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| Registros recuperados : 11 | |
| 3. |  | GAMA-RODRIGUES, A. C. da; BARROS, N. F. de; COMERFORD, N. B. Biomass and nutrient cycling in pure and mixed standes of native tree species in southeastern Bahia, Brasil. Revista Brasileira de Ciência do Solo, Viçosa, MG, v. 31, n. 2, p. 287-298, mar./abr. 2007. Título em Português: Biomassa e ciclagem de nutrientes por espécies florestais nativas em plantio puro e misto no sudeste da Bahia, Brasil.| Biblioteca(s): Embrapa Solos / UEP-Recife. |
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| 4. | | SANTANA, R. C.; BARROS, N. F.; NOVAIS, R. F; LEITE, H. G.; COMERFORD, N. B. Alocação de nutrientes em plantios de eucalipto no Brasil. Revista Brasileira de Ciência do Solo, Viçosa, MG, v. 32, número especial, p. 2723-2733, nov./dez., 2008. Separata de Revista Brasileira de Ciência do Solo, Viçosa, MG, v. 32, número especial, nov./dez., 2008.| Biblioteca(s): Embrapa Solos / UEP-Recife. |
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| 7. | | COMERFORD, N. B.; CROPPER, W.; GRIERSON, P. F.; ARAUJO, Q.; JOSE, S. Modeling P bioavailability and uptake in agroforestry systems. 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. 303-317. 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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| 8. | | SANTANA, R. C.; BARROS, N. F. de; LEITE, H. G.; COMERFORD, N. B.; NOVAIS, R. F. de. Estimativa de biomassa de plantios de eucalipto no Brasil. Revista Árvore, Viçosa, v. 32, n. 4, p. 687-696, jul./ago. 2008.| Biblioteca(s): Embrapa Florestas. |
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| 11. | | VELOSO, M. G.; DIECKOW, J.; ZANATTA, J. A.; BAYER, C.; HIGA, R. C. V.; BREVILIERI, R. C.; COMERFORD, N. B.; STOPPE, A. M. Reforestation with loblolly pine can restore the initial soil carbon stock relative to a subtropical natural forest after 30 years. European Journal of Forest Research, v. 137, p. 593-604, Oct. 2018.| Biblioteca(s): Embrapa Florestas. |
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| Registros recuperados : 11 | |
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 | Acesso ao texto completo restrito à biblioteca da Embrapa Florestas. Para informações adicionais entre em contato com cnpf.biblioteca@embrapa.br. |
Registro Completo
|
Biblioteca(s): |
Embrapa Florestas. |
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Data corrente: |
19/11/2018 |
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Data da última atualização: |
20/11/2018 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
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Circulação/Nível: |
B - 2 |
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Autoria: |
VELOSO, M. G.; DIECKOW, J.; ZANATTA, J. A.; BAYER, C.; HIGA, R. C. V.; BREVILIERI, R. C.; COMERFORD, N. B.; STOPPE, A. M. |
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Afiliação: |
Murilo Gomes Veloso, UFPR; Jeferson Dieckow, UFPR; JOSILEIA ACORDI ZANATTA, CNPF; Cimelio Bayer, UFRGS; ROSANA CLARA VICTORIA HIGA, CNPF; Reinaldo C. Brevilieri, UFPR; Nicholas B. Comerford, North Florida Research and Education Center; Aja M. Stoppe, University of Florida. |
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Título: |
Reforestation with loblolly pine can restore the initial soil carbon stock relative to a subtropical natural forest after 30 years. |
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Ano de publicação: |
2018 |
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Fonte/Imprenta: |
European Journal of Forest Research, v. 137, p. 593-604, Oct. 2018. |
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DOI: |
10.1007/s10342-018-1127-y |
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Idioma: |
Inglês |
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Conteúdo: |
We hypothesized that long-term loblolly pine (Pinus taeda L.) land-use restores SOC stock and lability of a subtropical Cambisol to the original levels of the natural forest (NF). Additionally, we hypothesized that roots are the major contributor to SOC and that soil stores most of the ecosystem total carbon (ETC). We investigated a chronosequence of loblolly pine land-use of 17 (first rotation) and 32 years (second rotation, unthinned or thinned) following clearing of the NF. The original SOC stock to 100 cm of NF (209 ± 9.4 Mg C ha?1) was depleted by 22% after 17 years of pine, possibly because of intense soil disturbance and low quantity and quality of the residue inputted during the pine stand implementation. However, the SOC stock was restored to the original stock of NF after 32 years of pine, with the input of above and belowground biomass at harvest of the first rotation possibly playing a role in this recovery. Thinning did not affect SOC stocks after 1 year. The POM-C reduced after 17 years and was not recovered after 32 years. We could not ascertain in 5-year evaluation whether root or litter was the major contributor to SOC. Soil held 72% of the ETC in NF and 48?59% in pine plantations, confirming that it stores most of the ETC. Overall, long-term loblolly pine land-use seems to restore the original soil carbon stock in this subtropical site, regardless of some lability losses. |
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Palavras-Chave: |
Forest floor; Loblolly pine; Physical fractionation; Soil carbon accumulation; Southern Brazil. |
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Thesagro: |
Carbono; Pinus Taeda; Solo. |
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Categoria do assunto: |
K Ciência Florestal e Produtos de Origem Vegetal |
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Marc: |
LEADER 02362naa a2200313 a 4500
001 2099552
005 2018-11-20
008 2018 bl uuuu u00u1 u #d
024 7 $a10.1007/s10342-018-1127-y$2DOI
100 1 $aVELOSO, M. G.
245 $aReforestation with loblolly pine can restore the initial soil carbon stock relative to a subtropical natural forest after 30 years.$h[electronic resource]
260 $c2018
520 $aWe hypothesized that long-term loblolly pine (Pinus taeda L.) land-use restores SOC stock and lability of a subtropical Cambisol to the original levels of the natural forest (NF). Additionally, we hypothesized that roots are the major contributor to SOC and that soil stores most of the ecosystem total carbon (ETC). We investigated a chronosequence of loblolly pine land-use of 17 (first rotation) and 32 years (second rotation, unthinned or thinned) following clearing of the NF. The original SOC stock to 100 cm of NF (209 ± 9.4 Mg C ha?1) was depleted by 22% after 17 years of pine, possibly because of intense soil disturbance and low quantity and quality of the residue inputted during the pine stand implementation. However, the SOC stock was restored to the original stock of NF after 32 years of pine, with the input of above and belowground biomass at harvest of the first rotation possibly playing a role in this recovery. Thinning did not affect SOC stocks after 1 year. The POM-C reduced after 17 years and was not recovered after 32 years. We could not ascertain in 5-year evaluation whether root or litter was the major contributor to SOC. Soil held 72% of the ETC in NF and 48?59% in pine plantations, confirming that it stores most of the ETC. Overall, long-term loblolly pine land-use seems to restore the original soil carbon stock in this subtropical site, regardless of some lability losses.
650 $aCarbono
650 $aPinus Taeda
650 $aSolo
653 $aForest floor
653 $aLoblolly pine
653 $aPhysical fractionation
653 $aSoil carbon accumulation
653 $aSouthern Brazil
700 1 $aDIECKOW, J.
700 1 $aZANATTA, J. A.
700 1 $aBAYER, C.
700 1 $aHIGA, R. C. V.
700 1 $aBREVILIERI, R. C.
700 1 $aCOMERFORD, N. B.
700 1 $aSTOPPE, A. M.
773 $tEuropean Journal of Forest Research$gv. 137, p. 593-604, Oct. 2018.
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