Geoprocessing techniques to evaluate the spatial distribution of natural rain erosion potential in the Hydrographic Basin of Cachoeira Dourada Reservoir – Brazil

Detalhes bibliográficos
Autor(a) principal: CABRAL, João Batista Pereira
Data de Publicação: 2005
Outros Autores: BECEGATO, Valter Antonio, SCOPEL, Iraci, LOPES, Regina Maria
Tipo de documento: Artigo
Idioma: por
Título da fonte: Ra'e Ga (Online)
Texto Completo: https://revistas.ufpr.br/raega/article/view/4982
Resumo: Natural potential erosion were defined from their main natural conditioners in the region of hydrographic basin of Cachoeira Dourada (between Goiás and Minas Gerais states −Brazil), with geoprocessing techniques and the Universal Soil Loss Equation (USLE). Upon the decision for natural erosion potential, a matrix with values of erosivity (R), erodibility (K), declivity, and ramp length (LS) was elaborated, where classes of low, medium, high, very high, and extremely high natural erosion potential (NEP) were established. Spatial distribution for the factors R, K, LS, and PNE was defined. The highest average R index for the rainy series was 8173.50 MJ ha mm-1 h-1 year-1. The period with data from 30 years (1973 – 2002) showed that the reservoir basin displayed areas susceptible to rill and interill erosion (69.16% of the total). There is a predominance of low erosion potential among the classes, which can be explained due to the soil predominant classes as well as to the low declivity. Areas with medium to extremely high erosion potential require the adoption of measures to avoid start and development of more severe erosion processes (ravines and gullies).
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spelling Geoprocessing techniques to evaluate the spatial distribution of natural rain erosion potential in the Hydrographic Basin of Cachoeira Dourada Reservoir – BrazilUSO DE TÉCNICAS DE GEOPROCESSAMENTO PARA MAPEAR O POTENCIAL NATURAL DE EROSÃO DA CHUVA NA BACIA HIDROGRÁFICA DO RESERVATÓRIO DE CACHOEIRA DOURADA – GO/MGSolos; erodibilidade; SIG; Cachoeira Dourada(GO/MG); Soils; erodibility; GIS; Cachoeira Dourada(Brazil)Natural potential erosion were defined from their main natural conditioners in the region of hydrographic basin of Cachoeira Dourada (between Goiás and Minas Gerais states −Brazil), with geoprocessing techniques and the Universal Soil Loss Equation (USLE). Upon the decision for natural erosion potential, a matrix with values of erosivity (R), erodibility (K), declivity, and ramp length (LS) was elaborated, where classes of low, medium, high, very high, and extremely high natural erosion potential (NEP) were established. Spatial distribution for the factors R, K, LS, and PNE was defined. The highest average R index for the rainy series was 8173.50 MJ ha mm-1 h-1 year-1. The period with data from 30 years (1973 – 2002) showed that the reservoir basin displayed areas susceptible to rill and interill erosion (69.16% of the total). There is a predominance of low erosion potential among the classes, which can be explained due to the soil predominant classes as well as to the low declivity. Areas with medium to extremely high erosion potential require the adoption of measures to avoid start and development of more severe erosion processes (ravines and gullies).Definiram-se as áreas de potencial natural de erosão a partir de seus principais condicionantes naturais na bacia hidrográfica do reservatório de Cachoeira Dourada, por meio da Equação Universal de Perdas de Solos (EUPS) e de técnicas de geoprocessamento. Na decisão para definição do potencial natural de erosão (PNE) foi elaborada uma matriz com valores de erosividade (R), erodibilidade (K), declividade e comprimento de rampa (LS), na qual delimitou-se classes de baixo, médio, alto, muito alto e extremamente alto potencial natural de erosão, obtendo-se a distribuição espacial dos fatores R, K, LS e PNE. O maior índice de R médio para a série histórica foi de 8173,50 MJ ha mm-1 h-1 ano-1. Observouse que no período de trinta anos (1973 – 2002), a bacia do reservatório apresentou muitas áreas sujeitas à erosão laminar e em sulcos (69,16% do total). Entre as classes definidas, a maior parte das áreas apresenta baixo potencial natural à erosão, o que pode ser explicado pelo tipo de solo predominante e a baixa declividade. Áreas com médio a extremamente alto potencial de erosão requerem a adoção de medidas para prevenir o aparecimento e o desenvolvimento de processos erosivos mais graves (ravinas e vossorocas).UFPRCABRAL, João Batista PereiraBECEGATO, Valter AntonioSCOPEL, IraciLOPES, Regina Maria2005-12-31info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://revistas.ufpr.br/raega/article/view/498210.5380/raega.v10i0.4982RA'E GA Journal - The Geographic Space in Analysis; v. 10 (2005)RAEGA - O Espaço Geográfico em Análise; v. 10 (2005)2177-27381516-413610.5380/raega.v10i0reponame:Ra'e Ga (Online)instname:Universidade Federal do Paraná (UFPR)instacron:UFPRporhttps://revistas.ufpr.br/raega/article/view/4982/3769info:eu-repo/semantics/openAccess2018-10-18T23:36:29Zoai:revistas.ufpr.br:article/4982Revistahttps://revistas.ufpr.br/raegaPUBhttps://revistas.ufpr.br/raega/oai||raega@ufpr.br2177-27382177-2738opendoar:2018-10-18T23:36:29Ra'e Ga (Online) - Universidade Federal do Paraná (UFPR)false
dc.title.none.fl_str_mv Geoprocessing techniques to evaluate the spatial distribution of natural rain erosion potential in the Hydrographic Basin of Cachoeira Dourada Reservoir – Brazil
USO DE TÉCNICAS DE GEOPROCESSAMENTO PARA MAPEAR O POTENCIAL NATURAL DE EROSÃO DA CHUVA NA BACIA HIDROGRÁFICA DO RESERVATÓRIO DE CACHOEIRA DOURADA – GO/MG
title Geoprocessing techniques to evaluate the spatial distribution of natural rain erosion potential in the Hydrographic Basin of Cachoeira Dourada Reservoir – Brazil
spellingShingle Geoprocessing techniques to evaluate the spatial distribution of natural rain erosion potential in the Hydrographic Basin of Cachoeira Dourada Reservoir – Brazil
CABRAL, João Batista Pereira
Solos; erodibilidade; SIG; Cachoeira Dourada(GO/MG); Soils; erodibility; GIS; Cachoeira Dourada(Brazil)
title_short Geoprocessing techniques to evaluate the spatial distribution of natural rain erosion potential in the Hydrographic Basin of Cachoeira Dourada Reservoir – Brazil
title_full Geoprocessing techniques to evaluate the spatial distribution of natural rain erosion potential in the Hydrographic Basin of Cachoeira Dourada Reservoir – Brazil
title_fullStr Geoprocessing techniques to evaluate the spatial distribution of natural rain erosion potential in the Hydrographic Basin of Cachoeira Dourada Reservoir – Brazil
title_full_unstemmed Geoprocessing techniques to evaluate the spatial distribution of natural rain erosion potential in the Hydrographic Basin of Cachoeira Dourada Reservoir – Brazil
title_sort Geoprocessing techniques to evaluate the spatial distribution of natural rain erosion potential in the Hydrographic Basin of Cachoeira Dourada Reservoir – Brazil
author CABRAL, João Batista Pereira
author_facet CABRAL, João Batista Pereira
BECEGATO, Valter Antonio
SCOPEL, Iraci
LOPES, Regina Maria
author_role author
author2 BECEGATO, Valter Antonio
SCOPEL, Iraci
LOPES, Regina Maria
author2_role author
author
author
dc.contributor.none.fl_str_mv
dc.contributor.author.fl_str_mv CABRAL, João Batista Pereira
BECEGATO, Valter Antonio
SCOPEL, Iraci
LOPES, Regina Maria
dc.subject.none.fl_str_mv
dc.subject.por.fl_str_mv Solos; erodibilidade; SIG; Cachoeira Dourada(GO/MG); Soils; erodibility; GIS; Cachoeira Dourada(Brazil)
topic Solos; erodibilidade; SIG; Cachoeira Dourada(GO/MG); Soils; erodibility; GIS; Cachoeira Dourada(Brazil)
description Natural potential erosion were defined from their main natural conditioners in the region of hydrographic basin of Cachoeira Dourada (between Goiás and Minas Gerais states −Brazil), with geoprocessing techniques and the Universal Soil Loss Equation (USLE). Upon the decision for natural erosion potential, a matrix with values of erosivity (R), erodibility (K), declivity, and ramp length (LS) was elaborated, where classes of low, medium, high, very high, and extremely high natural erosion potential (NEP) were established. Spatial distribution for the factors R, K, LS, and PNE was defined. The highest average R index for the rainy series was 8173.50 MJ ha mm-1 h-1 year-1. The period with data from 30 years (1973 – 2002) showed that the reservoir basin displayed areas susceptible to rill and interill erosion (69.16% of the total). There is a predominance of low erosion potential among the classes, which can be explained due to the soil predominant classes as well as to the low declivity. Areas with medium to extremely high erosion potential require the adoption of measures to avoid start and development of more severe erosion processes (ravines and gullies).
publishDate 2005
dc.date.none.fl_str_mv 2005-12-31
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.ufpr.br/raega/article/view/4982
10.5380/raega.v10i0.4982
url https://revistas.ufpr.br/raega/article/view/4982
identifier_str_mv 10.5380/raega.v10i0.4982
dc.language.iso.fl_str_mv por
language por
dc.relation.none.fl_str_mv https://revistas.ufpr.br/raega/article/view/4982/3769
dc.rights.driver.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
dc.publisher.none.fl_str_mv UFPR
publisher.none.fl_str_mv UFPR
dc.source.none.fl_str_mv RA'E GA Journal - The Geographic Space in Analysis; v. 10 (2005)
RAEGA - O Espaço Geográfico em Análise; v. 10 (2005)
2177-2738
1516-4136
10.5380/raega.v10i0
reponame:Ra'e Ga (Online)
instname:Universidade Federal do Paraná (UFPR)
instacron:UFPR
instname_str Universidade Federal do Paraná (UFPR)
instacron_str UFPR
institution UFPR
reponame_str Ra'e Ga (Online)
collection Ra'e Ga (Online)
repository.name.fl_str_mv Ra'e Ga (Online) - Universidade Federal do Paraná (UFPR)
repository.mail.fl_str_mv ||raega@ufpr.br
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