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| Registros recuperados : 219 | |
| 43. |  | PINHEIRO JUNIOR, C. R.; PEREIRA, M. G.; FONTANA, A.; PINTO, L. A. da S. R. Carbono das frações húmicas de perfis de solo da XIII RCC. In: SILVA, M. B. e; LUMBRERAS, J. F.; COELHO, M. R.; OLIVEIRA, V. A. de (ed.). Guia de campo da XIII Reunião Brasileira de Classificação e Correlação de Solos: RCC do Maranhão. Brasília, DF: Embrapa, 2020. E-book. cap. 16.| Biblioteca(s): Embrapa Solos. |
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| 46. | | MONTEIRO, J.; HISSA, H.; COELHO, M.; FONTANA, A.; FONSECA, K.; COSTA, M.; GOULART, A. C. Carbon stock measurement to evaluate ecosystem service from carbon sequestration. In: WORLD CONGRESS OF SOIL SCIENCE, 20., 2014, Jeju. Soils embrace life and universe: abstracts. [S.l.]: International Union of Soil Sciences, 2014.| Biblioteca(s): Embrapa Solos. |
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| 48. | | SHINZATO, E.; TEIXEIRA, W. G.; GONCALVES, A. O.; FONTANA, A.; CARDOSO, J. H.; MANSUR, K. Caracterização geoquímica do sambaqui da Fazenda Campos Novos - Cabo Frio (RJ). In: CONGRESSO BRASILEIRO DE GEOLOGIA, 48., 2016, Porto Alegre. As geotecnologias e o século XXI: anais... São Paulo: Sociedade Brasileira de Geologia, 2016.| Biblioteca(s): Embrapa Solos. |
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| 55. | | CAPOANE, V.; MESCOLOTTI, P. C.; FUSHIMI, M.; FONTANA, A.; KUPLICH, T. M.; SILVA, D. A. da. Detecção de focos de arenização na bacia hidrográfica do Córrego Guariroba, Campo Grande, Mato Grosso do Sul. Revista Brasileira de Geomorfologia, v. 25, n. 2, e2478, 2024. Título em inglês: Detection of arenization foci in the Guariroba river watershed, Campo Grande, Mato Grosso do Sul.| Biblioteca(s): Embrapa Solos. |
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| 56. | | TEIXEIRA, P. C.; CALDERANO, S. B.; CAMPOS, D. V. B. de; FONTANA, A. Ferro, alumínio, manganês e sílica extraíveis. In: TEIXEIRA, P. C.; DONAGEMMA, G. K.; FONTANA, A.; TEIXEIRA, W. G. (Ed.). Manual de métodos de análise de solo. 3. ed. rev. e ampl. Brasília, DF: Embrapa, 2017. pt. 2, cap. 19, p. 289-298.| Biblioteca(s): Embrapa Solos. |
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| 58. | | FONTANA, A.; PEREIRA, M. G.; SALTON, J. C.; LOSS, A.; CUNHA, T. J. F. Fósforo remanescente e correlação com as substâncias húmicas em um latossolo vermelho sob diferentes sucessões de cultura em plantio direto. Revista Brasileira de Agrociência, Pelotas, v. 14, n. 1, p. 161-166, 2008.| Biblioteca(s): Embrapa Semiárido. |
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| 60. | | VIANA, J. H. M.; DONAGEMMA, G. K.; FONTANA, A.; OLIVEIRA, A. P.; ANDRADE, H. M. Fracionamento da areia na distinção de solos arenosos de Luis Eduardo Magalhães-BA. In: SIMPÓSIO BRASILEIRO DE SOLOS ARENOSOS, 1., 2014, Presidente Prudente, SP. [Anais...]. Presidente Prudente, SP: Universidade do Oeste Paulista, 2014.| Biblioteca(s): Embrapa Milho e Sorgo. |
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Registro Completo
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Biblioteca(s): |
Embrapa Solos. |
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Data corrente: |
22/11/2019 |
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Data da última atualização: |
22/11/2019 |
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Tipo da produção científica: |
Resumo em Anais de Congresso |
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Autoria: |
MENEZES, A. R. de; FONTANA, A.; ANJOS, L. H. C. dos; PEREIRA, M. G. |
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Afiliação: |
ANDRESSA ROSAS DE MENEZES, UFRRJ; ADEMIR FONTANA, CNPS; LÚCIA HELENA CUNHA DOS ANJOS, UFRRJ; MARCOS GERVASIO PEREIRA, UFRRJ. |
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Título: |
Stock of organic carbon in spodic horizons of Brazilian Spodosols. |
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Ano de publicação: |
2019 |
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Fonte/Imprenta: |
In: WORLD CONGRESS OF SOIL SCIENCE, 21., 2018, Rio de Janeiro. Soil science: beyond food and fuel: proceedings... Viçosa, MG: SBCS, 2019. v. 2, p. 139-140. WCSS 2018. |
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Idioma: |
Inglês |
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Conteúdo: |
Soils classified as Spodosols in Brazil occur at different landscapes, from coastal plains to high altitude areas. Although they are present in different environments, these soils are formed mainly under humid climates, from sandy parent materials, and usually with shrub and grasses vegetation. They differ from Spodosols from the cold climates and under coniferous forests, from where the concept of podzolization process derived. This order of soils is defined by the Brazilian Soil Classification System (SiBCS) by the presence if a spodic horizon, which must have organic carbon (C org) accumulation in relation to the overlying horizons. To highlight the importance of the preservation of these soils due to their storage of carbon in subsurface, among other reasons related to the flora and fauna they support, the objective of this work was to estimate the organic carbon stock (Ec) of spodic horizons in Brazil. From an extensive bibliographical search, 38 profiles identified as Spodosols according to the SiBCS were selected, and the C org in g kg-1, bulk density (Ds) in Mg m-3 and thickness (E) in cm of the spodic sub-horizons data was organized in a spread sheet for evaluation of descriptive statistics |
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Palavras-Chave: |
Espodossolo; Estoque de carbono no solo; SiBCS. |
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Thesagro: |
Carbono. |
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Thesaurus NAL: |
Spodosols. |
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Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
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URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/205286/1/Stock-of-organic-carbon-in-spodic-horizons-of-Brazilian-Spodosols-2019.pdf
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Marc: |
LEADER 01925nam a2200205 a 4500
001 2114955
005 2019-11-22
008 2019 bl uuuu u00u1 u #d
100 1 $aMENEZES, A. R. de
245 $aStock of organic carbon in spodic horizons of Brazilian Spodosols.$h[electronic resource]
260 $aIn: WORLD CONGRESS OF SOIL SCIENCE, 21., 2018, Rio de Janeiro. Soil science: beyond food and fuel: proceedings... Viçosa, MG: SBCS, 2019. v. 2, p. 139-140. WCSS 2018.$c2018
520 $aSoils classified as Spodosols in Brazil occur at different landscapes, from coastal plains to high altitude areas. Although they are present in different environments, these soils are formed mainly under humid climates, from sandy parent materials, and usually with shrub and grasses vegetation. They differ from Spodosols from the cold climates and under coniferous forests, from where the concept of podzolization process derived. This order of soils is defined by the Brazilian Soil Classification System (SiBCS) by the presence if a spodic horizon, which must have organic carbon (C org) accumulation in relation to the overlying horizons. To highlight the importance of the preservation of these soils due to their storage of carbon in subsurface, among other reasons related to the flora and fauna they support, the objective of this work was to estimate the organic carbon stock (Ec) of spodic horizons in Brazil. From an extensive bibliographical search, 38 profiles identified as Spodosols according to the SiBCS were selected, and the C org in g kg-1, bulk density (Ds) in Mg m-3 and thickness (E) in cm of the spodic sub-horizons data was organized in a spread sheet for evaluation of descriptive statistics
650 $aSpodosols
650 $aCarbono
653 $aEspodossolo
653 $aEstoque de carbono no solo
653 $aSiBCS
700 1 $aFONTANA, A.
700 1 $aANJOS, L. H. C. dos
700 1 $aPEREIRA, M. G.
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