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Registro Completo |
Biblioteca(s): |
Embrapa Amazônia Oriental. |
Data corrente: |
17/08/2006 |
Data da última atualização: |
29/11/2022 |
Tipo da produção científica: |
Artigo em Periódico Indexado |
Autoria: |
SOMMER, R.; SÁ, T. D. de A.; VIELHAUER, K.; ARAÚJO, A. C. de; FÖLSTER, H.; VLEK, P. L. G. |
Afiliação: |
ROLF SOMMER, University of Bonn; TATIANA DEANE DE ABREU SA, CPATU; KONRAD VIELHAUER, University of Bonn; ALESSANDRO CARIOCA DE ARAÚJO, INPA; HORST FÖLSTER, University of Göttingen; University of Bonn. |
Título: |
Transpiration and canopy conductance of secondary vegetation in the eastern Amazon. |
Ano de publicação: |
2002 |
Fonte/Imprenta: |
Agricultural and Forest Meteorology, v. 112, n. 2, p. 103-121, Aug. 2002. |
Descrição Física: |
il. |
DOI: |
http://dx.doi.org/10.1016/S0168-1923(02)00044-8 |
Idioma: |
Inglês |
Conteúdo: |
Secondary woody vegetation in the Brazilian Amazon accounts for about 30% of the cleared area in this region, which exceeds 100,000 km2. Despite the relative predominance of secondary vegetation, the hydrological and climatic properties of these areas are not well documented. In an effort to address this, the evapotranspiration (E) of a 3.5-year-old secondary vegetation in the eastern Amazon of Brazil was measured over 1 year. The annual evapotranspiration according to the Bowen ratio energy balance (BREB) amounted to 1421 mm, which is equal to rates quoted for tropical primary forests. The secondary vegetation returned 73% of the annual rainfall (1954 mm) to the atmosphere. Evapotranspiration required 73% of the net-radiation (Rn) energy; this function remained fairly constant over the whole year. In order to estimate evapotranspiration with the Penman?Monteith (PM) method, the canopy conductance (gc) was determined using the BREB results. The monthly mean daily gc varied between 14 and 22 mm s?1 in the rainy season and the transitional period (January?August), and reached a minimum of 7 mm s?1 in the dry season in October. The hourly as well as daily mean canopy conductance were approximated by a multiple linear regression analysis incorporating hourly and daily averages of Rn and vapour pressure deficit, respectively. In addition, the Jarvis-type model, which is based on a set of environmental control functions, was applied to predict hourly gc. The multiple linear regression and the non-linear optimisation (Jarvis-type model) were equally suitable for gc prediction. The optimised environmental control functions were comparable to those predicted elsewhere for Amazonian primary forests. This underlines the similarity of secondary and primary forests with respect to hydrological characteristics as well as energy turnover. MenosSecondary woody vegetation in the Brazilian Amazon accounts for about 30% of the cleared area in this region, which exceeds 100,000 km2. Despite the relative predominance of secondary vegetation, the hydrological and climatic properties of these areas are not well documented. In an effort to address this, the evapotranspiration (E) of a 3.5-year-old secondary vegetation in the eastern Amazon of Brazil was measured over 1 year. The annual evapotranspiration according to the Bowen ratio energy balance (BREB) amounted to 1421 mm, which is equal to rates quoted for tropical primary forests. The secondary vegetation returned 73% of the annual rainfall (1954 mm) to the atmosphere. Evapotranspiration required 73% of the net-radiation (Rn) energy; this function remained fairly constant over the whole year. In order to estimate evapotranspiration with the Penman?Monteith (PM) method, the canopy conductance (gc) was determined using the BREB results. The monthly mean daily gc varied between 14 and 22 mm s?1 in the rainy season and the transitional period (January?August), and reached a minimum of 7 mm s?1 in the dry season in October. The hourly as well as daily mean canopy conductance were approximated by a multiple linear regression analysis incorporating hourly and daily averages of Rn and vapour pressure deficit, respectively. In addition, the Jarvis-type model, which is based on a set of environmental control functions, was applied to predict hourly gc. The multiple linear regres... Mostrar Tudo |
Palavras-Chave: |
Igarapé-Açu; Tipitamba. |
Thesagro: |
Desmatamento; Transpiração Vegetal; Vegetação Secundária. |
Thesaurus Nal: |
Amazonia. |
Categoria do assunto: |
K Ciência Florestal e Produtos de Origem Vegetal |
Marc: |
LEADER 02690naa a2200277 a 4500 001 1407956 005 2022-11-29 008 2002 bl uuuu u00u1 u #d 024 7 $ahttp://dx.doi.org/10.1016/S0168-1923(02)00044-8$2DOI 100 1 $aSOMMER, R. 245 $aTranspiration and canopy conductance of secondary vegetation in the eastern Amazon.$h[electronic resource] 260 $c2002 300 $cil. 520 $aSecondary woody vegetation in the Brazilian Amazon accounts for about 30% of the cleared area in this region, which exceeds 100,000 km2. Despite the relative predominance of secondary vegetation, the hydrological and climatic properties of these areas are not well documented. In an effort to address this, the evapotranspiration (E) of a 3.5-year-old secondary vegetation in the eastern Amazon of Brazil was measured over 1 year. The annual evapotranspiration according to the Bowen ratio energy balance (BREB) amounted to 1421 mm, which is equal to rates quoted for tropical primary forests. The secondary vegetation returned 73% of the annual rainfall (1954 mm) to the atmosphere. Evapotranspiration required 73% of the net-radiation (Rn) energy; this function remained fairly constant over the whole year. In order to estimate evapotranspiration with the Penman?Monteith (PM) method, the canopy conductance (gc) was determined using the BREB results. The monthly mean daily gc varied between 14 and 22 mm s?1 in the rainy season and the transitional period (January?August), and reached a minimum of 7 mm s?1 in the dry season in October. The hourly as well as daily mean canopy conductance were approximated by a multiple linear regression analysis incorporating hourly and daily averages of Rn and vapour pressure deficit, respectively. In addition, the Jarvis-type model, which is based on a set of environmental control functions, was applied to predict hourly gc. The multiple linear regression and the non-linear optimisation (Jarvis-type model) were equally suitable for gc prediction. The optimised environmental control functions were comparable to those predicted elsewhere for Amazonian primary forests. This underlines the similarity of secondary and primary forests with respect to hydrological characteristics as well as energy turnover. 650 $aAmazonia 650 $aDesmatamento 650 $aTranspiração Vegetal 650 $aVegetação Secundária 653 $aIgarapé-Açu 653 $aTipitamba 700 1 $aSÁ, T. D. de A. 700 1 $aVIELHAUER, K. 700 1 $aARAÚJO, A. C. de 700 1 $aFÖLSTER, H. 700 1 $aVLEK, P. L. G. 773 $tAgricultural and Forest Meteorology$gv. 112, n. 2, p. 103-121, Aug. 2002.
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Embrapa Amazônia Oriental (CPATU) |
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Biblioteca(s): |
Embrapa Agrobiologia. |
Data corrente: |
20/03/2015 |
Data da última atualização: |
28/08/2023 |
Tipo da produção científica: |
Artigo em Periódico Indexado |
Circulação/Nível: |
A - 2 |
Autoria: |
MARTINS, M. R.; JANTALIA, C. P.; POLIDORO, J. C.; BATISTA, J. N.; ALVES, B. J. R.; BODDEY, R. M.; URQUIAGA, S. |
Afiliação: |
CLAUDIA POZZI JANTALIA, CNPAB; JOSE CARLOS POLIDORO, CNPS; BOLSISTA DA EMBRAPA AGROBIOLOGIA; BRUNO JOSE RODRIGUES ALVES, CNPAB; ROBERT MICHAEL BODDEY, CNPAB; SEGUNDO SACRAMENTO U CABALLERO, CNPAB. |
Título: |
Nitrous oxide and ammonia emissions from N fertilization of maize crop under no-till in a Cerrado soil. |
Ano de publicação: |
2015 |
Fonte/Imprenta: |
Soil and Tillage Research, v. 151, p. 75-81, Aug. 2015. |
ISSN: |
0167-1987 |
Idioma: |
Inglês |
Palavras-Chave: |
Bioma Cerrado; Greenhouse gas; Maize; N balance; Savannah; Solo fertilizado; Tropical soil. |
Thesagro: |
Efeito Estufa. |
Categoria do assunto: |
-- |
URL: |
https://www.sciencedirect.com/science/article/pii/S0167198715000616
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Marc: |
LEADER 00805naa a2200289 a 4500 001 2011879 005 2023-08-28 008 2015 bl --- 0-- u #d 022 $a0167-1987 100 1 $aMARTINS, M. R. 245 $aNitrous oxide and ammonia emissions from N fertilization of maize crop under no-till in a Cerrado soil. 260 $c2015 650 $aEfeito Estufa 653 $aBioma Cerrado 653 $aGreenhouse gas 653 $aMaize 653 $aN balance 653 $aSavannah 653 $aSolo fertilizado 653 $aTropical soil 700 1 $aJANTALIA, C. P. 700 1 $aPOLIDORO, J. C. 700 1 $aBATISTA, J. N. 700 1 $aALVES, B. J. R. 700 1 $aBODDEY, R. M. 700 1 $aURQUIAGA, S. 773 $tSoil and Tillage Research$gv. 151, p. 75-81, Aug. 2015.
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