The hydrogeologic potential conditioning factors of hydrographic catchments of Upper Velhas River Basin, Southeastern Brazil.

Detalhes bibliográficos
Autor(a) principal: Costa, Fernanda Martineli
Data de Publicação: 2010
Outros Autores: Bacellar, Luis de Almeida Prado
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Repositório Institucional da UFOP
Texto Completo: http://www.repositorio.ufop.br/handle/123456789/8243
Resumo: The hydrogeologic potential of a drainage catchment represents its capacity of sustainable water production, with good maintenance of the baseflows. In basins of similar shapes and bio-climatic characteristics, the potential will depend on several physical and anthropogenic conditioning factors. The determination of the hydrogeologic potential is a complex procedure, but alternative methods exist, in which hydrologic series are used to determine certain indexes, such as the recession coefficient (a), the specific baseflow (SBF), the baseflow index (BFI), transmissivity and storativity. Aiming at the evaluation of the hydrogeologic potential and its conditioning factors in the Maracuja´ River Basin (southeastern Brazil), ten catchments were selected and monitored. The catchments have distinct geologic and geomorphologic characteristics but are submitted to similar climatic conditions. The hydrogeologic potential is higher in crystalline basement areas, especially where the relief is flat and the regolith is thick; however, it is lower in the areas affected by gullies. The advantages of the hydrologic method, in particular to regions where information is scarce, are that it is easily applied and of low cost, enabling the characterization of the hydrogeologic potential and contributing to the management of water resources.
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spelling Costa, Fernanda MartineliBacellar, Luis de Almeida Prado2017-07-14T16:00:33Z2017-07-14T16:00:33Z2010COSTA, F. M.; BACELLAR, L. de A. P. The hydrogeologic potential conditioning factors of hydrographic catchments of Upper Velhas River Basin, Southeastern Brazil. Revista Brasileira de Recursos Hídricos, v. 15, p. 38-54, 2010. Disponível em: <http://www.abrh.org.br/SGCv3/index.php?PUB=1&ID=5&SUMARIO=71>. Acesso em: 20 de jun. 2017. 2318-0331http://www.repositorio.ufop.br/handle/123456789/8243The hydrogeologic potential of a drainage catchment represents its capacity of sustainable water production, with good maintenance of the baseflows. In basins of similar shapes and bio-climatic characteristics, the potential will depend on several physical and anthropogenic conditioning factors. The determination of the hydrogeologic potential is a complex procedure, but alternative methods exist, in which hydrologic series are used to determine certain indexes, such as the recession coefficient (a), the specific baseflow (SBF), the baseflow index (BFI), transmissivity and storativity. Aiming at the evaluation of the hydrogeologic potential and its conditioning factors in the Maracuja´ River Basin (southeastern Brazil), ten catchments were selected and monitored. The catchments have distinct geologic and geomorphologic characteristics but are submitted to similar climatic conditions. The hydrogeologic potential is higher in crystalline basement areas, especially where the relief is flat and the regolith is thick; however, it is lower in the areas affected by gullies. The advantages of the hydrologic method, in particular to regions where information is scarce, are that it is easily applied and of low cost, enabling the characterization of the hydrogeologic potential and contributing to the management of water resources.Os trabalhos publicados no Brazilian Journal of Water Resources estão sob Licença Creative Commons que permite copiar, distribuir e transmitir o trabalho desde que sejam citados o autor e o licenciante. Fonte: Brazilian Journal of Water Resources <http://www.scielo.br/scielo.php?script=sci_serial&pid=2318-0331&lng=en&nrm=iso>. Acesso em: 13 jan. 2020.info:eu-repo/semantics/openAccessHydrogeologic potentialCatchmentsBaseflowRecession coefficientThe hydrogeologic potential conditioning factors of hydrographic catchments of Upper Velhas River Basin, Southeastern Brazil.info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articleengreponame:Repositório Institucional da UFOPinstname:Universidade Federal de Ouro Preto (UFOP)instacron:UFOPLICENSElicense.txtlicense.txttext/plain; charset=utf-8924http://www.repositorio.ufop.br/bitstream/123456789/8243/2/license.txt62604f8d955274beb56c80ce1ee5dcaeMD52ORIGINALARTIGO_HydrogeologicPotentialConditioning.pdfARTIGO_HydrogeologicPotentialConditioning.pdfapplication/pdf544152http://www.repositorio.ufop.br/bitstream/123456789/8243/1/ARTIGO_HydrogeologicPotentialConditioning.pdf86da4e1bf854d7b0dc7a082661e25f7aMD51123456789/82432020-01-13 07:52:59.295oai:localhost: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ório InstitucionalPUBhttp://www.repositorio.ufop.br/oai/requestrepositorio@ufop.edu.bropendoar:32332020-01-13T12:52:59Repositório Institucional da UFOP - Universidade Federal de Ouro Preto (UFOP)false
dc.title.pt_BR.fl_str_mv The hydrogeologic potential conditioning factors of hydrographic catchments of Upper Velhas River Basin, Southeastern Brazil.
title The hydrogeologic potential conditioning factors of hydrographic catchments of Upper Velhas River Basin, Southeastern Brazil.
spellingShingle The hydrogeologic potential conditioning factors of hydrographic catchments of Upper Velhas River Basin, Southeastern Brazil.
Costa, Fernanda Martineli
Hydrogeologic potential
Catchments
Baseflow
Recession coefficient
title_short The hydrogeologic potential conditioning factors of hydrographic catchments of Upper Velhas River Basin, Southeastern Brazil.
title_full The hydrogeologic potential conditioning factors of hydrographic catchments of Upper Velhas River Basin, Southeastern Brazil.
title_fullStr The hydrogeologic potential conditioning factors of hydrographic catchments of Upper Velhas River Basin, Southeastern Brazil.
title_full_unstemmed The hydrogeologic potential conditioning factors of hydrographic catchments of Upper Velhas River Basin, Southeastern Brazil.
title_sort The hydrogeologic potential conditioning factors of hydrographic catchments of Upper Velhas River Basin, Southeastern Brazil.
author Costa, Fernanda Martineli
author_facet Costa, Fernanda Martineli
Bacellar, Luis de Almeida Prado
author_role author
author2 Bacellar, Luis de Almeida Prado
author2_role author
dc.contributor.author.fl_str_mv Costa, Fernanda Martineli
Bacellar, Luis de Almeida Prado
dc.subject.por.fl_str_mv Hydrogeologic potential
Catchments
Baseflow
Recession coefficient
topic Hydrogeologic potential
Catchments
Baseflow
Recession coefficient
description The hydrogeologic potential of a drainage catchment represents its capacity of sustainable water production, with good maintenance of the baseflows. In basins of similar shapes and bio-climatic characteristics, the potential will depend on several physical and anthropogenic conditioning factors. The determination of the hydrogeologic potential is a complex procedure, but alternative methods exist, in which hydrologic series are used to determine certain indexes, such as the recession coefficient (a), the specific baseflow (SBF), the baseflow index (BFI), transmissivity and storativity. Aiming at the evaluation of the hydrogeologic potential and its conditioning factors in the Maracuja´ River Basin (southeastern Brazil), ten catchments were selected and monitored. The catchments have distinct geologic and geomorphologic characteristics but are submitted to similar climatic conditions. The hydrogeologic potential is higher in crystalline basement areas, especially where the relief is flat and the regolith is thick; however, it is lower in the areas affected by gullies. The advantages of the hydrologic method, in particular to regions where information is scarce, are that it is easily applied and of low cost, enabling the characterization of the hydrogeologic potential and contributing to the management of water resources.
publishDate 2010
dc.date.issued.fl_str_mv 2010
dc.date.accessioned.fl_str_mv 2017-07-14T16:00:33Z
dc.date.available.fl_str_mv 2017-07-14T16:00:33Z
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dc.identifier.citation.fl_str_mv COSTA, F. M.; BACELLAR, L. de A. P. The hydrogeologic potential conditioning factors of hydrographic catchments of Upper Velhas River Basin, Southeastern Brazil. Revista Brasileira de Recursos Hídricos, v. 15, p. 38-54, 2010. Disponível em: <http://www.abrh.org.br/SGCv3/index.php?PUB=1&ID=5&SUMARIO=71>. Acesso em: 20 de jun. 2017.
dc.identifier.uri.fl_str_mv http://www.repositorio.ufop.br/handle/123456789/8243
dc.identifier.issn.none.fl_str_mv  2318-0331
identifier_str_mv COSTA, F. M.; BACELLAR, L. de A. P. The hydrogeologic potential conditioning factors of hydrographic catchments of Upper Velhas River Basin, Southeastern Brazil. Revista Brasileira de Recursos Hídricos, v. 15, p. 38-54, 2010. Disponível em: <http://www.abrh.org.br/SGCv3/index.php?PUB=1&ID=5&SUMARIO=71>. Acesso em: 20 de jun. 2017.
 2318-0331
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