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6. | | ABREU JUNIOR, C. H.; MACHADO, R. C. R.; NG, E. Efeito da adubação N-P-K sobre produtividade de plantas velhas de cacau e fertilidade do solo, em área tradicional de cultivo no sul da Bahia. IN: CONGRESSO BRASILEIRO DE CIÊNÇIA DO SOLO, 25., 1995, Viçosa, MG. Resumos expandidos. Viçosa: UFV, 1995. v.2, p. 600-602. Biblioteca(s): Embrapa Tabuleiros Costeiros. |
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7. | | SOUZA, H. M. F.; MACHADO, R. C. R.; MORENO, M. A.; ALVIM, P. de T. Avaliacao da resistencia a seca, em gramineas forrageiras, mediante determinacao do "ponto de compensacao hidrica". Revista Theobroma, Ilheus, v.12, n.3, p.141-147, jul./set. 1982. Biblioteca(s): Embrapa Tabuleiros Costeiros. |
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9. | | SANTANA, S. O. de; MACHADO, R. C. R.; ABREU JUNIOR, C. H. Estudo pedológico semidetalhado considerando-se as caracteristicas hidricas dos solos de almirante - centro de estudos de cacau, Lomanto Junior, Bahia, Brasil. IN: CONGRESSO BRASILEIRO DE CIÊNÇIA DO SOLO, 25., 1995, Viçosa, MG. Resumos expandidos. Viçosa: UFV, 1995. v.3, p. 1545-1547. Biblioteca(s): Embrapa Semiárido; Embrapa Tabuleiros Costeiros. |
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19. | | GAMA-RODRIGUES, E. F. da; MOÇO, M. K. da S.; GAMA-RODRIGUES, A. C. da; MACHADO, R. C. R. Atributos biológicos em solos sob sistemas agroflorestais de Cacau: um estudo de caso. In: CONGRESSO BRASILEIRO DE SISTEMAS AGROFLORESTAIS, 6., 2006, Campos dos Goytacazes, RJ. Sistemas agroflorestais: bases científicas para o desenvolvimento sustentável: resumos. Campos dos Goytacazes: Universidade Estadual do Norte Fluminense Darcy Ribeiro; Salvador: Sociedade Brasileira de Sistemas Agroflorestais, 2006. p. 243-255. Editado por: GAMA-RODRIGUES, A. C. da; BARROS, N. F. de; GAMA-RODRIGUES, E. F. da; FREITAS, M. S. M.; VIANA, A. P.; JASMIN, J. M.; MARCIANO, C. R.; CARNEIRO, J. G. A. Biblioteca(s): Embrapa Florestas. |
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Registro Completo
Biblioteca(s): |
Embrapa Solos. |
Data corrente: |
10/01/2011 |
Data da última atualização: |
03/11/2021 |
Tipo da produção científica: |
Artigo em Periódico Indexado |
Circulação/Nível: |
A - 2 |
Autoria: |
BARRETO, P. A. B.; GAMA-RODRIGUES, E. F.; GAMA-RODRIGUES, A. C.; FONTES, A. G.; POLIDORO, J. C.; MOÇO, M. K. S.; MACHADO, R. C. R.; BALIGAR, V. C. |
Afiliação: |
Universidade Estadual do Sudoeste da Bahia; Universidade Estadual do Norte Fluminense; Universidade Estadual do Sudoeste da Bahia; Instituto Federal de Educação, Ciência e Tecnologia do Espírito Santo; JOSE CARLOS POLIDORO, CNPS; Universidade Estadual do Sudoeste da Bahia; MARS, Center of Cocoa Science; USDA. |
Título: |
Distribution of oxidizable organic C fractions in soils under cacao agroforestry systems in Southern Bahia, Brazil. |
Ano de publicação: |
2011 |
Fonte/Imprenta: |
Agroforestry Systems, v. 81, n. 3, p. 213-220, Mar. 2011. |
DOI: |
https://doi.org/10.1007/s10457-010-9300-4 |
Idioma: |
Inglês |
Conteúdo: |
Agroforestry systems can play a major role in the sequestration of carbon (C) because of their higher input of organic material to the soil. The importance of organic carbon to the physical, chemical, and biological aspects of soil quality is well recognized. However, total organic carbon measurements might not be sensitive indicators of changes in soil quality. Adoption of procedures that can extract the more labile fraction preferentially might be a more useful approach for the characterization of soil organic carbon resulting from different soils. This study aimed to evaluate organic carbon (C) fractions distribution in different soil layers up to 50 cm depth in two soil orders under cacao (Theobromacacao) agroforestry systems (AFS) in Bahia, Brazil. Soil samples were collected from four depth classes (0-5, 5-10, 10-30 and 30-50 cm) under two cacao agroforestry systems (30-year-old stands of cacao with Erythrina glauca, as shade trees) in Latosol and Cambisol, in Bahia, Brazil. The determination of oxidizable carbon by a modified Walkley-Black method was done to obtain four C fractions with different labile forms of C (fraction 1: labile fraction; fraction 2: moderate labile fraction; fraction 3: low labile fraction and fraction 4: recalcitrant fraction). Overall, at two cacao AFS, the C fractions generally declined with increase in soil depth. The C fractions 1 and 2 were 50% higher on upper layers (0-5 and 5-10 cm). More than 50% of organic C was found in more labile fraction (fraction 1) in all depths for both soils. High value of C fraction 1 (more labile C)-to-total organic C ratio was obtained (around 54-59%, on Latosol and Cambisol, respectively), indicating large input of organic matter in these soils. MenosAgroforestry systems can play a major role in the sequestration of carbon (C) because of their higher input of organic material to the soil. The importance of organic carbon to the physical, chemical, and biological aspects of soil quality is well recognized. However, total organic carbon measurements might not be sensitive indicators of changes in soil quality. Adoption of procedures that can extract the more labile fraction preferentially might be a more useful approach for the characterization of soil organic carbon resulting from different soils. This study aimed to evaluate organic carbon (C) fractions distribution in different soil layers up to 50 cm depth in two soil orders under cacao (Theobromacacao) agroforestry systems (AFS) in Bahia, Brazil. Soil samples were collected from four depth classes (0-5, 5-10, 10-30 and 30-50 cm) under two cacao agroforestry systems (30-year-old stands of cacao with Erythrina glauca, as shade trees) in Latosol and Cambisol, in Bahia, Brazil. The determination of oxidizable carbon by a modified Walkley-Black method was done to obtain four C fractions with different labile forms of C (fraction 1: labile fraction; fraction 2: moderate labile fraction; fraction 3: low labile fraction and fraction 4: recalcitrant fraction). Overall, at two cacao AFS, the C fractions generally declined with increase in soil depth. The C fractions 1 and 2 were 50% higher on upper layers (0-5 and 5-10 cm). More than 50% of organic C was found in more labile fr... Mostrar Tudo |
Palavras-Chave: |
Carbono lábil; Qualidade do carbono; Sequestro de carbono. |
Thesagro: |
Cacau; Erythrina Glauca. |
Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
Marc: |
LEADER 02623naa a2200277 a 4500 001 1872428 005 2021-11-03 008 2011 bl uuuu u00u1 u #d 024 7 $ahttps://doi.org/10.1007/s10457-010-9300-4$2DOI 100 1 $aBARRETO, P. A. B. 245 $aDistribution of oxidizable organic C fractions in soils under cacao agroforestry systems in Southern Bahia, Brazil.$h[electronic resource] 260 $c2011 520 $aAgroforestry systems can play a major role in the sequestration of carbon (C) because of their higher input of organic material to the soil. The importance of organic carbon to the physical, chemical, and biological aspects of soil quality is well recognized. However, total organic carbon measurements might not be sensitive indicators of changes in soil quality. Adoption of procedures that can extract the more labile fraction preferentially might be a more useful approach for the characterization of soil organic carbon resulting from different soils. This study aimed to evaluate organic carbon (C) fractions distribution in different soil layers up to 50 cm depth in two soil orders under cacao (Theobromacacao) agroforestry systems (AFS) in Bahia, Brazil. Soil samples were collected from four depth classes (0-5, 5-10, 10-30 and 30-50 cm) under two cacao agroforestry systems (30-year-old stands of cacao with Erythrina glauca, as shade trees) in Latosol and Cambisol, in Bahia, Brazil. The determination of oxidizable carbon by a modified Walkley-Black method was done to obtain four C fractions with different labile forms of C (fraction 1: labile fraction; fraction 2: moderate labile fraction; fraction 3: low labile fraction and fraction 4: recalcitrant fraction). Overall, at two cacao AFS, the C fractions generally declined with increase in soil depth. The C fractions 1 and 2 were 50% higher on upper layers (0-5 and 5-10 cm). More than 50% of organic C was found in more labile fraction (fraction 1) in all depths for both soils. High value of C fraction 1 (more labile C)-to-total organic C ratio was obtained (around 54-59%, on Latosol and Cambisol, respectively), indicating large input of organic matter in these soils. 650 $aCacau 650 $aErythrina Glauca 653 $aCarbono lábil 653 $aQualidade do carbono 653 $aSequestro de carbono 700 1 $aGAMA-RODRIGUES, E. F. 700 1 $aGAMA-RODRIGUES, A. C. 700 1 $aFONTES, A. G. 700 1 $aPOLIDORO, J. C. 700 1 $aMOÇO, M. K. S. 700 1 $aMACHADO, R. C. R. 700 1 $aBALIGAR, V. C. 773 $tAgroforestry Systems$gv. 81, n. 3, p. 213-220, Mar. 2011.
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