Morphoscopy and Morphology of Pedological Coverage at the Margins of Uruguai River, West of Santa Catarina State
Autor(a) principal: | |
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Data de Publicação: | 2016 |
Outros Autores: | , |
Tipo de documento: | Artigo |
Idioma: | por |
Título da fonte: | Anuário do Instituto de Geociências (Online) |
Texto Completo: | https://revistas.ufrj.br/index.php/aigeo/article/view/7016 |
Resumo: | Knowledge and interpretation of the sedimentary record of surface coverage and landscape soil is a valuable tool for understanding the paleoenvironment and its changes Pleistocene/Holocene why this happened during the last few thousand years of the Quaternary period. In this sense, from the pedostratigraphy and morfoestratigraphy point of view, this work intends to contribute to the understanding of the genesis of soil cover on the banks of the Uruguay River and its paleoenvironmental context that contains evidence of pre-Columbian populations along this pedogenizado stuff in Águas de Chapecó. Through morphological description and analysis morphoscopic of sands of three representative pedological profiles of low slope roofs, it is concluded that the morphoscopic analysis provided evidence of fluvial participation in both the banks of the Uruguay River where the study area is located. But the morphoscopic analysis was inefficient to distinguish the genetic origin of soil horizons in terms of allochthonous or autochthonous them. |
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Anuário do Instituto de Geociências (Online) |
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Morphoscopy and Morphology of Pedological Coverage at the Margins of Uruguai River, West of Santa Catarina StateMorfoscopia e Morfologia da Cobertura Pedológica às Margens do Rio Uruguai no Oeste de Santa CatarinaPedogeomorphology; Morphoscopy of sand; Uruguai river valley.Pedogeomorfologia; Morfoscopia de Areias; Vale do rio Uruguai.Knowledge and interpretation of the sedimentary record of surface coverage and landscape soil is a valuable tool for understanding the paleoenvironment and its changes Pleistocene/Holocene why this happened during the last few thousand years of the Quaternary period. In this sense, from the pedostratigraphy and morfoestratigraphy point of view, this work intends to contribute to the understanding of the genesis of soil cover on the banks of the Uruguay River and its paleoenvironmental context that contains evidence of pre-Columbian populations along this pedogenizado stuff in Águas de Chapecó. Through morphological description and analysis morphoscopic of sands of three representative pedological profiles of low slope roofs, it is concluded that the morphoscopic analysis provided evidence of fluvial participation in both the banks of the Uruguay River where the study area is located. But the morphoscopic analysis was inefficient to distinguish the genetic origin of soil horizons in terms of allochthonous or autochthonous them.A compreensão das coberturas superficiais é um valioso instrumento para se avaliar a influência dos fatores pedogenéticos e da paisagem no desenvolvimento e evolução das coberturas pedológicas. Nesse sentido, a partir de análises morfológicas e morfoscópicas da areia este trabalho analisou três perfis pedológicos no vale do rio Uruguai, na divisa entre Santa Catarina e Rio Grande do Sul, a fim de contribuir à gênese dessas coberturas e à participação fluvial na sua constituição. Por meio da descrição morfológica dos perfis e da análise morfoscópica de suas areias conclui-se que a despeito da textura predominantemente argilosa dos perfis existe uma heterogeneidade dos solos nesse setor do vale do rio Uruguai em escala de detalhe. A análise morfoscópica forneceu indícios da participação fluvial indiferenciada em ambos perfis de baixa vertente, associada ao aspecto polido e arredondado da maior parte dos grãos aí presentes. Enquanto o perfil de média vertente representado por Cambissolo, cuja morfoscopia da areia apresentou-se com grãos predominantemente angulosos e foscos, deve estar associado a uma cobertura de alteração in situ com pouco retrabalhamento.Universidade Federal do Rio de Janeiro2016-10-03info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://revistas.ufrj.br/index.php/aigeo/article/view/701610.11137/2016_3_71_78Anuário do Instituto de Geociências; Vol 39, No 3 (2016); 71-78Anuário do Instituto de Geociências; Vol 39, No 3 (2016); 71-781982-39080101-9759reponame:Anuário do Instituto de Geociências (Online)instname:Universidade Federal do Rio de Janeiro (UFRJ)instacron:UFRJporhttps://revistas.ufrj.br/index.php/aigeo/article/view/7016/5583Copyright (c) 2016 Anuário do Instituto de Geociênciashttp://creativecommons.org/licenses/by/4.0info:eu-repo/semantics/openAccessBertolini, William ZaneteCosta, Isael Machado daLima, Gisele Leite de2017-02-15T18:21:53Zoai:www.revistas.ufrj.br:article/7016Revistahttps://revistas.ufrj.br/index.php/aigeo/indexPUBhttps://revistas.ufrj.br/index.php/aigeo/oaianuario@igeo.ufrj.br||1982-39080101-9759opendoar:2017-02-15T18:21:53Anuário do Instituto de Geociências (Online) - Universidade Federal do Rio de Janeiro (UFRJ)false |
dc.title.none.fl_str_mv |
Morphoscopy and Morphology of Pedological Coverage at the Margins of Uruguai River, West of Santa Catarina State Morfoscopia e Morfologia da Cobertura Pedológica às Margens do Rio Uruguai no Oeste de Santa Catarina |
title |
Morphoscopy and Morphology of Pedological Coverage at the Margins of Uruguai River, West of Santa Catarina State |
spellingShingle |
Morphoscopy and Morphology of Pedological Coverage at the Margins of Uruguai River, West of Santa Catarina State Bertolini, William Zanete Pedogeomorphology; Morphoscopy of sand; Uruguai river valley. Pedogeomorfologia; Morfoscopia de Areias; Vale do rio Uruguai. |
title_short |
Morphoscopy and Morphology of Pedological Coverage at the Margins of Uruguai River, West of Santa Catarina State |
title_full |
Morphoscopy and Morphology of Pedological Coverage at the Margins of Uruguai River, West of Santa Catarina State |
title_fullStr |
Morphoscopy and Morphology of Pedological Coverage at the Margins of Uruguai River, West of Santa Catarina State |
title_full_unstemmed |
Morphoscopy and Morphology of Pedological Coverage at the Margins of Uruguai River, West of Santa Catarina State |
title_sort |
Morphoscopy and Morphology of Pedological Coverage at the Margins of Uruguai River, West of Santa Catarina State |
author |
Bertolini, William Zanete |
author_facet |
Bertolini, William Zanete Costa, Isael Machado da Lima, Gisele Leite de |
author_role |
author |
author2 |
Costa, Isael Machado da Lima, Gisele Leite de |
author2_role |
author author |
dc.contributor.author.fl_str_mv |
Bertolini, William Zanete Costa, Isael Machado da Lima, Gisele Leite de |
dc.subject.por.fl_str_mv |
Pedogeomorphology; Morphoscopy of sand; Uruguai river valley. Pedogeomorfologia; Morfoscopia de Areias; Vale do rio Uruguai. |
topic |
Pedogeomorphology; Morphoscopy of sand; Uruguai river valley. Pedogeomorfologia; Morfoscopia de Areias; Vale do rio Uruguai. |
description |
Knowledge and interpretation of the sedimentary record of surface coverage and landscape soil is a valuable tool for understanding the paleoenvironment and its changes Pleistocene/Holocene why this happened during the last few thousand years of the Quaternary period. In this sense, from the pedostratigraphy and morfoestratigraphy point of view, this work intends to contribute to the understanding of the genesis of soil cover on the banks of the Uruguay River and its paleoenvironmental context that contains evidence of pre-Columbian populations along this pedogenizado stuff in Águas de Chapecó. Through morphological description and analysis morphoscopic of sands of three representative pedological profiles of low slope roofs, it is concluded that the morphoscopic analysis provided evidence of fluvial participation in both the banks of the Uruguay River where the study area is located. But the morphoscopic analysis was inefficient to distinguish the genetic origin of soil horizons in terms of allochthonous or autochthonous them. |
publishDate |
2016 |
dc.date.none.fl_str_mv |
2016-10-03 |
dc.type.none.fl_str_mv |
|
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion |
format |
article |
status_str |
publishedVersion |
dc.identifier.uri.fl_str_mv |
https://revistas.ufrj.br/index.php/aigeo/article/view/7016 10.11137/2016_3_71_78 |
url |
https://revistas.ufrj.br/index.php/aigeo/article/view/7016 |
identifier_str_mv |
10.11137/2016_3_71_78 |
dc.language.iso.fl_str_mv |
por |
language |
por |
dc.relation.none.fl_str_mv |
https://revistas.ufrj.br/index.php/aigeo/article/view/7016/5583 |
dc.rights.driver.fl_str_mv |
Copyright (c) 2016 Anuário do Instituto de Geociências http://creativecommons.org/licenses/by/4.0 info:eu-repo/semantics/openAccess |
rights_invalid_str_mv |
Copyright (c) 2016 Anuário do Instituto de Geociências http://creativecommons.org/licenses/by/4.0 |
eu_rights_str_mv |
openAccess |
dc.format.none.fl_str_mv |
application/pdf |
dc.publisher.none.fl_str_mv |
Universidade Federal do Rio de Janeiro |
publisher.none.fl_str_mv |
Universidade Federal do Rio de Janeiro |
dc.source.none.fl_str_mv |
Anuário do Instituto de Geociências; Vol 39, No 3 (2016); 71-78 Anuário do Instituto de Geociências; Vol 39, No 3 (2016); 71-78 1982-3908 0101-9759 reponame:Anuário do Instituto de Geociências (Online) instname:Universidade Federal do Rio de Janeiro (UFRJ) instacron:UFRJ |
instname_str |
Universidade Federal do Rio de Janeiro (UFRJ) |
instacron_str |
UFRJ |
institution |
UFRJ |
reponame_str |
Anuário do Instituto de Geociências (Online) |
collection |
Anuário do Instituto de Geociências (Online) |
repository.name.fl_str_mv |
Anuário do Instituto de Geociências (Online) - Universidade Federal do Rio de Janeiro (UFRJ) |
repository.mail.fl_str_mv |
anuario@igeo.ufrj.br|| |
_version_ |
1797053545076228096 |