Linear Erosive Features in Cuesta Environments: a case study in the interior of paulista
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Data de Publicação: | 2020 |
Outros Autores: | |
Tipo de documento: | Artigo |
Idioma: | por |
Título da fonte: | Geografia (Londrina) |
Texto Completo: | https://ojs.uel.br/revistas/uel/index.php/geografia/article/view/39779 |
Resumo: | With the improvement of the technique, human being started to infer and modify the natural environment, especially the relief, which presents significant changes. In this sense, the present work aims to identify the evolution of linear erosive features and to evaluate in which lithological, soil and land use conditions these occur in the Cabeça River Watershed (SP). Thus, using data as a mapping of land use and occupation and linear erosive features in different periods (1988 and 2010, with field rework in 2019), the dynamics of use and occupation were analyzed, as well as their relation with the occurrence of linear erosive features. The comparative analysis of the mappings showed that the erosive ridges, ravines and gullies occur predominantly in sectors occupied by pasture, arranged over sandy lithologies and soils derived from this lithology. In addition, it was found that the use and occupation by increasing activities associated with mining and agricultural practices such as sugarcane monoculture also contribute to the occurrence of erosive processes and the appearance of these features. In this sense, it is possible to affirm that the intense use of the land added to the litho-pedological characteristics of the cuesta-depression contact, can dynamize the linear erosive processes. |
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Linear Erosive Features in Cuesta Environments: a case study in the interior of paulistaCaracterísticas Erosivas Lineales en Entornos Cuesta: un estudio de caso en el interior paulistaFeições Erosivas Lineares em Ambientes de Cuesta: estudo de caso no interior paulistaAnthropogeomorphologyGeomorphological mappingLand use and occupation.AntropogeomorfologíaMapeo geomorfológicoUso de la tierra y ocupación.AntropogeomorfologiaMapeamento geomorfológicoUso e ocupação da terra.With the improvement of the technique, human being started to infer and modify the natural environment, especially the relief, which presents significant changes. In this sense, the present work aims to identify the evolution of linear erosive features and to evaluate in which lithological, soil and land use conditions these occur in the Cabeça River Watershed (SP). Thus, using data as a mapping of land use and occupation and linear erosive features in different periods (1988 and 2010, with field rework in 2019), the dynamics of use and occupation were analyzed, as well as their relation with the occurrence of linear erosive features. The comparative analysis of the mappings showed that the erosive ridges, ravines and gullies occur predominantly in sectors occupied by pasture, arranged over sandy lithologies and soils derived from this lithology. In addition, it was found that the use and occupation by increasing activities associated with mining and agricultural practices such as sugarcane monoculture also contribute to the occurrence of erosive processes and the appearance of these features. In this sense, it is possible to affirm that the intense use of the land added to the litho-pedological characteristics of the cuesta-depression contact, can dynamize the linear erosive processes.Con la mejora de la técnica, el ser humano comenzó a inferir y modificar el entorno natural, especialmente el relieve, que presenta cambios significativos. En este sentido, el presente trabajo tiene como objetivo identificar la evolución de las características erosivas lineales y evaluar en qué condiciones litológicas, del suelo y del uso de la tierra ocurren en la cuenca del río Cabeça (SP). Por lo tanto, utilizando datos como un mapeo del uso y ocupación del suelo y características erosivas lineales en diferentes períodos (1988 y 2010, com divagaciones en el campo em 2019), se analizaron las dinámicas de uso y ocupación, así como su relación con la aparición de características erosivas lineales. El análisis comparativo de los mapeos mostró que las crestas erosivas, barrancos y quebradas ocurren predominantemente en sectores ocupados por pastizales, dispuestos sobre litologías arenosas y suelos derivados de esta litología. Además, se descubrió que el uso y la ocupación al aumentar las actividades asociadas con las prácticas mineras y agrícolas destinadas al monocultivo de la caña de azúcar también contribuyen a la aparición de procesos erosivos y la instalación de estas características. En este sentido, es posible afirmar que el uso intenso de la tierra sumado a las características lito-pedológicas del contacto cuesta-depresión, puede dinamizar los procesos erosivos lineales.Com o aprimoramento da técnica, o ser humano passou cada vez mais a interferir e modificar o ambiente natural, em especial o relevo, que apresenta significativas mudanças. Nesse sentido, o presente trabalho tem por objetivo identificar a evolução das feições erosivas lineares e avaliar em que condições litológicas, de solos e de uso da terra ocorrem na Bacia do Rio Cabeça (SP). Dessa forma, tendo como fonte de dados mapeamentos de uso e ocupação da terra e das feições erosivas lineares em períodos distintos (1988 e 2010, com reambulação em campo em 2019), foram analisadas as dinâmicas de uso e ocupação, assim como as suas relações com a ocorrência das feições erosivas lineares. A análise comparativa dos mapeamentos permitiu constatar que os sulcos erosivos, ravinas e voçorocas ocorrem predominantemente em setores ocupados por pastagem, dispostos sobre litologias arenosas e solos derivados dessa litologia. Além disso, verificou-se que o uso e ocupação por crescentes atividades associadas à mineração e práticas agrícolas voltadas à monocultura de cana-de-açúcar também contribuem para a ocorrência dos processos erosivos e para a instalação dessas feições. Nesse sentido, é possível afirmar que o intenso uso da terra, somado às características lito-pedológicas do contato cuesta-depressão, podem dinamizar os processos erosivos lineares.Universidade Estadual de Londrina2020-12-30info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionAvaliado pelos paresapplication/pdfhttps://ojs.uel.br/revistas/uel/index.php/geografia/article/view/3977910.5433/2447-1747.2021v30n1p421GEOGRAFIA (Londrina); v. 30 n. 1 (2021); 421 - 4372447-1747reponame:Geografia (Londrina)instname:Universidade Estadual de Londrina (UEL)instacron:UELporhttps://ojs.uel.br/revistas/uel/index.php/geografia/article/view/39779/28761Copyright (c) 2020 GEOGRAFIA (Londrina)http://creativecommons.org/licenses/by-nc/4.0info:eu-repo/semantics/openAccessSilva, Melina de MeloLupinacci, Cenira Maria2022-09-20T15:26:33Zoai:ojs.pkp.sfu.ca:article/39779Revistahttps://www.uel.br/revistas/uel/index.php/geografiaPUBhttps://www.uel.br/revistas/uel/index.php/geografia/oairevista.geografia.uel@gmail.com||marcar@uel.br||laudi@uel.br2447-17470102-3888opendoar:2022-09-20T15:26:33Geografia (Londrina) - Universidade Estadual de Londrina (UEL)false |
dc.title.none.fl_str_mv |
Linear Erosive Features in Cuesta Environments: a case study in the interior of paulista Características Erosivas Lineales en Entornos Cuesta: un estudio de caso en el interior paulista Feições Erosivas Lineares em Ambientes de Cuesta: estudo de caso no interior paulista |
title |
Linear Erosive Features in Cuesta Environments: a case study in the interior of paulista |
spellingShingle |
Linear Erosive Features in Cuesta Environments: a case study in the interior of paulista Silva, Melina de Melo Anthropogeomorphology Geomorphological mapping Land use and occupation. Antropogeomorfología Mapeo geomorfológico Uso de la tierra y ocupación. Antropogeomorfologia Mapeamento geomorfológico Uso e ocupação da terra. |
title_short |
Linear Erosive Features in Cuesta Environments: a case study in the interior of paulista |
title_full |
Linear Erosive Features in Cuesta Environments: a case study in the interior of paulista |
title_fullStr |
Linear Erosive Features in Cuesta Environments: a case study in the interior of paulista |
title_full_unstemmed |
Linear Erosive Features in Cuesta Environments: a case study in the interior of paulista |
title_sort |
Linear Erosive Features in Cuesta Environments: a case study in the interior of paulista |
author |
Silva, Melina de Melo |
author_facet |
Silva, Melina de Melo Lupinacci, Cenira Maria |
author_role |
author |
author2 |
Lupinacci, Cenira Maria |
author2_role |
author |
dc.contributor.author.fl_str_mv |
Silva, Melina de Melo Lupinacci, Cenira Maria |
dc.subject.por.fl_str_mv |
Anthropogeomorphology Geomorphological mapping Land use and occupation. Antropogeomorfología Mapeo geomorfológico Uso de la tierra y ocupación. Antropogeomorfologia Mapeamento geomorfológico Uso e ocupação da terra. |
topic |
Anthropogeomorphology Geomorphological mapping Land use and occupation. Antropogeomorfología Mapeo geomorfológico Uso de la tierra y ocupación. Antropogeomorfologia Mapeamento geomorfológico Uso e ocupação da terra. |
description |
With the improvement of the technique, human being started to infer and modify the natural environment, especially the relief, which presents significant changes. In this sense, the present work aims to identify the evolution of linear erosive features and to evaluate in which lithological, soil and land use conditions these occur in the Cabeça River Watershed (SP). Thus, using data as a mapping of land use and occupation and linear erosive features in different periods (1988 and 2010, with field rework in 2019), the dynamics of use and occupation were analyzed, as well as their relation with the occurrence of linear erosive features. The comparative analysis of the mappings showed that the erosive ridges, ravines and gullies occur predominantly in sectors occupied by pasture, arranged over sandy lithologies and soils derived from this lithology. In addition, it was found that the use and occupation by increasing activities associated with mining and agricultural practices such as sugarcane monoculture also contribute to the occurrence of erosive processes and the appearance of these features. In this sense, it is possible to affirm that the intense use of the land added to the litho-pedological characteristics of the cuesta-depression contact, can dynamize the linear erosive processes. |
publishDate |
2020 |
dc.date.none.fl_str_mv |
2020-12-30 |
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Avaliado pelos pares |
format |
article |
status_str |
publishedVersion |
dc.identifier.uri.fl_str_mv |
https://ojs.uel.br/revistas/uel/index.php/geografia/article/view/39779 10.5433/2447-1747.2021v30n1p421 |
url |
https://ojs.uel.br/revistas/uel/index.php/geografia/article/view/39779 |
identifier_str_mv |
10.5433/2447-1747.2021v30n1p421 |
dc.language.iso.fl_str_mv |
por |
language |
por |
dc.relation.none.fl_str_mv |
https://ojs.uel.br/revistas/uel/index.php/geografia/article/view/39779/28761 |
dc.rights.driver.fl_str_mv |
Copyright (c) 2020 GEOGRAFIA (Londrina) http://creativecommons.org/licenses/by-nc/4.0 info:eu-repo/semantics/openAccess |
rights_invalid_str_mv |
Copyright (c) 2020 GEOGRAFIA (Londrina) http://creativecommons.org/licenses/by-nc/4.0 |
eu_rights_str_mv |
openAccess |
dc.format.none.fl_str_mv |
application/pdf |
dc.publisher.none.fl_str_mv |
Universidade Estadual de Londrina |
publisher.none.fl_str_mv |
Universidade Estadual de Londrina |
dc.source.none.fl_str_mv |
GEOGRAFIA (Londrina); v. 30 n. 1 (2021); 421 - 437 2447-1747 reponame:Geografia (Londrina) instname:Universidade Estadual de Londrina (UEL) instacron:UEL |
instname_str |
Universidade Estadual de Londrina (UEL) |
instacron_str |
UEL |
institution |
UEL |
reponame_str |
Geografia (Londrina) |
collection |
Geografia (Londrina) |
repository.name.fl_str_mv |
Geografia (Londrina) - Universidade Estadual de Londrina (UEL) |
repository.mail.fl_str_mv |
revista.geografia.uel@gmail.com||marcar@uel.br||laudi@uel.br |
_version_ |
1799315432457371648 |