Please use this identifier to cite or link to this item: http://repositorio.lnec.pt:8080/jspui/handle/123456789/1002261
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dc.contributor.authorPicado, A.pt_BR
dc.contributor.authorSilva, P. A.pt_BR
dc.contributor.authorFortunato, A. B.pt_BR
dc.contributor.authorDias, J. M.pt_BR
dc.date.accessioned2011-07-14T17:47:05Zpt_BR
dc.date.accessioned2014-10-20T09:51:41Zpt_BR
dc.date.accessioned2016-04-28T14:18:01Z-
dc.date.available2011-07-14T17:47:05Zpt_BR
dc.date.available2014-10-20T09:51:41Zpt_BR
dc.date.available2016-04-28T14:18:01Z-
dc.date.issued2011pt_BR
dc.identifier.issn0749-0208pt_BR
dc.identifier.urihttps://repositorio.lnec.pt/jspui/handle/123456789/1002261-
dc.description.abstractTidal currents in an estuary carry all types of dissolved, suspended or floating material. Particle tracking models constitute powerful tools in assessing the transport of this material, through the study of the particles trajectories and settling positions. Thus, this work aims at using a Lagrangian particle tracking model driven by hydrodynamic fields to study the impact of morphologic anthropogenic and natural changes in sediments transport at Ria de Aveiro. In fact, as many coastal systems, Ria de Aveiro is in progressive degradation associated to the lack of maintenance and to the strong currents occurring in its channels, which erode their protective walls. Hence, the model VELApart, which is driven by the hydrodynamic model ELCIRC (previously calibrated for this lagoon), was applied for two configurations of the Ria de Aveiro: one representing the present situation of the lagoon and another representing a scenario with the enlargement of its flooded area. According to model results, morphologic changes influence the sediments pathways and final position, as well as the settling time. Generally for the flooded bathymetry the sediments travel a longer distance and the preferential zones of deposition are inside the flooded area, while for the present configuration sediments settle down in the main adjacent channels. The settling times also increase with the enlargement of the flooded area.pt_BR
dc.language.isoengpt_BR
dc.rightsrestrictedAccesspt_BR
dc.subjectFlooded areaspt_BR
dc.subjectSediments transportpt_BR
dc.subjectSediments pathwaypt_BR
dc.subjectSettling timept_BR
dc.titleParticle tracking-modeling of morphologic changes in the Ria de Aveiropt_BR
dc.typeworkingPaperpt_BR
dc.description.pages1560 - 1564pt_BR
dc.description.sectorDHA/NECpt_BR
dc.description.magazineJournal of Coastal Research, ICS2011 (Proceedings)pt_BR
Appears in Collections:DHA/NEC - Comunicações a congressos e artigos de revista

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