A Quasi-2D Hydro-Morphological Mathematical Model: An Application to the Argentinean Paraná River

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dc.citation.titleInternational Journal of Sediment Researches
dc.citation.volume17(1)es
dc.creatorBasile, Pedro A.
dc.creatorRiccardi, Gerardo Adrián
dc.date.accessioned2018-07-24T17:29:01Z
dc.date.available2018-07-24T17:29:01Z
dc.date.issued2002
dc.descriptionHerein a quasi-two dimensional horizontal hydro-morphological mathematical model is presented. The governing equations for the quasi-2D horizontal time-depending flow field are represented by the well-known approach of interconnected cells. New discharge laws between cells are incorporated. The model is capable of predicting temporal changes in water depth, velocity distribution, sediment transport, bed level, as well as water and suspended sediment exchange between main stream and flood plains. An application of the model in the middle reach of the Argentinean Paraná river is presented. Satisfactory results were obtained during model calibration, validation and application.es
dc.description.filUniversidad Nacional de Rosarioes
dc.formatapplication/pdf
dc.format.extent20-30es
dc.identifier.issn1001-6279es
dc.identifier.urihttp://hdl.handle.net/2133/11539
dc.language.isoenges
dc.publisherIRTCES-International Research and Training Centre on Erosion and Sedimentation. Beijing. China.es
dc.rightsopenAccesses
dc.rights.urihttp://creativecommons.org/publicdomain/zero/1.0/*
dc.subjectMorphodynamics of alluvial riverses
dc.subjectMathematical modellinges
dc.subjectParaná Riveres
dc.titleA Quasi-2D Hydro-Morphological Mathematical Model: An Application to the Argentinean Paraná Riveres
dc.typearticle
dc.typeartículo
dc.typepublishedVersion
dc.type.collectionarticulo
dc.type.versionpublishedVersiones

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