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| 1. |  | RAUEN, V.; GONZAGA, J. V.; MACHADO, J. R. M.; FINGER, C. A. G. Aproveitamento de madeira fina na indústria de celulose. Silvicultura, São Paulo, v. 11, n. 41, p. 172, 1986. Resumo. Edição dos anais do 5º Congresso Florestal Brasileiro, 1986, Olinda. Usos múltiplos da floresta: uma necessidade.| Biblioteca(s): Embrapa Florestas. |
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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
|
Biblioteca(s): |
Embrapa Amazônia Oriental. |
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Data corrente: |
26/06/2013 |
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Data da última atualização: |
07/11/2022 |
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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: |
TELLES, E. de C. C.; CAMARGO, P. B. de; MARTINELLI, L. A.; TRUMBORE, S. E.; COSTA, E. S. da; SANTOS, J.; HIGUCHI, N.; OLIVEIRA JUNIOR, R. C. |
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Afiliação: |
Everaldo de Carvalho Conceição Telles, CENA/USP; Plínio Barbosa de Camargo, CENA/USP; Luiz A. Martinelli, CENA/USP; Susan E. Trumbore, University of California; Enir Salazar da Costa, University of California; JOAQUIM SANTOS, INPA; Niro Higuchi, INPA; RAIMUNDO COSME DE OLIVEIRA JUNIOR, CPATU. |
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Título: |
Influence of soil texture on carbon dynamics and storage potential in tropical forest soils of Amazonia. |
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Ano de publicação: |
2003 |
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Fonte/Imprenta: |
Global Biogeochemical Cycles, v. 17, n. 2, Jun. 2003. |
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DOI: |
10.1029/2002GB001953 |
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Idioma: |
Inglês |
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Conteúdo: |
Stable and radiocarbon isotopes were used to investigate the role of soil clay content in the storage and dynamics of soil carbon in tropical forest soils. Organic matter in clay-rich Oxisols and Ultisols contains at least two distinct components: (1) material with light δ13C signatures and turnover times of decades or less; and (2) clay-associated, 13C-enriched, carbon with turnover times of decades at the surface to millennia at depths >20 cm. Soil texture, in this case clay content, exerts a major control on the amount of slowly cycling carbon and therefore influences the storage and dynamics of carbon in tropical forest soils. Soils in primary tropical forest have been proposed as a potentially large sink for anthropogenic carbon. Comparison of carbon stocks in Oxisols sampled near Manaus, Brazil, shows no measurable change in organic carbon stocks over the past 20 years. Simple models estimating the response of soil carbon pools to a sustained 0.5% yr−1 increase in productivity result in C storage rates of 0.09 to 0.13 MgC ha−1 yr8722;1 in soil organic matter, with additional potential storage of 0.18 to 0.27 MgC ha−1 yr−1 in surface litter and roots. Most storage occurs in organic matter pools with turnover times less than a decade. Export of carbon in dissolved form from upland terra firme Oxisols likely accounts for <0.2 MgC ha8722;1 yr8722;1, but more work is required to assess the export potential for periodically inundated Spodosols. |
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Palavras-Chave: |
Ciclo de carbono. |
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Thesagro: |
Carbono; Decomposição; Solo; Solo Tropical; Textura. |
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Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
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Marc: |
LEADER 02342naa a2200289 a 4500
001 1960656
005 2022-11-07
008 2003 bl uuuu u00u1 u #d
024 7 $a10.1029/2002GB001953$2DOI
100 1 $aTELLES, E. de C. C.
245 $aInfluence of soil texture on carbon dynamics and storage potential in tropical forest soils of Amazonia.$h[electronic resource]
260 $c2003
520 $aStable and radiocarbon isotopes were used to investigate the role of soil clay content in the storage and dynamics of soil carbon in tropical forest soils. Organic matter in clay-rich Oxisols and Ultisols contains at least two distinct components: (1) material with light δ13C signatures and turnover times of decades or less; and (2) clay-associated, 13C-enriched, carbon with turnover times of decades at the surface to millennia at depths >20 cm. Soil texture, in this case clay content, exerts a major control on the amount of slowly cycling carbon and therefore influences the storage and dynamics of carbon in tropical forest soils. Soils in primary tropical forest have been proposed as a potentially large sink for anthropogenic carbon. Comparison of carbon stocks in Oxisols sampled near Manaus, Brazil, shows no measurable change in organic carbon stocks over the past 20 years. Simple models estimating the response of soil carbon pools to a sustained 0.5% yr−1 increase in productivity result in C storage rates of 0.09 to 0.13 MgC ha−1 yr8722;1 in soil organic matter, with additional potential storage of 0.18 to 0.27 MgC ha−1 yr−1 in surface litter and roots. Most storage occurs in organic matter pools with turnover times less than a decade. Export of carbon in dissolved form from upland terra firme Oxisols likely accounts for <0.2 MgC ha8722;1 yr8722;1, but more work is required to assess the export potential for periodically inundated Spodosols.
650 $aCarbono
650 $aDecomposição
650 $aSolo
650 $aSolo Tropical
650 $aTextura
653 $aCiclo de carbono
700 1 $aCAMARGO, P. B. de
700 1 $aMARTINELLI, L. A.
700 1 $aTRUMBORE, S. E.
700 1 $aCOSTA, E. S. da
700 1 $aSANTOS, J.
700 1 $aHIGUCHI, N.
700 1 $aOLIVEIRA JUNIOR, R. C.
773 $tGlobal Biogeochemical Cycles$gv. 17, n. 2, Jun. 2003.
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