc.subjectNearshore hydrodynamicsen_US
dc.subjectParticle dispersionen_US
dc.titleEulerian–Lagrangian simulation of wave-induced microplastic dispersion in nearshore zones : processes and implicationsen_US
dc.typeJournal/Magazine Articleen_US
dc.identifier.volume328en_US
dc.identifier.doi10.1016/j.ecss.2025.109626en_US
dcterms.abstractMicroplastics are a pervasive marine pollutant, threatening coastal ecosystems and biodiversity. Understanding nearshore transport and dispersion is crucial for predicting microplastics’ fate and mitigating impacts. This study employs an Eulerian–Lagrangian model to simulate spherical microplastics, accounting for inertia and buoyancy, under regular and irregular waves in the nearshore region. Using realistic size–density distributions, the simulated particles range from non-buoyant to buoyant and from weakly to highly inertial. The shear layer, formed by Stokes drift and undertow, drives buoyant microplastics shoreward, controlling non-buoyant trajectories. The breaking region acts as a natural barrier, with few low-density, inertial particles passing through and potentially settling above the swash zone, while non-passing particles accumulate in the shoaling zone. Particle–wave characteristics are linked through dimensionless parameters, and we propose applicable dimensionless diffusive coefficients of K<inf>h</inf>(1)T/L<inf>0</inf>2≈O(10−4) and K<inf>v</inf>(1)T/L<inf>0</inf>2≈O(10−5). Dispersion regimes transit from initial ballistic to subdiffusive within 10 wave periods. The subsequent superdiffusive regime is governed primarily by wave steepness and weakly by depth, particle density, and size. However, the absence of a sustained diffusive regime indicates diffusion coefficients may misestimate nearshore microplastic concentrations.en_US
dcterms.accessRightsembargoed accessen_US
dcterms.bibliographicCitationEstuarine, coastal and shelf science, Jan. 2026, v. 328, 109626en_US
dcterms.isPartOfEstuarine, coastal and shelf scienceen_US
dcterms.issued2026-01-
dc.identifier.scopus2-s2.0-105022790993-
dc.identifier.artn109626en_US
dc.description.validate202605 bchyen_US
dc.description.oaNot applicableen_US
dc.identifier.SubFormIDG001579/2026-01-
dc.description.fundingSourceRGCen_US
dc.description.fundingTextThis work was also partially supported by the Research Grants Council of the Hong Kong Special Administrative Region, China (GRF Project Reference Number: 15216422)en_US
dc.description.pubStatusPublisheden_US
dc.date.embargo2028-01-31en_US
dc.description.oaCategoryGreen (AAM)en_US
Appears in Collections:Journal/Magazine Article
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