EFFECT OF SPATIAL-TEMPORAL VARIATION OF LAND USE AND LAND COVER ON SOIL EROSION
Autor(a) principal: | |
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Data de Publicação: | 2021 |
Outros Autores: | , , , |
Tipo de documento: | Artigo |
Idioma: | eng |
Título da fonte: | Revista Caatinga |
Texto Completo: | https://periodicos.ufersa.edu.br/caatinga/article/view/9169 |
Resumo: | Land use and land cover changes are the main factors of human influence on the erosive process. Thus, this work aimed to evaluate the effect of land use and land cover changes over 30 years on water erosion in a tropical subbasin in southeastern Brazil. The hypothesis was tested that the expansion of coffee and reforestation areas decreased soil losses due to water erosion. The Potential Erosion Method (EPM) was used to estimate water erosion in 1988, 1998, 2008 and 2018. In the first two decades, the predominant land use in the subbasin was corn, while in 2008 and 2018, coffee and reforestation areas became the main land use class in the area. The acquisition of EPM input parameters and data analysis was performed using remote sensing techniques and the Geographic Information System. Between 1988 and 1998, the total soil loss increased by 50.36 Mg year-1 due to the conversion of pasturelands to coffee plantations and the increase of deforestation. However, between 1998 and 2018, there was a soil loss reduction of 660.21 Mg year-1 (-37.46%), once the conversion of pasture and corn areas to coffee with the adoption of conservation practices, and the expansion of reforestation areas among 1988 - 2018, contributed to the decrease of soil erosion rates. |
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EFFECT OF SPATIAL-TEMPORAL VARIATION OF LAND USE AND LAND COVER ON SOIL EROSIONEFEITO DA VARIAÇÃO ESPAÇO-TEMPORAL DO USO E COBERTURA DA TERRA SOB A EROSÃO DO SOLOConservação do solo. Modelagem. Método de Erosão Potencial.Soil conservation. Modelling. Erosion Potential Method.Land use and land cover changes are the main factors of human influence on the erosive process. Thus, this work aimed to evaluate the effect of land use and land cover changes over 30 years on water erosion in a tropical subbasin in southeastern Brazil. The hypothesis was tested that the expansion of coffee and reforestation areas decreased soil losses due to water erosion. The Potential Erosion Method (EPM) was used to estimate water erosion in 1988, 1998, 2008 and 2018. In the first two decades, the predominant land use in the subbasin was corn, while in 2008 and 2018, coffee and reforestation areas became the main land use class in the area. The acquisition of EPM input parameters and data analysis was performed using remote sensing techniques and the Geographic Information System. Between 1988 and 1998, the total soil loss increased by 50.36 Mg year-1 due to the conversion of pasturelands to coffee plantations and the increase of deforestation. However, between 1998 and 2018, there was a soil loss reduction of 660.21 Mg year-1 (-37.46%), once the conversion of pasture and corn areas to coffee with the adoption of conservation practices, and the expansion of reforestation areas among 1988 - 2018, contributed to the decrease of soil erosion rates.As mudanças no uso e cobertura da terra são os principais fatores de influência humana no processo erosivo. Dessa forma, o trabalho teve como objetivo avaliar o efeito das mudanças de uso e cobertura da terra ao longo de 30 anos sob a erosão hídrica em uma sub-bacia tropical no sudeste do Brasil. Foi testada a hipótese de que a expansão das áreas de café e reflorestamento diminuíram as perdas de solo por erosão hídrica. Utilizou-se o Método de Erosão Potencial (EPM) para estimar a erosão hídrica em 1988, 1998, 2008 e 2018. Nas duas primeiras décadas, o uso da terra predominante na sub-bacia era o milho, enquanto em 2008 e 2018, o café e as áreas de reflorestamento se tornaram as principais classe de uso da terra da área. A aquisição dos parâmetros de entrada do EPM e a análise dos dados foi realizada por meio de técnicas de sensoriamento remoto e Sistema de Informações Geográficas. Entre 1988 e 1998, a perda total de solo aumentou 50,36 Mg ano-1 devido à conversão de pastagens em plantações de café e o aumento do desmatamento. Entre 1998 e 2018, houve uma redução nas perdas de solo de 660,21 Mg ano-1 (-37,46%). A conversão de áreas de pastagem e milho em cultivos de café com adoção de práticas conservacionistas e a expansão de áreas de reflorestamento entre 1988-2018 contribuíram para a diminuição das taxas de erosão do solo. Universidade Federal Rural do Semi-Árido2021-03-03info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://periodicos.ufersa.edu.br/caatinga/article/view/916910.1590/1983-21252021v34n110rcREVISTA CAATINGA; Vol. 34 No. 1 (2021); 90-98Revista Caatinga; v. 34 n. 1 (2021); 90-981983-21250100-316Xreponame:Revista Caatingainstname:Universidade Federal Rural do Semi-Árido (UFERSA)instacron:UFERSAenghttps://periodicos.ufersa.edu.br/caatinga/article/view/9169/10559Copyright (c) 2021 Revista Caatingainfo:eu-repo/semantics/openAccessLense, Guilherme Henrique ExpeditoParreiras, Taya CristoMoreira, Rodrigo SantosAvanzi, Junior CesarMincato, Ronaldo Luiz2023-07-19T12:28:39Zoai:ojs.periodicos.ufersa.edu.br:article/9169Revistahttps://periodicos.ufersa.edu.br/index.php/caatinga/indexPUBhttps://periodicos.ufersa.edu.br/index.php/caatinga/oaipatricio@ufersa.edu.br|| caatinga@ufersa.edu.br1983-21250100-316Xopendoar:2024-04-29T09:46:46.581434Revista Caatinga - Universidade Federal Rural do Semi-Árido (UFERSA)true |
dc.title.none.fl_str_mv |
EFFECT OF SPATIAL-TEMPORAL VARIATION OF LAND USE AND LAND COVER ON SOIL EROSION EFEITO DA VARIAÇÃO ESPAÇO-TEMPORAL DO USO E COBERTURA DA TERRA SOB A EROSÃO DO SOLO |
title |
EFFECT OF SPATIAL-TEMPORAL VARIATION OF LAND USE AND LAND COVER ON SOIL EROSION |
spellingShingle |
EFFECT OF SPATIAL-TEMPORAL VARIATION OF LAND USE AND LAND COVER ON SOIL EROSION Lense, Guilherme Henrique Expedito Conservação do solo. Modelagem. Método de Erosão Potencial. Soil conservation. Modelling. Erosion Potential Method. |
title_short |
EFFECT OF SPATIAL-TEMPORAL VARIATION OF LAND USE AND LAND COVER ON SOIL EROSION |
title_full |
EFFECT OF SPATIAL-TEMPORAL VARIATION OF LAND USE AND LAND COVER ON SOIL EROSION |
title_fullStr |
EFFECT OF SPATIAL-TEMPORAL VARIATION OF LAND USE AND LAND COVER ON SOIL EROSION |
title_full_unstemmed |
EFFECT OF SPATIAL-TEMPORAL VARIATION OF LAND USE AND LAND COVER ON SOIL EROSION |
title_sort |
EFFECT OF SPATIAL-TEMPORAL VARIATION OF LAND USE AND LAND COVER ON SOIL EROSION |
author |
Lense, Guilherme Henrique Expedito |
author_facet |
Lense, Guilherme Henrique Expedito Parreiras, Taya Cristo Moreira, Rodrigo Santos Avanzi, Junior Cesar Mincato, Ronaldo Luiz |
author_role |
author |
author2 |
Parreiras, Taya Cristo Moreira, Rodrigo Santos Avanzi, Junior Cesar Mincato, Ronaldo Luiz |
author2_role |
author author author author |
dc.contributor.author.fl_str_mv |
Lense, Guilherme Henrique Expedito Parreiras, Taya Cristo Moreira, Rodrigo Santos Avanzi, Junior Cesar Mincato, Ronaldo Luiz |
dc.subject.por.fl_str_mv |
Conservação do solo. Modelagem. Método de Erosão Potencial. Soil conservation. Modelling. Erosion Potential Method. |
topic |
Conservação do solo. Modelagem. Método de Erosão Potencial. Soil conservation. Modelling. Erosion Potential Method. |
description |
Land use and land cover changes are the main factors of human influence on the erosive process. Thus, this work aimed to evaluate the effect of land use and land cover changes over 30 years on water erosion in a tropical subbasin in southeastern Brazil. The hypothesis was tested that the expansion of coffee and reforestation areas decreased soil losses due to water erosion. The Potential Erosion Method (EPM) was used to estimate water erosion in 1988, 1998, 2008 and 2018. In the first two decades, the predominant land use in the subbasin was corn, while in 2008 and 2018, coffee and reforestation areas became the main land use class in the area. The acquisition of EPM input parameters and data analysis was performed using remote sensing techniques and the Geographic Information System. Between 1988 and 1998, the total soil loss increased by 50.36 Mg year-1 due to the conversion of pasturelands to coffee plantations and the increase of deforestation. However, between 1998 and 2018, there was a soil loss reduction of 660.21 Mg year-1 (-37.46%), once the conversion of pasture and corn areas to coffee with the adoption of conservation practices, and the expansion of reforestation areas among 1988 - 2018, contributed to the decrease of soil erosion rates. |
publishDate |
2021 |
dc.date.none.fl_str_mv |
2021-03-03 |
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://periodicos.ufersa.edu.br/caatinga/article/view/9169 10.1590/1983-21252021v34n110rc |
url |
https://periodicos.ufersa.edu.br/caatinga/article/view/9169 |
identifier_str_mv |
10.1590/1983-21252021v34n110rc |
dc.language.iso.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
https://periodicos.ufersa.edu.br/caatinga/article/view/9169/10559 |
dc.rights.driver.fl_str_mv |
Copyright (c) 2021 Revista Caatinga info:eu-repo/semantics/openAccess |
rights_invalid_str_mv |
Copyright (c) 2021 Revista Caatinga |
eu_rights_str_mv |
openAccess |
dc.format.none.fl_str_mv |
application/pdf |
dc.publisher.none.fl_str_mv |
Universidade Federal Rural do Semi-Árido |
publisher.none.fl_str_mv |
Universidade Federal Rural do Semi-Árido |
dc.source.none.fl_str_mv |
REVISTA CAATINGA; Vol. 34 No. 1 (2021); 90-98 Revista Caatinga; v. 34 n. 1 (2021); 90-98 1983-2125 0100-316X reponame:Revista Caatinga instname:Universidade Federal Rural do Semi-Árido (UFERSA) instacron:UFERSA |
instname_str |
Universidade Federal Rural do Semi-Árido (UFERSA) |
instacron_str |
UFERSA |
institution |
UFERSA |
reponame_str |
Revista Caatinga |
collection |
Revista Caatinga |
repository.name.fl_str_mv |
Revista Caatinga - Universidade Federal Rural do Semi-Árido (UFERSA) |
repository.mail.fl_str_mv |
patricio@ufersa.edu.br|| caatinga@ufersa.edu.br |
_version_ |
1797674028410863616 |