Sedimentation rates by the 210Pb chronological method in Itanhaém river watershed, southeast Brazil
Autor(a) principal: | |
---|---|
Data de Publicação: | 2021 |
Outros Autores: | , |
Tipo de documento: | Artigo |
Idioma: | eng |
Título da fonte: | Repositório Institucional da UNESP |
Texto Completo: | http://dx.doi.org/10.1007/s10661-021-09593-y http://hdl.handle.net/11449/233819 |
Resumo: | The historical variation of sedimentation rate was investigated in five cores collected from the Itanhaém watershed main rivers, the second largest coastal watershed of the São Paulo state, Brazil, using the lead-210 radioisotope as a geochronometer. The main characteristics of the rivers’ waters and sediments were determined in order to support the geochronological analysis results and associate sediments with possible source areas. In this context, the fluvial waters’ general classification indicated the facies sulfated or chlorinated sodium in the winter and summer seasons, except for the Branco river waters in summer, which were classified as calcium or magnesium bicarbonate. A longitudinal salinity gradient was found in the downstream river courses, under greater marine influence, with the ions Cl−, Na+, SO42+, Mg2+, Ca2+, and K+ being most common in the waters. Silica is the predominant constituent in the sediment cores and is inversely related to the organic matter (OM) presence. Inverse correlations were also found between silica and other constituents. The watershed sedimentation rates were determined in the range of 0.31 up to 3.97 g/cm2/year and 0.30 up to 3.40 cm/year, highlighting the core extracted from Branco river, which showed the highest sedimentation rate. The profiles corresponding to Preto and Aguapeú rivers presented discontinuities in the sedimentation rates. The discontinuities were dated and would probably be related to the anthropic activities, which intensified in the municipality of Itanhaém around the middle of the twentieth century. |
id |
UNSP_9d41f2166b2e942aaed452df5b4f6880 |
---|---|
oai_identifier_str |
oai:repositorio.unesp.br:11449/233819 |
network_acronym_str |
UNSP |
network_name_str |
Repositório Institucional da UNESP |
repository_id_str |
2946 |
spelling |
Sedimentation rates by the 210Pb chronological method in Itanhaém river watershed, southeast BrazilCoastal watershedGeochronologyLead-210Sediment coresSedimentation rateThe historical variation of sedimentation rate was investigated in five cores collected from the Itanhaém watershed main rivers, the second largest coastal watershed of the São Paulo state, Brazil, using the lead-210 radioisotope as a geochronometer. The main characteristics of the rivers’ waters and sediments were determined in order to support the geochronological analysis results and associate sediments with possible source areas. In this context, the fluvial waters’ general classification indicated the facies sulfated or chlorinated sodium in the winter and summer seasons, except for the Branco river waters in summer, which were classified as calcium or magnesium bicarbonate. A longitudinal salinity gradient was found in the downstream river courses, under greater marine influence, with the ions Cl−, Na+, SO42+, Mg2+, Ca2+, and K+ being most common in the waters. Silica is the predominant constituent in the sediment cores and is inversely related to the organic matter (OM) presence. Inverse correlations were also found between silica and other constituents. The watershed sedimentation rates were determined in the range of 0.31 up to 3.97 g/cm2/year and 0.30 up to 3.40 cm/year, highlighting the core extracted from Branco river, which showed the highest sedimentation rate. The profiles corresponding to Preto and Aguapeú rivers presented discontinuities in the sedimentation rates. The discontinuities were dated and would probably be related to the anthropic activities, which intensified in the municipality of Itanhaém around the middle of the twentieth century.Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)Instituto de Geociências E Ciências Exatas-IGCE Universidade Estadual Paulista-UNESP, Av. 24-A No. 1515, P.O. Box 178Instituto de Biociências-IB Universidade Estadual Paulista-UNESP, Av. 24-A No. 1515, P.O. Box 178Instituto de Geociências E Ciências Exatas-IGCE Universidade Estadual Paulista-UNESP, Av. 24-A No. 1515, P.O. Box 178Instituto de Biociências-IB Universidade Estadual Paulista-UNESP, Av. 24-A No. 1515, P.O. Box 178Universidade Estadual Paulista (UNESP)Cigagna, Cristiano [UNESP]Bonotto, Daniel Marcos [UNESP]Camargo, Antonio F. Monteiro [UNESP]2022-05-01T10:35:02Z2022-05-01T10:35:02Z2021-12-01info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articlehttp://dx.doi.org/10.1007/s10661-021-09593-yEnvironmental Monitoring and Assessment, v. 193, n. 12, 2021.1573-29590167-6369http://hdl.handle.net/11449/23381910.1007/s10661-021-09593-y2-s2.0-85119452626Scopusreponame:Repositório Institucional da UNESPinstname:Universidade Estadual Paulista (UNESP)instacron:UNESPengEnvironmental Monitoring and Assessmentinfo:eu-repo/semantics/openAccess2022-05-01T10:35:02Zoai:repositorio.unesp.br:11449/233819Repositório InstitucionalPUBhttp://repositorio.unesp.br/oai/requestopendoar:29462024-08-05T21:00:32.728505Repositório Institucional da UNESP - Universidade Estadual Paulista (UNESP)false |
dc.title.none.fl_str_mv |
Sedimentation rates by the 210Pb chronological method in Itanhaém river watershed, southeast Brazil |
title |
Sedimentation rates by the 210Pb chronological method in Itanhaém river watershed, southeast Brazil |
spellingShingle |
Sedimentation rates by the 210Pb chronological method in Itanhaém river watershed, southeast Brazil Cigagna, Cristiano [UNESP] Coastal watershed Geochronology Lead-210 Sediment cores Sedimentation rate |
title_short |
Sedimentation rates by the 210Pb chronological method in Itanhaém river watershed, southeast Brazil |
title_full |
Sedimentation rates by the 210Pb chronological method in Itanhaém river watershed, southeast Brazil |
title_fullStr |
Sedimentation rates by the 210Pb chronological method in Itanhaém river watershed, southeast Brazil |
title_full_unstemmed |
Sedimentation rates by the 210Pb chronological method in Itanhaém river watershed, southeast Brazil |
title_sort |
Sedimentation rates by the 210Pb chronological method in Itanhaém river watershed, southeast Brazil |
author |
Cigagna, Cristiano [UNESP] |
author_facet |
Cigagna, Cristiano [UNESP] Bonotto, Daniel Marcos [UNESP] Camargo, Antonio F. Monteiro [UNESP] |
author_role |
author |
author2 |
Bonotto, Daniel Marcos [UNESP] Camargo, Antonio F. Monteiro [UNESP] |
author2_role |
author author |
dc.contributor.none.fl_str_mv |
Universidade Estadual Paulista (UNESP) |
dc.contributor.author.fl_str_mv |
Cigagna, Cristiano [UNESP] Bonotto, Daniel Marcos [UNESP] Camargo, Antonio F. Monteiro [UNESP] |
dc.subject.por.fl_str_mv |
Coastal watershed Geochronology Lead-210 Sediment cores Sedimentation rate |
topic |
Coastal watershed Geochronology Lead-210 Sediment cores Sedimentation rate |
description |
The historical variation of sedimentation rate was investigated in five cores collected from the Itanhaém watershed main rivers, the second largest coastal watershed of the São Paulo state, Brazil, using the lead-210 radioisotope as a geochronometer. The main characteristics of the rivers’ waters and sediments were determined in order to support the geochronological analysis results and associate sediments with possible source areas. In this context, the fluvial waters’ general classification indicated the facies sulfated or chlorinated sodium in the winter and summer seasons, except for the Branco river waters in summer, which were classified as calcium or magnesium bicarbonate. A longitudinal salinity gradient was found in the downstream river courses, under greater marine influence, with the ions Cl−, Na+, SO42+, Mg2+, Ca2+, and K+ being most common in the waters. Silica is the predominant constituent in the sediment cores and is inversely related to the organic matter (OM) presence. Inverse correlations were also found between silica and other constituents. The watershed sedimentation rates were determined in the range of 0.31 up to 3.97 g/cm2/year and 0.30 up to 3.40 cm/year, highlighting the core extracted from Branco river, which showed the highest sedimentation rate. The profiles corresponding to Preto and Aguapeú rivers presented discontinuities in the sedimentation rates. The discontinuities were dated and would probably be related to the anthropic activities, which intensified in the municipality of Itanhaém around the middle of the twentieth century. |
publishDate |
2021 |
dc.date.none.fl_str_mv |
2021-12-01 2022-05-01T10:35:02Z 2022-05-01T10:35:02Z |
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 |
http://dx.doi.org/10.1007/s10661-021-09593-y Environmental Monitoring and Assessment, v. 193, n. 12, 2021. 1573-2959 0167-6369 http://hdl.handle.net/11449/233819 10.1007/s10661-021-09593-y 2-s2.0-85119452626 |
url |
http://dx.doi.org/10.1007/s10661-021-09593-y http://hdl.handle.net/11449/233819 |
identifier_str_mv |
Environmental Monitoring and Assessment, v. 193, n. 12, 2021. 1573-2959 0167-6369 10.1007/s10661-021-09593-y 2-s2.0-85119452626 |
dc.language.iso.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
Environmental Monitoring and Assessment |
dc.rights.driver.fl_str_mv |
info:eu-repo/semantics/openAccess |
eu_rights_str_mv |
openAccess |
dc.source.none.fl_str_mv |
Scopus reponame:Repositório Institucional da UNESP instname:Universidade Estadual Paulista (UNESP) instacron:UNESP |
instname_str |
Universidade Estadual Paulista (UNESP) |
instacron_str |
UNESP |
institution |
UNESP |
reponame_str |
Repositório Institucional da UNESP |
collection |
Repositório Institucional da UNESP |
repository.name.fl_str_mv |
Repositório Institucional da UNESP - Universidade Estadual Paulista (UNESP) |
repository.mail.fl_str_mv |
|
_version_ |
1808129273474580480 |