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| 124. | | BARBOSA-OLIVEIRA, C.; PARRON, L. M.; FREITAS, J. S.; RODRIGUES, M. S. Variação sazonal de comunidades zooplanctônicas em sub-bacias da bacia hidrográfica do Rio Preto, Médio São Francisco. In: ENCONTRO DE JOVENS TALENTOS DA EMBRAPA CERRADOS, 3., 2007, Planaltina, DF. Resumos apresentados. Planaltina, DF: Embrapa Cerrados, 2007. p. 29. (Embrapa Cerrados. Documentos, 176).| Biblioteca(s): Embrapa Cerrados. |
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| 125. | | CAMPANHA, M. M.; PRADO, R. B.; PARRON, L. M.; SILVA, M. S. L. da; MATTHIENSEN, A. Visão geral das contribuições da Embrapa. In: SILVA, M. S. L. da; MATTHIENSEN, A.; BRITO, L. T. de L.; LIMA, J. E. F. W.; CARVALHO, C. J. R. de (Ed.). Água e saneamento: contribuições da Embrapa. Brasília, DF: Embrapa, 2018. cap. 2. E-book. (Objetivos de Desenvolvimento Sustentável, 6).| Biblioteca(s): Embrapa Florestas; Embrapa Milho e Sorgo; Embrapa Solos; Embrapa Suínos e Aves. |
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| 126. | | AGUIAR JUNIOR, T. R. de; BORTOLOZO, F. R.; PARRON, L. M. Zonas-tampão ripárias no planejamento e gestão de ecossistemas fluviais em paisagens agrícolas. In: EVENTO DE INICIAÇÃO CIENTÍFICA DA EMBRAPA FLORESTAS, 12., 2013, Colombo. Anais. Colombo: Embrapa Florestas, 2013. (Embrapa Florestas. Documentos, 253). Editores técnicos: Marcílio José Thomazini, Elenice Fritzsons, Patrícia Raquel Silva, Guilherme Schnell e Schuhli, Denise Jeton Cardoso, Luziane Franciscon. EVINCI. Resumos.| Biblioteca(s): Embrapa Florestas. |
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| 127. | | OLIVEIRA, C. B.; POMPÊO, M. L. M.; FREITAS, J. S. de; PARRON, L. M. Zooplâncton em córregos sob diferentes impactos na bacia do Rio Preto, Brasil. In: SIMPÓSIO NACIONAL CERRADO, 9.; SIMPÓSIO INTERNACIONAL SAVANAS TROPICAIS, 2., 2008, Brasília, DF. Desafios e estratégias para o equilíbrio entre sociedade, agronegócio e recursos naturais: anais... Planaltina, DF: Embrapa Cerrados, 2008. 1 CD-ROM.| Biblioteca(s): Embrapa Cerrados. |
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| 128. | | MARKEWITZ, D.; FIGUEIREDO, R. de O.; DAVIDSON, E. A.; BUSTAMANTE, M. M. C.; PARRON, L.; RESENDE, J. The chemistry of two streams draining kaolinitic soils. In: CONFERÊNCIA CIENTÍFICA DO LBA, 3., 2004, Brasília, DF. Anais de trabalhos completos. Brasília, DF: LBA, 2004. Plenária 6. Resumo 20.5.| Biblioteca(s): Embrapa Amazônia Oriental. |
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| 130. | | SILVA, M. P. da; PARRON, L. M.; MAZZA, C. A. da S.; POTT, A.; MAURO, R. de A. Composicao botanica da dieta de bubalinos no Pantanal Mato-Grossense da Nhecolandia, MS. In: REUNIAO ANUAL DA SOCIEDADE BRASILEIRA DE ZOOTECNIA, 26., 1989, Porto Alegre. Anais... Porto Alegre: SBZ, 1989. p.90.| Biblioteca(s): Embrapa Pantanal. |
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| 133. | | PARRON, L. M.; FAVARETTO, N.; PORFIRIO-DA-SILVA, V.; RODRIGUES, L. N.; FRITZSONS, E.; GOMES, J. B. V. Avaliação de indicadores associados à conservação dos recursos hídricos em distintos sistemas de uso da terra para valoração de serviços ambientais. In: SEMINÁRIO DA REDE AGROHIDRO, 1., 2012, Rio de Janeiro. Água: desafios para a sustentabilidade da agricultura: anais. Rio de Janeiro: Embrapa Solos, 2014. 83 p. (Embrapa Solos. Documentos, 167). p. 22-24.| Biblioteca(s): Embrapa Cerrados. |
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| 134. | | PARRON, L. M.; FAVARETTO, N.; PORFIRIO-DA-SILVA, V.; RODRIGUES, L. N.; FRITZSONS, E.; GOMES, J. B. V. Avaliação de indicadores associados à conservação dos recursos hídricos em distintos sistemas de uso da terra para valoração de serviços ambientais. In: SEMINÁRIO DA REDE AGROHIDRO, 1., 2012, Rio de Janeiro. Água: desafios para a sustentabilidade da agricultura: anais. Rio de Janeiro: Embrapa Solos, 2014. 83 p. (Embrapa Solos. Documentos, 167). p. 22-24.| Biblioteca(s): Embrapa Florestas. |
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| 135. | | MARKEWITZ, D.; RESENDE, J. C. F.; PARRON, L.; BUSTAMANTE, M.; KLINK, C. A.; FIGUEIREDO, R. de O.; DAVIDSON, E. A. Dissolved rainfall inputs and streamwater outputs in an undisturbed watershed on highly weathered soils in the brazilian cerrado. Hydrological Processes, v. 20, n. 12, p. 2615-2639, Aug. 2006.| Biblioteca(s): Embrapa Amazônia Oriental. |
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| 137. | | COSER, T. R.; PARRON, L. M.; MADALENA, J. O.; DUBOC, E.; LARANJEIRA, N.; DALLACORTE, J. L.; CAMARGOS, J. M. R. Escolas rurais e gestão de recursos hídricos: a experiência da Embrapa Cerrados. In: ENCONTRO DE JOVENS TALENTOS DA EMBRAPA CERRADOS, 3., 2007, Planaltina, DF. Resumos apresentados. Planaltina, DF: Embrapa Cerrados, 2007. p. 52. (Embrapa Cerrados. Documentos, 176).| Biblioteca(s): Embrapa Cerrados. |
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| 138. | | PEIXOTO, R. T. dos G.; MAIA, C. M. B. de F.; SANTOS, L. M. dos; PARRON, L. M. Dendrometric aspects of the biochar application in Eucalyptus urograndis. Pesquisa Florestal Brasileira, Colombo, v. 39, (nesp), e201902043, 2019. p. 658. Edição especial dos resumos do IUFRO World Congress, 25., 2019, Curitiba.| Biblioteca(s): Embrapa Florestas. |
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| 139. | | PEIXOTO, R. T. dos G.; MAIA, C. M. B. de F.; SANTOS, L. M. dos; PARRON, L. M. Dendrometric aspects of the biochar application in Eucalyptus urograndis. Pesquisa Florestal Brasileira, v. 39, e201902043, p. 658, 2019. Special issue. Abstracts of the XXV IUFRO World Congress, Curitiba, Sept./Oct. 2019.| Biblioteca(s): Embrapa Solos. |
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| 140. | | SCHLEDER, A. A.; PARRON, L. M.; HANSEL, F. A.; FROEHNER, S.; PALAGANO, L. T.; ROSA FILHO, E. F. da. Evaluation of occurrence of NO3-, coliform and atrazine in a karst aquifer, Colombo, PR. Revista Brasileira de Recursos Hídricos, Porto Alegre, v. 22, e20, 2017.| Biblioteca(s): Embrapa Florestas. |
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| Registros recuperados : 185 | |
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 | Acesso ao texto completo restrito à biblioteca da Embrapa Amazônia Oriental. Para informações adicionais entre em contato com cpatu.biblioteca@embrapa.br. |
Registro Completo
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Biblioteca(s): |
Embrapa Amazônia Oriental. |
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Data corrente: |
18/12/2009 |
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Data da última atualização: |
08/06/2022 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
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Circulação/Nível: |
Internacional - A |
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Autoria: |
MARKEWITZ, D.; RESENDE, J. C. F.; PARRON, L.; BUSTAMANTE, M.; KLINK, C. A.; FIGUEIREDO, R. de O.; DAVIDSON, E. A. |
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Afiliação: |
DANIEL MARKEWITZ, The University of Georgia; JULIO C. F. RESENDE, UNB; LUCILIA PARRON, UNB; MERCEDES BUSTAMANTE, UNB; CARLOS A. KLINK, UNB; RICARDO DE OLIVEIRA FIGUEIREDO, CPATU; ERIC A. DAVIDSON, The Woods Hole Research Center. |
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Título: |
Dissolved rainfall inputs and streamwater outputs in an undisturbed watershed on highly weathered soils in the brazilian cerrado. |
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Ano de publicação: |
2006 |
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Fonte/Imprenta: |
Hydrological Processes, v. 20, n. 12, p. 2615-2639, Aug. 2006. |
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DOI: |
10.1002/hyp.6219 |
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Idioma: |
Inglês |
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Conteúdo: |
The cerrados of Brazil cover 2 million km2. Despite the extent of these seasonally dry ecosystems, little watershed research has been focused in this region, particularly relative to the watersheds of the Amazon Basin. The cerrado shares pedogenic characteristics with the Amazon Basin in draining portions of the Brazilian shield and in possessing Oxisols over much of the landscape. The objective of this research was to quantify the stream water geochemical relationships of an undisturbed 1200 ha cerrado watershed for comparison to river geochemistry in the Amazon. Furthermore, this undisturbed watershed was used to evaluate stream discharge versus dissolved ion concentration relationships. This research was conducted in the Córrego Roncador watershed of the Reserva Ecológica do Roncador (RECOR) of the Instituto Brasileiro Geografia e Estatística (IBGE) near Brasilia, Brazil. Bulk precipitation and stream water chemistry were analysed between May 1998 and May 2000. The upland soils of this watershed are nutrient poor possessing total stocks of exchangeable elements in the upper 1 m of 81 ± 13, 77 ± 4, 25 ± 3, and 1 ± 1 kg ha?1 of K, Ca, Mg, and P, respectively. Bulk precipitation inputs of dissolved nutrients for this watershed are low and consistent with previous estimates. The nutrient-poor soils of this watershed, however, increase the relative importance of precipitation for nutrient replenishment to vegetation during episodes of ecosystem disturbance. Stream water dissolved loads were extremely dilute with conductivities ranging from 4 to 10 µS cm?1 during periods of high- and low-flow, respectively. Despite the low concentrations in this stream, geochemical relationships were similar to other Amazonian streams draining shield geologies. Discharge-concentration relationships for Ca and Mg in these highly weathered soils developed from igneous rocks of the Brazilian shield demonstrated a significant negative relationship indicating a continued predominance of groundwater baseflow contributions these cationic elements. Copyright © 2006 John Wiley & Sons, Ltd. MenosThe cerrados of Brazil cover 2 million km2. Despite the extent of these seasonally dry ecosystems, little watershed research has been focused in this region, particularly relative to the watersheds of the Amazon Basin. The cerrado shares pedogenic characteristics with the Amazon Basin in draining portions of the Brazilian shield and in possessing Oxisols over much of the landscape. The objective of this research was to quantify the stream water geochemical relationships of an undisturbed 1200 ha cerrado watershed for comparison to river geochemistry in the Amazon. Furthermore, this undisturbed watershed was used to evaluate stream discharge versus dissolved ion concentration relationships. This research was conducted in the Córrego Roncador watershed of the Reserva Ecológica do Roncador (RECOR) of the Instituto Brasileiro Geografia e Estatística (IBGE) near Brasilia, Brazil. Bulk precipitation and stream water chemistry were analysed between May 1998 and May 2000. The upland soils of this watershed are nutrient poor possessing total stocks of exchangeable elements in the upper 1 m of 81 ± 13, 77 ± 4, 25 ± 3, and 1 ± 1 kg ha?1 of K, Ca, Mg, and P, respectively. Bulk precipitation inputs of dissolved nutrients for this watershed are low and consistent with previous estimates. The nutrient-poor soils of this watershed, however, increase the relative importance of precipitation for nutrient replenishment to vegetation during episodes of ecosystem disturbance. Stream water dissol... Mostrar Tudo |
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Palavras-Chave: |
Watershed. |
|
Thesaurus NAL: |
geochemistry; nutrient balance. |
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Categoria do assunto: |
-- |
|
Marc: |
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001 1578388
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008 2006 bl uuuu u00u1 u #d
024 7 $a10.1002/hyp.6219$2DOI
100 1 $aMARKEWITZ, D.
245 $aDissolved rainfall inputs and streamwater outputs in an undisturbed watershed on highly weathered soils in the brazilian cerrado.$h[electronic resource]
260 $c2006
520 $aThe cerrados of Brazil cover 2 million km2. Despite the extent of these seasonally dry ecosystems, little watershed research has been focused in this region, particularly relative to the watersheds of the Amazon Basin. The cerrado shares pedogenic characteristics with the Amazon Basin in draining portions of the Brazilian shield and in possessing Oxisols over much of the landscape. The objective of this research was to quantify the stream water geochemical relationships of an undisturbed 1200 ha cerrado watershed for comparison to river geochemistry in the Amazon. Furthermore, this undisturbed watershed was used to evaluate stream discharge versus dissolved ion concentration relationships. This research was conducted in the Córrego Roncador watershed of the Reserva Ecológica do Roncador (RECOR) of the Instituto Brasileiro Geografia e Estatística (IBGE) near Brasilia, Brazil. Bulk precipitation and stream water chemistry were analysed between May 1998 and May 2000. The upland soils of this watershed are nutrient poor possessing total stocks of exchangeable elements in the upper 1 m of 81 ± 13, 77 ± 4, 25 ± 3, and 1 ± 1 kg ha?1 of K, Ca, Mg, and P, respectively. Bulk precipitation inputs of dissolved nutrients for this watershed are low and consistent with previous estimates. The nutrient-poor soils of this watershed, however, increase the relative importance of precipitation for nutrient replenishment to vegetation during episodes of ecosystem disturbance. Stream water dissolved loads were extremely dilute with conductivities ranging from 4 to 10 µS cm?1 during periods of high- and low-flow, respectively. Despite the low concentrations in this stream, geochemical relationships were similar to other Amazonian streams draining shield geologies. Discharge-concentration relationships for Ca and Mg in these highly weathered soils developed from igneous rocks of the Brazilian shield demonstrated a significant negative relationship indicating a continued predominance of groundwater baseflow contributions these cationic elements. Copyright © 2006 John Wiley & Sons, Ltd.
650 $ageochemistry
650 $anutrient balance
653 $aWatershed
700 1 $aRESENDE, J. C. F.
700 1 $aPARRON, L.
700 1 $aBUSTAMANTE, M.
700 1 $aKLINK, C. A.
700 1 $aFIGUEIREDO, R. de O.
700 1 $aDAVIDSON, E. A.
773 $tHydrological Processes$gv. 20, n. 12, p. 2615-2639, Aug. 2006.
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