Runoff measurement and prediction for a watershed under natural vegetation in central Brazil
Autor(a) principal: | |
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Data de Publicação: | 1999 |
Outros Autores: | |
Tipo de documento: | Artigo |
Idioma: | eng |
Título da fonte: | Repositório Institucional da UnB |
Texto Completo: | http://repositorio.unb.br/handle/10482/25500 https://dx.doi.org/10.1590/S0100-06831999000300024 |
Resumo: | This work aimed to measure and analyze total rainfall (P), rainfall intensity and five-day antecedent rainfall effects on runoff (R); to compare measured and simulated R values using the Soil Conservation Service Curve Number method (CN) for each rainfall event; and to establish average R/P ratios for observed R values. A one-year (07/01/96 to 06/30/97) rainfall-runoff data study was carried out in the Capetinga watershed (962.4 ha), located at the Federal District of Brazil, 47° 52' longitude West and 15° 52' latitude South. Soils of the watershed were predominantly covered by natural vegetation. Total rainfall and runoff for the period were 1,744 and 52.5 mm, respectively, providing R/P of 3% and suggesting that watershed physical characteristics favored water infiltration into the soil. A multivariate regression analysis for 31 main rainfall-runoff events totaling 781.9 and 51.0 mm, respectively, indicated that the amount of runoff was only dependent upon rainfall volume. Simulated values of total runoff were underestimated about 15% when using CN method and an area-weighted average of the CN based on published values. On the other hand, when average values of CN were calculated for the watershed, total runoff was overestimated about 39%, suggesting that CN method shoud be used with care in areas under natural vegetation. |
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Runoff measurement and prediction for a watershed under natural vegetation in central BrazilMedição e simulação do escoamento superficial para uma microbacia hidrográfica sob vegetação natural localizada no centro-oeste brasileiroMétodo da curva númeroInfiltração de águaRelação escoamentoThis work aimed to measure and analyze total rainfall (P), rainfall intensity and five-day antecedent rainfall effects on runoff (R); to compare measured and simulated R values using the Soil Conservation Service Curve Number method (CN) for each rainfall event; and to establish average R/P ratios for observed R values. A one-year (07/01/96 to 06/30/97) rainfall-runoff data study was carried out in the Capetinga watershed (962.4 ha), located at the Federal District of Brazil, 47° 52' longitude West and 15° 52' latitude South. Soils of the watershed were predominantly covered by natural vegetation. Total rainfall and runoff for the period were 1,744 and 52.5 mm, respectively, providing R/P of 3% and suggesting that watershed physical characteristics favored water infiltration into the soil. A multivariate regression analysis for 31 main rainfall-runoff events totaling 781.9 and 51.0 mm, respectively, indicated that the amount of runoff was only dependent upon rainfall volume. Simulated values of total runoff were underestimated about 15% when using CN method and an area-weighted average of the CN based on published values. On the other hand, when average values of CN were calculated for the watershed, total runoff was overestimated about 39%, suggesting that CN method shoud be used with care in areas under natural vegetation.Este trabalho objetivou medir e analisar o efeito das variáveis total precipitado (P), intensidade de chuva e precipitação antecedente em cinco dias, no escoamento superficial (R); comparar valores observados e simulados de R, usando o método da Curva Número (CN), proposto pelo Serviço de Conservação de Solos dos EUA, e estabelecer a relação R/P. No período de 01/07/96 a 30/06/97, foram medidos a precipitação (1.744 mm) e o escoamento superficial (52,5 mm) na microbacia do Córrego Capetinga (964,2 ha), localizada no Distrito Federal. A cobertura vegetal da microbacia é predominantemente natural, constituída de cerrados, campo-cerrado, campo sujo e campo limpo. Em virtude do pequeno volume de escoamento superficial, evidenciaram-se boas características para infiltração na microbacia, haja vista que, no período analisado, a relação R/P foi apenas de 3%. Uma análise de regressão multivariada das 31 principais chuvas, totalizando 781,9 mm as quais provocaram um escoamento de 51,0 mm, indicou que o escoamento dependeu somente da magnitude de cada chuva. Tomando valores da curva número (CN), dados pelos manuais de hidrologia a serem usados no método de mesmo nome e selecionados em função das características edafogeológicas e vegetativas da microbacia, verificou-se uma subestimativa nos valores simulados do escoamento superficial total de 15%, quando comparados com os valores observados. Utilizando valores de CN calculados para a microbacia, o método superestimou os resultados em 39%. Em razão dessas discrepâncias, recomenda-se cautela no uso desse método em áreas sob vegetação natural.Em processamentoSociedade Brasileira de Ciência do Solo2017-12-07T04:31:42Z2017-12-07T04:31:42Z1999info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articleapplication/pdfRev. Bras. Ciênc. Solo,v.23,n.3,p.695-701,1999http://repositorio.unb.br/handle/10482/25500https://dx.doi.org/10.1590/S0100-06831999000300024Silva, C. L.Oliveira, C. A. S.info:eu-repo/semantics/openAccessengreponame:Repositório Institucional da UnBinstname:Universidade de Brasília (UnB)instacron:UNB2024-08-28T16:32:44Zoai:repositorio.unb.br:10482/25500Repositório InstitucionalPUBhttps://repositorio.unb.br/oai/requestrepositorio@unb.bropendoar:2024-08-28T16:32:44Repositório Institucional da UnB - Universidade de Brasília (UnB)false |
dc.title.none.fl_str_mv |
Runoff measurement and prediction for a watershed under natural vegetation in central Brazil Medição e simulação do escoamento superficial para uma microbacia hidrográfica sob vegetação natural localizada no centro-oeste brasileiro |
title |
Runoff measurement and prediction for a watershed under natural vegetation in central Brazil |
spellingShingle |
Runoff measurement and prediction for a watershed under natural vegetation in central Brazil Silva, C. L. Método da curva número Infiltração de água Relação escoamento |
title_short |
Runoff measurement and prediction for a watershed under natural vegetation in central Brazil |
title_full |
Runoff measurement and prediction for a watershed under natural vegetation in central Brazil |
title_fullStr |
Runoff measurement and prediction for a watershed under natural vegetation in central Brazil |
title_full_unstemmed |
Runoff measurement and prediction for a watershed under natural vegetation in central Brazil |
title_sort |
Runoff measurement and prediction for a watershed under natural vegetation in central Brazil |
author |
Silva, C. L. |
author_facet |
Silva, C. L. Oliveira, C. A. S. |
author_role |
author |
author2 |
Oliveira, C. A. S. |
author2_role |
author |
dc.contributor.author.fl_str_mv |
Silva, C. L. Oliveira, C. A. S. |
dc.subject.por.fl_str_mv |
Método da curva número Infiltração de água Relação escoamento |
topic |
Método da curva número Infiltração de água Relação escoamento |
description |
This work aimed to measure and analyze total rainfall (P), rainfall intensity and five-day antecedent rainfall effects on runoff (R); to compare measured and simulated R values using the Soil Conservation Service Curve Number method (CN) for each rainfall event; and to establish average R/P ratios for observed R values. A one-year (07/01/96 to 06/30/97) rainfall-runoff data study was carried out in the Capetinga watershed (962.4 ha), located at the Federal District of Brazil, 47° 52' longitude West and 15° 52' latitude South. Soils of the watershed were predominantly covered by natural vegetation. Total rainfall and runoff for the period were 1,744 and 52.5 mm, respectively, providing R/P of 3% and suggesting that watershed physical characteristics favored water infiltration into the soil. A multivariate regression analysis for 31 main rainfall-runoff events totaling 781.9 and 51.0 mm, respectively, indicated that the amount of runoff was only dependent upon rainfall volume. Simulated values of total runoff were underestimated about 15% when using CN method and an area-weighted average of the CN based on published values. On the other hand, when average values of CN were calculated for the watershed, total runoff was overestimated about 39%, suggesting that CN method shoud be used with care in areas under natural vegetation. |
publishDate |
1999 |
dc.date.none.fl_str_mv |
1999 2017-12-07T04:31:42Z 2017-12-07T04:31:42Z |
dc.type.status.fl_str_mv |
info:eu-repo/semantics/publishedVersion |
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/article |
format |
article |
status_str |
publishedVersion |
dc.identifier.uri.fl_str_mv |
Rev. Bras. Ciênc. Solo,v.23,n.3,p.695-701,1999 http://repositorio.unb.br/handle/10482/25500 https://dx.doi.org/10.1590/S0100-06831999000300024 |
identifier_str_mv |
Rev. Bras. Ciênc. Solo,v.23,n.3,p.695-701,1999 |
url |
http://repositorio.unb.br/handle/10482/25500 https://dx.doi.org/10.1590/S0100-06831999000300024 |
dc.language.iso.fl_str_mv |
eng |
language |
eng |
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 |
Sociedade Brasileira de Ciência do Solo |
publisher.none.fl_str_mv |
Sociedade Brasileira de Ciência do Solo |
dc.source.none.fl_str_mv |
reponame:Repositório Institucional da UnB instname:Universidade de Brasília (UnB) instacron:UNB |
instname_str |
Universidade de Brasília (UnB) |
instacron_str |
UNB |
institution |
UNB |
reponame_str |
Repositório Institucional da UnB |
collection |
Repositório Institucional da UnB |
repository.name.fl_str_mv |
Repositório Institucional da UnB - Universidade de Brasília (UnB) |
repository.mail.fl_str_mv |
repositorio@unb.br |
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1814508178352635904 |