Use este identificador para citar ou linkar para este item: https://repositorio.ufba.br/handle/ri/18097
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dc.contributor.authorGuimarães, Junia Kacenelenbogen-
dc.contributor.authorTraini, Camille-
dc.contributor.authorSchrottke, Kerstin-
dc.contributor.authorStattegger, Karl-
dc.contributor.authorDominguez, José Maria Landim-
dc.contributor.authorVital, Helenice-
dc.contributor.authorBeserra, Diego D'Avila-
dc.contributor.authorSilva, AndréGiskard Aquino da-
dc.creatorGuimarães, Junia Kacenelenbogen-
dc.creatorTraini, Camille-
dc.creatorSchrottke, Kerstin-
dc.creatorStattegger, Karl-
dc.creatorDominguez, José Maria Landim-
dc.creatorVital, Helenice-
dc.creatorBeserra, Diego D'Avila-
dc.creatorSilva, AndréGiskard Aquino da-
dc.date.accessioned2015-10-09T18:51:00Z-
dc.date.issued2012-
dc.identifier.issn0749-0208-
dc.identifier.urihttp://repositorio.ufba.br/ri/handle/ri/18097-
dc.descriptionTexto completo: acesso restrito. p. 1580-1590pt_BR
dc.description.abstractEconomic development of the São Francisco River basin has increased by building seven river dams since the 1950s. Subsequently, strong coastal erosion reaching maximum rates of 98.6 m/year has been recorded at the river mouth, also leading to the destruction of a coastal village. This work combines discharge data with new sediment and hydro-acoustic records, collected in January 2009, to verify the impact of river damming on processes, controlling coastline evolution. Data analysis is focused on discharge evolution, morphology and sediment composition of subaqueous dunes as well as on the impact by tidal currents. Discharge has been strongly regulated since 1986, when the last river dam was implemented. Again, bedform morphology seems to be not affected neither by reduced river-discharge nor by reduced sediment supply. However, migration rates of these dunes, as calculated, are lower due to decreased discharge. At the same time, tidal impact is strengthened at the lowermost part of the river. From this we assume, that the replenishment of sediment at the coast near the river-mouth might be time-delayed, which could support coastal erosion.pt_BR
dc.language.isoenpt_BR
dc.rightsAcesso Abertopt_BR
dc.sourcehttp://dx.doi.org/10.2112/JCOASTRES-D-10-00195.1pt_BR
dc.titleMorphology of Subaqueous Dunes at the Mouth of the Dammed River São Francisco (Brazil)pt_BR
dc.title.alternativeJournal of Coastal Researchpt_BR
dc.typeArtigo de Periódicopt_BR
dc.identifier.numberv. 28, n. 6pt_BR
dc.embargo.liftdate10000-01-01-
dc.publisher.countryBrasilpt_BR
Aparece nas coleções:Artigo Publicado em Periódico (IGEO)

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