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| 2. |  | PARAHYBA, R. da B. V.; SILVA, M. S. L. da; ROLIN NETO, F. C. R.; LOPES, E. H. B.; CALDAS, A. M. Avaliação do potencial agrícola das terras do município de Inhapi-AL. In: JORNADA DE ENSINO, PESQUISA E EXTENSÃO DA UFRPE, 10., 2010, Recife. Anais... Recife: UFRPE, 2010.| Biblioteca(s): Embrapa Solos. |
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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
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Biblioteca(s): |
Embrapa Amazônia Oriental. |
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Data corrente: |
10/05/1997 |
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Data da última atualização: |
07/07/2020 |
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Autoria: |
NEPSTAD, D. C.; CARVALHO, C. R. de; DAVIDSON, E. A.; JIPP, P. H.; LEFEBIRE, P. A.; NEGREIROS, G. H.; SILVA, E. D. da; STONE, T. A.; TRUMBORE, S. E. |
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Afiliação: |
Daniel C. Nepstad, Woods Hole Research Center; CLAUDIO JOSE REIS DE CARVALHO, CPATU; Eric A. Davidson, Woods Hole Research Center; Peter H. Jipp, Woods Hole Research Center; Paul A. Lefebvre, Woods Hole Research Center; Gustavo H. Negreiros, Woods Hole Research Center; Elson D. da Silva, CPATU; Thomas A. Stone, Woods Hole Research Center; Susan E. Trumbore, University of Californi. |
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Título: |
The role of deep roots in the hydrological and carbon cycles of Amazonian forests and pastures. |
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Ano de publicação: |
1994 |
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Fonte/Imprenta: |
Nature, v. 372, n. 6507, p.666-669, Dec. 1994. |
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DOI: |
10.1038/372666a0 |
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Idioma: |
Inglês |
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Conteúdo: |
DEFORESTATION and logging transform more forest in eastern and southern Amazonia than in any other region of the world1?3. This forest alteration affects regional hydrology4?11 and the global carbon cycle12?14, but current analyses of these effects neglect an important deep-soil link between the water and carbon cycles. Using rainfall data, satellite imagery and field studies, we estimate here that half of the closed forests of Brazilian Amazonia depend on deep root systems to maintain green canopies during the dry season. Evergreen forests in northeastern Pará state maintain evapotranspiration during five-month dry periods by absorbing water from the soil to depths of more than 8m. In contrast, although the degraded pastures of this region also contain deep-rooted woody plants, most pasture plants substantially reduce their leaf canopy in response to seasonal drought, thus reducing dry-season evapotranspiration and increasing potential subsurface runoff relative to the forests they replace. Deep roots that extract water also provide carbon to the soil. The forest soil below 1 m depth contains more carbon than does above-ground biomass, and as much as 15% of this deep-soil carbon turns over on annual or decadal timescales. Thus, forest alteration that affects depth distributions of carbon inputs from roots may also affect net carbon storage in the soil. |
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Palavras-Chave: |
Brasil; Ciclagem de carbono; Cycling; Essecia florestal; Forest; Plants; Profundidade da raiz. |
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Thesagro: |
Balanço Hídrico; Floresta; Pastagem; Planta. |
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Thesaurus NAL: |
Amazonia; depth; forest trees; pastures; roots; water balance. |
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Categoria do assunto: |
-- |
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Marc: |
LEADER 02493naa a2200433 a 4500
001 1373121
005 2020-07-07
008 1994 bl uuuu u00u1 u #d
024 7 $a10.1038/372666a0$2DOI
100 1 $aNEPSTAD, D. C.
245 $aThe role of deep roots in the hydrological and carbon cycles of Amazonian forests and pastures.
260 $c1994
520 $aDEFORESTATION and logging transform more forest in eastern and southern Amazonia than in any other region of the world1?3. This forest alteration affects regional hydrology4?11 and the global carbon cycle12?14, but current analyses of these effects neglect an important deep-soil link between the water and carbon cycles. Using rainfall data, satellite imagery and field studies, we estimate here that half of the closed forests of Brazilian Amazonia depend on deep root systems to maintain green canopies during the dry season. Evergreen forests in northeastern Pará state maintain evapotranspiration during five-month dry periods by absorbing water from the soil to depths of more than 8m. In contrast, although the degraded pastures of this region also contain deep-rooted woody plants, most pasture plants substantially reduce their leaf canopy in response to seasonal drought, thus reducing dry-season evapotranspiration and increasing potential subsurface runoff relative to the forests they replace. Deep roots that extract water also provide carbon to the soil. The forest soil below 1 m depth contains more carbon than does above-ground biomass, and as much as 15% of this deep-soil carbon turns over on annual or decadal timescales. Thus, forest alteration that affects depth distributions of carbon inputs from roots may also affect net carbon storage in the soil.
650 $aAmazonia
650 $adepth
650 $aforest trees
650 $apastures
650 $aroots
650 $awater balance
650 $aBalanço Hídrico
650 $aFloresta
650 $aPastagem
650 $aPlanta
653 $aBrasil
653 $aCiclagem de carbono
653 $aCycling
653 $aEssecia florestal
653 $aForest
653 $aPlants
653 $aProfundidade da raiz
700 1 $aCARVALHO, C. R. de
700 1 $aDAVIDSON, E. A.
700 1 $aJIPP, P. H.
700 1 $aLEFEBIRE, P. A.
700 1 $aNEGREIROS, G. H.
700 1 $aSILVA, E. D. da
700 1 $aSTONE, T. A.
700 1 $aTRUMBORE, S. E.
773 $tNature$gv. 372, n. 6507, p.666-669, Dec. 1994.
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