A shoreface morphodynamic zonation and the equilibrium profile variability on the northern coastline of Rio Grande do Sul, Brazil
Autor(a) principal: | |
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Data de Publicação: | 2006 |
Outros Autores: | , , , |
Tipo de documento: | Artigo |
Idioma: | eng |
Título da fonte: | Repositório Institucional da FURG (RI FURG) |
Texto Completo: | http://repositorio.furg.br/handle/1/2119 |
Resumo: | The sedimentary distribution variation of a 60 km shoreface tract on the northern coastline of Rio Grande do Sul shows a relationship between distinct morphodynamic zones. This relationship was based on 11 beach and shoreface equilibrium profiles of up to 15 m of water depth, at 55 shoreface and 4 beach sedimentary samples. Textural variations displayed contrasting dynamics that were revealed by the distinct designs and shapes of the profiles. These were extended and taken over the closure depth (7.5 m for the area). They revealed a dissipative beach sand systems, with a shape factor of m = 0.74.Ahigh variability was identified, reflecting the erosion tendencies on this coastline segment. Statistical sedimentary parameters for such sedimentary distributions permitted the identification of two main sediment facies: (A) sandy facies: (B) muddy sand with bioclastic gravel facies. Crossshore variations show three morphodynamic zones: high energy (2 to 4 m), transitional (6 to 9 m) and low energy zones (11 to 16 m), and classifying, high, intermediate and low shoreface patterns. The morpho-sedimentary distribution defined three sections: (a) North, having moderate slope profiles (0.010) with less variability in sediment fractions, (b) Center, showing a wide range of profiles (from 0.008 to 0.010) with a finer and coarser sedimentary distribution and (c) Center-South, identifying much steeper slope (0,017) with seaward fining sediments. Morphodynamic shoreface-inner shelf boundaries (toe) were shown at 18 m at the North section, changing to 16 to 25mat the Center and Center-South sections. |
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A shoreface morphodynamic zonation and the equilibrium profile variability on the northern coastline of Rio Grande do Sul, BrazilEquilibrium profileDissipative beachesSedimentsThe sedimentary distribution variation of a 60 km shoreface tract on the northern coastline of Rio Grande do Sul shows a relationship between distinct morphodynamic zones. This relationship was based on 11 beach and shoreface equilibrium profiles of up to 15 m of water depth, at 55 shoreface and 4 beach sedimentary samples. Textural variations displayed contrasting dynamics that were revealed by the distinct designs and shapes of the profiles. These were extended and taken over the closure depth (7.5 m for the area). They revealed a dissipative beach sand systems, with a shape factor of m = 0.74.Ahigh variability was identified, reflecting the erosion tendencies on this coastline segment. Statistical sedimentary parameters for such sedimentary distributions permitted the identification of two main sediment facies: (A) sandy facies: (B) muddy sand with bioclastic gravel facies. Crossshore variations show three morphodynamic zones: high energy (2 to 4 m), transitional (6 to 9 m) and low energy zones (11 to 16 m), and classifying, high, intermediate and low shoreface patterns. The morpho-sedimentary distribution defined three sections: (a) North, having moderate slope profiles (0.010) with less variability in sediment fractions, (b) Center, showing a wide range of profiles (from 0.008 to 0.010) with a finer and coarser sedimentary distribution and (c) Center-South, identifying much steeper slope (0,017) with seaward fining sediments. Morphodynamic shoreface-inner shelf boundaries (toe) were shown at 18 m at the North section, changing to 16 to 25mat the Center and Center-South sections.2012-07-09T18:00:07Z2012-07-09T18:00:07Z2006info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articleapplication/pdfGRUBER, Nelson Luiz Sambaqui, et al. A shoreface morphodynamic zonation and the equilibrium profile variability on the northern coastline of Rio Grande do Sul, Brazil. Journal of Coastal Research, v. 39, p. 504-508, 2006. Disponível em: <http://siaiacad09.univali.br/ics2004/arquivos/100_gruber.pdf>. Acesso em: 4 jul. 2012.0749-0208http://repositorio.furg.br/handle/1/2119engGruber, Nelson Luiz SambaquiToldo Junior, Elirio ErnestinoBarboza, Eduardo GuimarãesNicolodi, João LuísZouain, Ricardo Norberto Ayupinfo:eu-repo/semantics/openAccessreponame:Repositório Institucional da FURG (RI FURG)instname:Universidade Federal do Rio Grande (FURG)instacron:FURG2023-01-24T19:19:05Zoai:repositorio.furg.br:1/2119Repositório InstitucionalPUBhttps://repositorio.furg.br/oai/request || http://200.19.254.174/oai/requestopendoar:2023-01-24T19:19:05Repositório Institucional da FURG (RI FURG) - Universidade Federal do Rio Grande (FURG)false |
dc.title.none.fl_str_mv |
A shoreface morphodynamic zonation and the equilibrium profile variability on the northern coastline of Rio Grande do Sul, Brazil |
title |
A shoreface morphodynamic zonation and the equilibrium profile variability on the northern coastline of Rio Grande do Sul, Brazil |
spellingShingle |
A shoreface morphodynamic zonation and the equilibrium profile variability on the northern coastline of Rio Grande do Sul, Brazil Gruber, Nelson Luiz Sambaqui Equilibrium profile Dissipative beaches Sediments |
title_short |
A shoreface morphodynamic zonation and the equilibrium profile variability on the northern coastline of Rio Grande do Sul, Brazil |
title_full |
A shoreface morphodynamic zonation and the equilibrium profile variability on the northern coastline of Rio Grande do Sul, Brazil |
title_fullStr |
A shoreface morphodynamic zonation and the equilibrium profile variability on the northern coastline of Rio Grande do Sul, Brazil |
title_full_unstemmed |
A shoreface morphodynamic zonation and the equilibrium profile variability on the northern coastline of Rio Grande do Sul, Brazil |
title_sort |
A shoreface morphodynamic zonation and the equilibrium profile variability on the northern coastline of Rio Grande do Sul, Brazil |
author |
Gruber, Nelson Luiz Sambaqui |
author_facet |
Gruber, Nelson Luiz Sambaqui Toldo Junior, Elirio Ernestino Barboza, Eduardo Guimarães Nicolodi, João Luís Zouain, Ricardo Norberto Ayup |
author_role |
author |
author2 |
Toldo Junior, Elirio Ernestino Barboza, Eduardo Guimarães Nicolodi, João Luís Zouain, Ricardo Norberto Ayup |
author2_role |
author author author author |
dc.contributor.author.fl_str_mv |
Gruber, Nelson Luiz Sambaqui Toldo Junior, Elirio Ernestino Barboza, Eduardo Guimarães Nicolodi, João Luís Zouain, Ricardo Norberto Ayup |
dc.subject.por.fl_str_mv |
Equilibrium profile Dissipative beaches Sediments |
topic |
Equilibrium profile Dissipative beaches Sediments |
description |
The sedimentary distribution variation of a 60 km shoreface tract on the northern coastline of Rio Grande do Sul shows a relationship between distinct morphodynamic zones. This relationship was based on 11 beach and shoreface equilibrium profiles of up to 15 m of water depth, at 55 shoreface and 4 beach sedimentary samples. Textural variations displayed contrasting dynamics that were revealed by the distinct designs and shapes of the profiles. These were extended and taken over the closure depth (7.5 m for the area). They revealed a dissipative beach sand systems, with a shape factor of m = 0.74.Ahigh variability was identified, reflecting the erosion tendencies on this coastline segment. Statistical sedimentary parameters for such sedimentary distributions permitted the identification of two main sediment facies: (A) sandy facies: (B) muddy sand with bioclastic gravel facies. Crossshore variations show three morphodynamic zones: high energy (2 to 4 m), transitional (6 to 9 m) and low energy zones (11 to 16 m), and classifying, high, intermediate and low shoreface patterns. The morpho-sedimentary distribution defined three sections: (a) North, having moderate slope profiles (0.010) with less variability in sediment fractions, (b) Center, showing a wide range of profiles (from 0.008 to 0.010) with a finer and coarser sedimentary distribution and (c) Center-South, identifying much steeper slope (0,017) with seaward fining sediments. Morphodynamic shoreface-inner shelf boundaries (toe) were shown at 18 m at the North section, changing to 16 to 25mat the Center and Center-South sections. |
publishDate |
2006 |
dc.date.none.fl_str_mv |
2006 2012-07-09T18:00:07Z 2012-07-09T18:00:07Z |
dc.type.status.fl_str_mv |
info:eu-repo/semantics/publishedVersion |
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/article |
format |
article |
status_str |
publishedVersion |
dc.identifier.uri.fl_str_mv |
GRUBER, Nelson Luiz Sambaqui, et al. A shoreface morphodynamic zonation and the equilibrium profile variability on the northern coastline of Rio Grande do Sul, Brazil. Journal of Coastal Research, v. 39, p. 504-508, 2006. Disponível em: <http://siaiacad09.univali.br/ics2004/arquivos/100_gruber.pdf>. Acesso em: 4 jul. 2012. 0749-0208 http://repositorio.furg.br/handle/1/2119 |
identifier_str_mv |
GRUBER, Nelson Luiz Sambaqui, et al. A shoreface morphodynamic zonation and the equilibrium profile variability on the northern coastline of Rio Grande do Sul, Brazil. Journal of Coastal Research, v. 39, p. 504-508, 2006. Disponível em: <http://siaiacad09.univali.br/ics2004/arquivos/100_gruber.pdf>. Acesso em: 4 jul. 2012. 0749-0208 |
url |
http://repositorio.furg.br/handle/1/2119 |
dc.language.iso.fl_str_mv |
eng |
language |
eng |
dc.rights.driver.fl_str_mv |
info:eu-repo/semantics/openAccess |
eu_rights_str_mv |
openAccess |
dc.format.none.fl_str_mv |
application/pdf |
dc.source.none.fl_str_mv |
reponame:Repositório Institucional da FURG (RI FURG) instname:Universidade Federal do Rio Grande (FURG) instacron:FURG |
instname_str |
Universidade Federal do Rio Grande (FURG) |
instacron_str |
FURG |
institution |
FURG |
reponame_str |
Repositório Institucional da FURG (RI FURG) |
collection |
Repositório Institucional da FURG (RI FURG) |
repository.name.fl_str_mv |
Repositório Institucional da FURG (RI FURG) - Universidade Federal do Rio Grande (FURG) |
repository.mail.fl_str_mv |
|
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1813187250948669440 |