Geoprocessing techniques to evaluate the spatial distribution of natural rain erosion potential in the Hydrographic Basin of Cachoeira Dourada Reservoir Brazil
Autor(a) principal: | |
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Data de Publicação: | 2005 |
Outros Autores: | , , |
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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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 |
_version_ |
1799712046155038720 |