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Registro Completo |
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Biblioteca(s): |
Embrapa Hortaliças. |
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Data corrente: |
10/11/2003 |
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Data da última atualização: |
10/11/2003 |
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Autoria: |
CAVALCANTI, M. L. F.; SOARES, F. A. L.; SOUSA JÚNIOR, S. P. de; SIQUEIRA, E. da C.; SILVA, C. F. da; BARROS JÚNIOR, G. |
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Título: |
Coaplicação de lâmina de irrigação na cultura da cenoura combinadas com diferentes doses de fósforo I: germinação e vigor inicial. |
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Ano de publicação: |
2003 |
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Fonte/Imprenta: |
In: CONGRESSO NACIONAL DE IRRIGAÇÃO E DRENAGEM, 13., 2003, Juazeiro. O agronegócio da agricultura irrigada com revitalização hídrica: a chave para mais empregos e reversão de ciclos de pobreza em ciclos de prosperidade: anais. Brasília: Associação Brasileira de Irrigação e Drenagem: Governo do Estado da Bahia, 2003. |
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Descrição Física: |
CD-ROM. |
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Idioma: |
Português |
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Palavras-Chave: |
Casa de vegetação; Lâmina de água. |
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Thesagro: |
Cenoura; Cultivo Protegido; Daucus Carota; Fósforo; Germinação; Irrigação. |
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Thesaurus Nal: |
vigor. |
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Categoria do assunto: |
-- |
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Marc: |
LEADER 01141naa a2200289 a 4500
001 1774864
005 2003-11-10
008 2003 bl uuuu u00u1 u #d
100 1 $aCAVALCANTI, M. L. F.
245 $aCoaplicação de lâmina de irrigação na cultura da cenoura combinadas com diferentes doses de fósforo I$bgerminação e vigor inicial.
260 $c2003
300 $cCD-ROM.
650 $avigor
650 $aCenoura
650 $aCultivo Protegido
650 $aDaucus Carota
650 $aFósforo
650 $aGerminação
650 $aIrrigação
653 $aCasa de vegetação
653 $aLâmina de água
700 1 $aSOARES, F. A. L.
700 1 $aSOUSA JÚNIOR, S. P. de
700 1 $aSIQUEIRA, E. da C.
700 1 $aSILVA, C. F. da
700 1 $aBARROS JÚNIOR, G.
773 $tIn: CONGRESSO NACIONAL DE IRRIGAÇÃO E DRENAGEM, 13., 2003, Juazeiro. O agronegócio da agricultura irrigada com revitalização hídrica: a chave para mais empregos e reversão de ciclos de pobreza em ciclos de prosperidade: anais. Brasília: Associação Brasileira de Irrigação e Drenagem: Governo do Estado da Bahia, 2003.
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Registro original: |
Embrapa Hortaliças (CNPH) |
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 | Acesso ao texto completo restrito à biblioteca da Embrapa Solos. Para informações adicionais entre em contato com cnps.biblioteca@embrapa.br. |
Registro Completo
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Biblioteca(s): |
Embrapa Solos. |
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Data corrente: |
27/04/2023 |
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Data da última atualização: |
05/12/2023 |
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Tipo da produção científica: |
Capítulo em Livro Técnico-Científico |
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Autoria: |
VIDAL-TORRADO, P.; BUURMAN, P.; MARTINEZ, P.; LOPES-MAZZETTO, J. M.; SCHELLEKENS, J.; COELHO, M. R.; GOMES, F. H. |
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Afiliação: |
PABLO VIDAL-TORRADO, UNIVERSIDADE DE SÃO PAULO; PETER BUURMAN, WAGENINGEN UNIVERSITY; PEDRO MARTINEZ, OREGON STATE UNIVERSITY; JOSIANE MILLANI LOPES-MAZZETTO, LINCOLN UNIVERSITY; JUDITH SCHELLEKENS, KU LEUVEN; MAURICIO RIZZATO COELHO, CNPS; FELIPE HAENEL GOMES, UNIVERSIDADE FEDERAL DE LAVRAS. |
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Título: |
Soils of restingas. |
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Ano de publicação: |
2023 |
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Fonte/Imprenta: |
In: SCHAEFER, C. E. G. R. (ed.). The soils of Brazil. Cham: Springer, 2023. cap. 14, p. 393-410. (World soils book series). |
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DOI: |
https://doi.org/10.1007/978-3-031-19949-3_14 |
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Idioma: |
Inglês |
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Conteúdo: |
The Restinga is one of the ecosystems of the Atlantic Rainforest biome in Brazil. It is characterized by extremely nutrient-poor soils formed in sandy coastal sediments from the Quaternary age. The highly dynamic environment of sandy coasts causes landforms with different microrelief. This, in combination with the poor and harsh conditions strongly influence both vegetation composition and ecological succession. Consequently soil formation and vegetation has remarkable variation at short distances within the Restinga ecosystem. This variation strongly depends on (i) geomorphological evolution (deposition/ erosion and age), (ii) particle size of the sediment (sand or clay), (iii) drainage conditions, and (iv) organic matter inputs. Soils from the Restinga ecosystem include Espodossolos (Podzols), Neossolos Quartzarênicos (Arenosols), Organossolos (Histosols), and Gleissolos (Gleysols). However, poorly drained Espodossolos (Podzols) dominate this forested landscape due to the low and flat relief of the shoreline and large amounts of dissolved organic matter (DOM) produced upon decomposition of litter and roots in H, O, and A horizons. The morphology of Espodossolos in the Restinga ecosystem is complex, with a large short-distance variability in depths and shapes of the E- and B-horizons. In order to interpret soil-forming processes in the context of the landscape, transects of related profiles are studied in detail in the different geomorphic units. We connect soil morphology, micromorphology, organic matter chemistry, and microbiology with geomorphology at the ecosystem level. MenosThe Restinga is one of the ecosystems of the Atlantic Rainforest biome in Brazil. It is characterized by extremely nutrient-poor soils formed in sandy coastal sediments from the Quaternary age. The highly dynamic environment of sandy coasts causes landforms with different microrelief. This, in combination with the poor and harsh conditions strongly influence both vegetation composition and ecological succession. Consequently soil formation and vegetation has remarkable variation at short distances within the Restinga ecosystem. This variation strongly depends on (i) geomorphological evolution (deposition/ erosion and age), (ii) particle size of the sediment (sand or clay), (iii) drainage conditions, and (iv) organic matter inputs. Soils from the Restinga ecosystem include Espodossolos (Podzols), Neossolos Quartzarênicos (Arenosols), Organossolos (Histosols), and Gleissolos (Gleysols). However, poorly drained Espodossolos (Podzols) dominate this forested landscape due to the low and flat relief of the shoreline and large amounts of dissolved organic matter (DOM) produced upon decomposition of litter and roots in H, O, and A horizons. The morphology of Espodossolos in the Restinga ecosystem is complex, with a large short-distance variability in depths and shapes of the E- and B-horizons. In order to interpret soil-forming processes in the context of the landscape, transects of related profiles are studied in detail in the different geomorphic units. We connect soil morphology,... Mostrar Tudo |
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Palavras-Chave: |
Bh degradation; Brazilian coastal plain; Ichnofossil; Podzol micromorphology; Podzol morphology; Podzolization; Tropical podzol. |
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Thesagro: |
Podzólico; Restinga; Solo Tropical. |
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Thesaurus NAL: |
Podzols; Tropical soils. |
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Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
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Marc: |
LEADER 02619naa a2200349 a 4500
001 2153407
005 2023-12-05
008 2023 bl uuuu u00u1 u #d
024 7 $ahttps://doi.org/10.1007/978-3-031-19949-3_14$2DOI
100 1 $aVIDAL-TORRADO, P.
245 $aSoils of restingas.$h[electronic resource]
260 $c2023
520 $aThe Restinga is one of the ecosystems of the Atlantic Rainforest biome in Brazil. It is characterized by extremely nutrient-poor soils formed in sandy coastal sediments from the Quaternary age. The highly dynamic environment of sandy coasts causes landforms with different microrelief. This, in combination with the poor and harsh conditions strongly influence both vegetation composition and ecological succession. Consequently soil formation and vegetation has remarkable variation at short distances within the Restinga ecosystem. This variation strongly depends on (i) geomorphological evolution (deposition/ erosion and age), (ii) particle size of the sediment (sand or clay), (iii) drainage conditions, and (iv) organic matter inputs. Soils from the Restinga ecosystem include Espodossolos (Podzols), Neossolos Quartzarênicos (Arenosols), Organossolos (Histosols), and Gleissolos (Gleysols). However, poorly drained Espodossolos (Podzols) dominate this forested landscape due to the low and flat relief of the shoreline and large amounts of dissolved organic matter (DOM) produced upon decomposition of litter and roots in H, O, and A horizons. The morphology of Espodossolos in the Restinga ecosystem is complex, with a large short-distance variability in depths and shapes of the E- and B-horizons. In order to interpret soil-forming processes in the context of the landscape, transects of related profiles are studied in detail in the different geomorphic units. We connect soil morphology, micromorphology, organic matter chemistry, and microbiology with geomorphology at the ecosystem level.
650 $aPodzols
650 $aTropical soils
650 $aPodzólico
650 $aRestinga
650 $aSolo Tropical
653 $aBh degradation
653 $aBrazilian coastal plain
653 $aIchnofossil
653 $aPodzol micromorphology
653 $aPodzol morphology
653 $aPodzolization
653 $aTropical podzol
700 1 $aBUURMAN, P.
700 1 $aMARTINEZ, P.
700 1 $aLOPES-MAZZETTO, J. M.
700 1 $aSCHELLEKENS, J.
700 1 $aCOELHO, M. R.
700 1 $aGOMES, F. H.
773 $tIn: SCHAEFER, C. E. G. R. (ed.). The soils of Brazil. Cham: Springer, 2023. cap. 14, p. 393-410. (World soils book series).
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