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

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dc.creator Basile, Pedro A.
dc.creator Riccardi, Gerardo A.
dc.date.accessioned 2018-07-24T17:29:01Z
dc.date.available 2018-07-24T17:29:01Z
dc.date.issued 2002
dc.identifier.issn 1001-6279 es
dc.identifier.uri http://hdl.handle.net/2133/11539
dc.description Herein 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.format application/pdf
dc.format.extent 20-30 es
dc.language.iso eng es
dc.publisher IRTCES-International Research and Training Centre on Erosion and Sedimentation. Beijing. China. es
dc.rights openAccess es
dc.rights.uri http://creativecommons.org/publicdomain/zero/1.0/ *
dc.subject Morphodynamics of alluvial rivers es
dc.subject Mathematical modelling es
dc.subject Paraná River es
dc.title A Quasi-2D Hydro-Morphological Mathematical Model: An Application to the Argentinean Paraná River es
dc.type article
dc.type artículo
dc.type publishedVersion
dc.citation.title International Journal of Sediment Research es
dc.citation.volume 17(1) es
dc.description.fil Universidad Nacional de Rosario es
dc.type.collection articulo
dc.type.version publishedVersion es


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