Suspended sediment transport and deposition over a dune: Río Paraná, Argentina

Autores
Kostaschuk, Ray; Shugar, Dan; Best, Jim; Parsons, Dan; Lane, Stuart; Hardy, Rich; Orfeo, Oscar
Año de publicación
2009
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
Field data from the Rio Paraná, Argentina, are used to examine patterns of suspended sediment transport over a sand dune. Measurements of three-dimensional velocity are made with an acoustic Doppler current profiler whilst suspended sediment concentration and particle size have been quantified using a laser in situ sediment scattering transmissometer. Suspended sediment concentration and streamwise and vertical sediment flux are highest close to the bed, with an upward vertical flux over the stoss side of the dune and downward flux over the lee side. Suspended sediment concentrations are higher over the crest compared with the trough and suspended sediment is coarsest near the bed. About 17% of the suspended-load transported over the crest is deposited in the lee side before it reaches the trough. Most of this deposited sand is coarser sediment that originates close to the bed over the crest, a result consistent with simulations based on the model of Mohrig and Smith (Water Resources Research 1996; 32: 3207-3217) for the excursion lengths of sediment dispersed in the lee side of a dune.
Fil: Kostaschuk, Ray. University of Guelph; Canadá
Fil: Shugar, Dan. University Fraser Simon; Canadá
Fil: Best, Jim. University of Illinois; Estados Unidos
Fil: Parsons, Dan. University Of Leeds;
Fil: Lane, Stuart. University Of Durham; Reino Unido
Fil: Hardy, Rich. University Of Durham; Reino Unido
Fil: Orfeo, Oscar. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Nordeste. Centro de Ecología Aplicada del Litoral. Universidad Nacional del Nordeste. Centro de Ecología Aplicada del Litoral; Argentina
Materia
Deposition
Dune
Rio Parana
Sand Transport
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/36750
Acceder
id CONICETDig_905320632149782115fe031b97e7c39c
oai_identifier_str oai:ri.conicet.gov.ar:11336/36750
network_acronym_str CONICETDig
repository_id_str 3498
network_name_str CONICET Digital (CONICET)
spelling Suspended sediment transport and deposition over a dune: Río Paraná, ArgentinaKostaschuk, RayShugar, DanBest, JimParsons, DanLane, StuartHardy, RichOrfeo, OscarDepositionDuneRio ParanaSand Transporthttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Field data from the Rio Paraná, Argentina, are used to examine patterns of suspended sediment transport over a sand dune. Measurements of three-dimensional velocity are made with an acoustic Doppler current profiler whilst suspended sediment concentration and particle size have been quantified using a laser in situ sediment scattering transmissometer. Suspended sediment concentration and streamwise and vertical sediment flux are highest close to the bed, with an upward vertical flux over the stoss side of the dune and downward flux over the lee side. Suspended sediment concentrations are higher over the crest compared with the trough and suspended sediment is coarsest near the bed. About 17% of the suspended-load transported over the crest is deposited in the lee side before it reaches the trough. Most of this deposited sand is coarser sediment that originates close to the bed over the crest, a result consistent with simulations based on the model of Mohrig and Smith (Water Resources Research 1996; 32: 3207-3217) for the excursion lengths of sediment dispersed in the lee side of a dune.Fil: Kostaschuk, Ray. University of Guelph; CanadáFil: Shugar, Dan. University Fraser Simon; CanadáFil: Best, Jim. University of Illinois; Estados UnidosFil: Parsons, Dan. University Of Leeds;Fil: Lane, Stuart. University Of Durham; Reino UnidoFil: Hardy, Rich. University Of Durham; Reino UnidoFil: Orfeo, Oscar. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Nordeste. Centro de Ecología Aplicada del Litoral. Universidad Nacional del Nordeste. Centro de Ecología Aplicada del Litoral; ArgentinaJohn Wiley & Sons Ltd2009-09info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/36750Kostaschuk, Ray; Shugar, Dan; Best, Jim; Parsons, Dan; Lane, Stuart; et al.; Suspended sediment transport and deposition over a dune: Río Paraná, Argentina; John Wiley & Sons Ltd; Earth Surface Processes And Landforms; 34; 12; 9-2009; 1605-16110197-9337CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/http://onlinelibrary.wiley.com/doi/10.1002/esp.1847/abstractinfo:eu-repo/semantics/altIdentifier/doi/10.1002/esp.1847info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T10:15:55Zoai:ri.conicet.gov.ar:11336/36750instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-29 10:15:55.608CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Suspended sediment transport and deposition over a dune: Río Paraná, Argentina
title Suspended sediment transport and deposition over a dune: Río Paraná, Argentina
spellingShingle Suspended sediment transport and deposition over a dune: Río Paraná, Argentina
Kostaschuk, Ray
Deposition
Dune
Rio Parana
Sand Transport
title_short Suspended sediment transport and deposition over a dune: Río Paraná, Argentina
title_full Suspended sediment transport and deposition over a dune: Río Paraná, Argentina
title_fullStr Suspended sediment transport and deposition over a dune: Río Paraná, Argentina
title_full_unstemmed Suspended sediment transport and deposition over a dune: Río Paraná, Argentina
title_sort Suspended sediment transport and deposition over a dune: Río Paraná, Argentina
dc.creator.none.fl_str_mv Kostaschuk, Ray
Shugar, Dan
Best, Jim
Parsons, Dan
Lane, Stuart
Hardy, Rich
Orfeo, Oscar
author Kostaschuk, Ray
author_facet Kostaschuk, Ray
Shugar, Dan
Best, Jim
Parsons, Dan
Lane, Stuart
Hardy, Rich
Orfeo, Oscar
author_role author
author2 Shugar, Dan
Best, Jim
Parsons, Dan
Lane, Stuart
Hardy, Rich
Orfeo, Oscar
author2_role author
author
author
author
author
author
dc.subject.none.fl_str_mv Deposition
Dune
Rio Parana
Sand Transport
topic Deposition
Dune
Rio Parana
Sand Transport
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv Field data from the Rio Paraná, Argentina, are used to examine patterns of suspended sediment transport over a sand dune. Measurements of three-dimensional velocity are made with an acoustic Doppler current profiler whilst suspended sediment concentration and particle size have been quantified using a laser in situ sediment scattering transmissometer. Suspended sediment concentration and streamwise and vertical sediment flux are highest close to the bed, with an upward vertical flux over the stoss side of the dune and downward flux over the lee side. Suspended sediment concentrations are higher over the crest compared with the trough and suspended sediment is coarsest near the bed. About 17% of the suspended-load transported over the crest is deposited in the lee side before it reaches the trough. Most of this deposited sand is coarser sediment that originates close to the bed over the crest, a result consistent with simulations based on the model of Mohrig and Smith (Water Resources Research 1996; 32: 3207-3217) for the excursion lengths of sediment dispersed in the lee side of a dune.
Fil: Kostaschuk, Ray. University of Guelph; Canadá
Fil: Shugar, Dan. University Fraser Simon; Canadá
Fil: Best, Jim. University of Illinois; Estados Unidos
Fil: Parsons, Dan. University Of Leeds;
Fil: Lane, Stuart. University Of Durham; Reino Unido
Fil: Hardy, Rich. University Of Durham; Reino Unido
Fil: Orfeo, Oscar. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Nordeste. Centro de Ecología Aplicada del Litoral. Universidad Nacional del Nordeste. Centro de Ecología Aplicada del Litoral; Argentina
description Field data from the Rio Paraná, Argentina, are used to examine patterns of suspended sediment transport over a sand dune. Measurements of three-dimensional velocity are made with an acoustic Doppler current profiler whilst suspended sediment concentration and particle size have been quantified using a laser in situ sediment scattering transmissometer. Suspended sediment concentration and streamwise and vertical sediment flux are highest close to the bed, with an upward vertical flux over the stoss side of the dune and downward flux over the lee side. Suspended sediment concentrations are higher over the crest compared with the trough and suspended sediment is coarsest near the bed. About 17% of the suspended-load transported over the crest is deposited in the lee side before it reaches the trough. Most of this deposited sand is coarser sediment that originates close to the bed over the crest, a result consistent with simulations based on the model of Mohrig and Smith (Water Resources Research 1996; 32: 3207-3217) for the excursion lengths of sediment dispersed in the lee side of a dune.
publishDate 2009
dc.date.none.fl_str_mv 2009-09
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
http://purl.org/coar/resource_type/c_6501
info:ar-repo/semantics/articulo
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/36750
Kostaschuk, Ray; Shugar, Dan; Best, Jim; Parsons, Dan; Lane, Stuart; et al.; Suspended sediment transport and deposition over a dune: Río Paraná, Argentina; John Wiley & Sons Ltd; Earth Surface Processes And Landforms; 34; 12; 9-2009; 1605-1611
0197-9337
CONICET Digital
CONICET
url http://hdl.handle.net/11336/36750
identifier_str_mv Kostaschuk, Ray; Shugar, Dan; Best, Jim; Parsons, Dan; Lane, Stuart; et al.; Suspended sediment transport and deposition over a dune: Río Paraná, Argentina; John Wiley & Sons Ltd; Earth Surface Processes And Landforms; 34; 12; 9-2009; 1605-1611
0197-9337
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/url/http://onlinelibrary.wiley.com/doi/10.1002/esp.1847/abstract
info:eu-repo/semantics/altIdentifier/doi/10.1002/esp.1847
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
dc.publisher.none.fl_str_mv John Wiley & Sons Ltd
publisher.none.fl_str_mv John Wiley & Sons Ltd
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
collection CONICET Digital (CONICET)
instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
repository.name.fl_str_mv CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas
repository.mail.fl_str_mv dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar
_version_ 1844614098591940608
score 13.070432

Publicaciones similares