Quasi-2D modeling of hydro-sedimentological processes in large lowland river-floodplain systems

Autores
Basile, Pedro A.; Riccardi, Gerardo A.; Garcia, Marina; Stenta, Hernán
Año de publicación
2007
Idioma
inglés
Tipo de recurso
documento de conferencia
Estado
versión publicada
Descripción
In this work a quasi two-dimensional model called CTSS8_FLUSED, suitable for the time-dependent water and fine sediment transport processes simulation in large lowland river systems, including their floodplains, is presented. Water flow and sediment equations are represented by means of the interconnected cells scheme. Different simplifications of the Saint Venant momentum equation are used to represent the discharge laws between fluvial cells. Spatially-distributed transport, deposition and erosion processes of fine sediments throughout the river-floodplain system can be simulated. The model is particularly appropriated for simulations at large space scale and for both short and long-term scale. The hydrodynamic module of the model is applied along a 205 km reach of the Paraná River, Argentina, and involving a river-floodplain area of nearly 8000 km2. Hydraulic processes in the main stream-floodplain system were simulated. The numerical simulations were carried out for both low and mean river water stages and satisfactory results were obtained during model calibration and validation.
Fil: Universidad Nacional de Rosario
Materia
Large lowland rivers
Sediment transport
Mathematical modelling
Nivel de accesibilidad
acceso abierto
Condiciones de uso
http://creativecommons.org/publicdomain/zero/1.0/
Repositorio
RepHipUNR (UNR)
Institución
Universidad Nacional de Rosario
OAI Identificador
oai:rephip.unr.edu.ar:2133/11540

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network_name_str RepHipUNR (UNR)
spelling Quasi-2D modeling of hydro-sedimentological processes in large lowland river-floodplain systemsBasile, Pedro A.Riccardi, Gerardo A.Garcia, MarinaStenta, HernánLarge lowland riversSediment transportMathematical modellingIn this work a quasi two-dimensional model called CTSS8_FLUSED, suitable for the time-dependent water and fine sediment transport processes simulation in large lowland river systems, including their floodplains, is presented. Water flow and sediment equations are represented by means of the interconnected cells scheme. Different simplifications of the Saint Venant momentum equation are used to represent the discharge laws between fluvial cells. Spatially-distributed transport, deposition and erosion processes of fine sediments throughout the river-floodplain system can be simulated. The model is particularly appropriated for simulations at large space scale and for both short and long-term scale. The hydrodynamic module of the model is applied along a 205 km reach of the Paraná River, Argentina, and involving a river-floodplain area of nearly 8000 km2. Hydraulic processes in the main stream-floodplain system were simulated. The numerical simulations were carried out for both low and mean river water stages and satisfactory results were obtained during model calibration and validation.Fil: Universidad Nacional de RosarioFacultad de Ingeniería y Ciencias Hídricas – UNL2007-11-12info:eu-repo/semantics/conferenceObjectinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_5794info:ar-repo/semantics/documentoDeConferenciaapplication/pdfhttp://hdl.handle.net/2133/11540enginfo:eu-repo/semantics/openAccesshttp://creativecommons.org/publicdomain/zero/1.0/Licencia RepHipreponame:RepHipUNR (UNR)instname:Universidad Nacional de Rosario2025-09-29T13:42:13Zoai:rephip.unr.edu.ar:2133/11540instacron:UNRInstitucionalhttps://rephip.unr.edu.ar/Universidad públicaNo correspondehttps://rephip.unr.edu.ar/oai/requestrephip@unr.edu.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:15502025-09-29 13:42:13.697RepHipUNR (UNR) - Universidad Nacional de Rosariofalse
dc.title.none.fl_str_mv Quasi-2D modeling of hydro-sedimentological processes in large lowland river-floodplain systems
title Quasi-2D modeling of hydro-sedimentological processes in large lowland river-floodplain systems
spellingShingle Quasi-2D modeling of hydro-sedimentological processes in large lowland river-floodplain systems
Basile, Pedro A.
Large lowland rivers
Sediment transport
Mathematical modelling
title_short Quasi-2D modeling of hydro-sedimentological processes in large lowland river-floodplain systems
title_full Quasi-2D modeling of hydro-sedimentological processes in large lowland river-floodplain systems
title_fullStr Quasi-2D modeling of hydro-sedimentological processes in large lowland river-floodplain systems
title_full_unstemmed Quasi-2D modeling of hydro-sedimentological processes in large lowland river-floodplain systems
title_sort Quasi-2D modeling of hydro-sedimentological processes in large lowland river-floodplain systems
dc.creator.none.fl_str_mv Basile, Pedro A.
Riccardi, Gerardo A.
Garcia, Marina
Stenta, Hernán
author Basile, Pedro A.
author_facet Basile, Pedro A.
Riccardi, Gerardo A.
Garcia, Marina
Stenta, Hernán
author_role author
author2 Riccardi, Gerardo A.
Garcia, Marina
Stenta, Hernán
author2_role author
author
author
dc.contributor.none.fl_str_mv Facultad de Ingeniería y Ciencias Hídricas – UNL
dc.subject.none.fl_str_mv Large lowland rivers
Sediment transport
Mathematical modelling
topic Large lowland rivers
Sediment transport
Mathematical modelling
dc.description.none.fl_txt_mv In this work a quasi two-dimensional model called CTSS8_FLUSED, suitable for the time-dependent water and fine sediment transport processes simulation in large lowland river systems, including their floodplains, is presented. Water flow and sediment equations are represented by means of the interconnected cells scheme. Different simplifications of the Saint Venant momentum equation are used to represent the discharge laws between fluvial cells. Spatially-distributed transport, deposition and erosion processes of fine sediments throughout the river-floodplain system can be simulated. The model is particularly appropriated for simulations at large space scale and for both short and long-term scale. The hydrodynamic module of the model is applied along a 205 km reach of the Paraná River, Argentina, and involving a river-floodplain area of nearly 8000 km2. Hydraulic processes in the main stream-floodplain system were simulated. The numerical simulations were carried out for both low and mean river water stages and satisfactory results were obtained during model calibration and validation.
Fil: Universidad Nacional de Rosario
description In this work a quasi two-dimensional model called CTSS8_FLUSED, suitable for the time-dependent water and fine sediment transport processes simulation in large lowland river systems, including their floodplains, is presented. Water flow and sediment equations are represented by means of the interconnected cells scheme. Different simplifications of the Saint Venant momentum equation are used to represent the discharge laws between fluvial cells. Spatially-distributed transport, deposition and erosion processes of fine sediments throughout the river-floodplain system can be simulated. The model is particularly appropriated for simulations at large space scale and for both short and long-term scale. The hydrodynamic module of the model is applied along a 205 km reach of the Paraná River, Argentina, and involving a river-floodplain area of nearly 8000 km2. Hydraulic processes in the main stream-floodplain system were simulated. The numerical simulations were carried out for both low and mean river water stages and satisfactory results were obtained during model calibration and validation.
publishDate 2007
dc.date.none.fl_str_mv 2007-11-12
dc.type.none.fl_str_mv info:eu-repo/semantics/conferenceObject


info:eu-repo/semantics/publishedVersion
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url http://hdl.handle.net/2133/11540
dc.language.none.fl_str_mv eng
language eng
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
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Licencia RepHip
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Licencia RepHip
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repository.name.fl_str_mv RepHipUNR (UNR) - Universidad Nacional de Rosario
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