Characterization of Bottom Sediments in the Rió de la Plata Estuary

Moreira, D.; Simionato, C.G.; Dragani, W.; Cayocca, F., and Luz Clara Tejedor, M., 2016. Characterization of bottom sediments in the Rió de la Plata estuary. Bottom sediments and surface water samples were collected in the intermediate and outer Rió de la Plata (RDP) estuary, South America, during 2...

Descripción completa

Guardado en:
Detalles Bibliográficos
Autores principales: Simionato, Claudia Gloria, Dragani, Walter César
Publicado: 2016
Materias:
Acceso en línea:https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_07490208_v32_n6_p1473_Moreira
http://hdl.handle.net/20.500.12110/paper_07490208_v32_n6_p1473_Moreira
Aporte de:
id paper:paper_07490208_v32_n6_p1473_Moreira
record_format dspace
spelling paper:paper_07490208_v32_n6_p1473_Moreira2025-07-30T18:21:49Z Characterization of Bottom Sediments in the Rió de la Plata Estuary Simionato, Claudia Gloria Dragani, Walter César Grain size distribution grain size trend analysis net sediment transport. sedimentology clay convergence data set estuarine sediment flocculation geometry grain size hydrodynamics regional pattern sediment analysis sediment transport sedimentology silt size distribution texture trend analysis Montevideo [Uruguay] Rio de la Plata Santa Lucia Basin Uruguay Moreira, D.; Simionato, C.G.; Dragani, W.; Cayocca, F., and Luz Clara Tejedor, M., 2016. Characterization of bottom sediments in the Rió de la Plata estuary. Bottom sediments and surface water samples were collected in the intermediate and outer Rió de la Plata (RDP) estuary, South America, during 2009-10, in six repeated cruises, with 26 stations each. Samples were processed for grain size and for water and organic matter content. The aim of this work is to analyze this new data set to provide a comprehensive and objective characterization of the bottom sediment distribution, to study the composition, and to construct a conceptual model of the involved physical mechanisms. Principal components analysis is applied to the bottom sediment size histograms to investigate the spatial patterns. Variations in grain size parameters contain information on possible sediment transport patterns, which were analyzed by means of trend vectors. Sediments show a gradational arrangement of textures: sand dominant at the head, silt in the intermediate estuary, and clayey silt and clay at its mouth. Textures become progressively more poorly sorted offshore, and the water and organic matter content increase and seem to be strongly related to the geometry and the hydrodynamics. Along the northern coast of the intermediate RDP, well-sorted medium and fine silt predominates, whereas along the southern coast, coarser and less sorted silt prevails from differences in tidal currents, in the tributaries' water pathways, or both. Around Barra del Indio, clay prevails over silt and sand, and the water and organic matter content reach a maximum, probably because of flocculation and reduction of the currents. Immediately seaward of the bottom salinity front, net transport reverses its direction, and well-sorted, coarser sand from the adjacent shelf dominates. Relict sediment is observed between the Santa Luciá River and Montevideo, consisting of poorly sorted fine silt and clay. The inferred net transport suggests convergence at the bottom salinity front, where the limit of the estuarine deposits is observed. © 2016 Coastal Education and Research Foundation, Inc. Fil:Simionato, C.G. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Dragani, W. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. 2016 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_07490208_v32_n6_p1473_Moreira http://hdl.handle.net/20.500.12110/paper_07490208_v32_n6_p1473_Moreira
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic Grain size distribution
grain size trend analysis
net sediment transport.
sedimentology
clay
convergence
data set
estuarine sediment
flocculation
geometry
grain size
hydrodynamics
regional pattern
sediment analysis
sediment transport
sedimentology
silt
size distribution
texture
trend analysis
Montevideo [Uruguay]
Rio de la Plata
Santa Lucia Basin
Uruguay
spellingShingle Grain size distribution
grain size trend analysis
net sediment transport.
sedimentology
clay
convergence
data set
estuarine sediment
flocculation
geometry
grain size
hydrodynamics
regional pattern
sediment analysis
sediment transport
sedimentology
silt
size distribution
texture
trend analysis
Montevideo [Uruguay]
Rio de la Plata
Santa Lucia Basin
Uruguay
Simionato, Claudia Gloria
Dragani, Walter César
Characterization of Bottom Sediments in the Rió de la Plata Estuary
topic_facet Grain size distribution
grain size trend analysis
net sediment transport.
sedimentology
clay
convergence
data set
estuarine sediment
flocculation
geometry
grain size
hydrodynamics
regional pattern
sediment analysis
sediment transport
sedimentology
silt
size distribution
texture
trend analysis
Montevideo [Uruguay]
Rio de la Plata
Santa Lucia Basin
Uruguay
description Moreira, D.; Simionato, C.G.; Dragani, W.; Cayocca, F., and Luz Clara Tejedor, M., 2016. Characterization of bottom sediments in the Rió de la Plata estuary. Bottom sediments and surface water samples were collected in the intermediate and outer Rió de la Plata (RDP) estuary, South America, during 2009-10, in six repeated cruises, with 26 stations each. Samples were processed for grain size and for water and organic matter content. The aim of this work is to analyze this new data set to provide a comprehensive and objective characterization of the bottom sediment distribution, to study the composition, and to construct a conceptual model of the involved physical mechanisms. Principal components analysis is applied to the bottom sediment size histograms to investigate the spatial patterns. Variations in grain size parameters contain information on possible sediment transport patterns, which were analyzed by means of trend vectors. Sediments show a gradational arrangement of textures: sand dominant at the head, silt in the intermediate estuary, and clayey silt and clay at its mouth. Textures become progressively more poorly sorted offshore, and the water and organic matter content increase and seem to be strongly related to the geometry and the hydrodynamics. Along the northern coast of the intermediate RDP, well-sorted medium and fine silt predominates, whereas along the southern coast, coarser and less sorted silt prevails from differences in tidal currents, in the tributaries' water pathways, or both. Around Barra del Indio, clay prevails over silt and sand, and the water and organic matter content reach a maximum, probably because of flocculation and reduction of the currents. Immediately seaward of the bottom salinity front, net transport reverses its direction, and well-sorted, coarser sand from the adjacent shelf dominates. Relict sediment is observed between the Santa Luciá River and Montevideo, consisting of poorly sorted fine silt and clay. The inferred net transport suggests convergence at the bottom salinity front, where the limit of the estuarine deposits is observed. © 2016 Coastal Education and Research Foundation, Inc.
author Simionato, Claudia Gloria
Dragani, Walter César
author_facet Simionato, Claudia Gloria
Dragani, Walter César
author_sort Simionato, Claudia Gloria
title Characterization of Bottom Sediments in the Rió de la Plata Estuary
title_short Characterization of Bottom Sediments in the Rió de la Plata Estuary
title_full Characterization of Bottom Sediments in the Rió de la Plata Estuary
title_fullStr Characterization of Bottom Sediments in the Rió de la Plata Estuary
title_full_unstemmed Characterization of Bottom Sediments in the Rió de la Plata Estuary
title_sort characterization of bottom sediments in the rió de la plata estuary
publishDate 2016
url https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_07490208_v32_n6_p1473_Moreira
http://hdl.handle.net/20.500.12110/paper_07490208_v32_n6_p1473_Moreira
work_keys_str_mv AT simionatoclaudiagloria characterizationofbottomsedimentsintheriodelaplataestuary
AT draganiwaltercesar characterizationofbottomsedimentsintheriodelaplataestuary
_version_ 1840326212415651840