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| 18. |  | GARCIA, F. R. M.; TORRES, V. S. A importancia da preservacao da mata nativa do Rio Grande do Sul com fins de reduzir a migracao de Maecolaspis sp. (Coleoptera. chrysomelidae, elmopinae) para areas com plantas cultivadas. In: CONGRESSO FLORESTAL PANAMERICANO, 1.; CONGRESSO FLORESTAL BRASILEIRO, 7., 1993, Curitiba. Floresta para o Desenvolvimento: Política, Ambiente, Tecnologia e Mercado: anais. São Paulo: SBS; [S.l.]: SBEF, 1993. v. 2, p. 715.| Biblioteca(s): Embrapa Florestas. |
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| Registros recuperados : 155 | |
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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
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Biblioteca(s): |
Embrapa Florestas. |
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Data corrente: |
02/10/2015 |
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Data da última atualização: |
01/02/2016 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
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Circulação/Nível: |
A - 1 |
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Autoria: |
RAMOS, M. R.; MELO, V. F.; UHLMANN, A.; DEDECEK, R. A.; CURCIO, G. R. |
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Afiliação: |
Michele Ribeiro Ramos, Embrapa Florestas; Vander Freitas Melo, UFPR; ALEXANDRE UHLMANN, CNPF; Renato Antonio Dedecek, Embrapa Florestas; GUSTAVO RIBAS CURCIO, CNPF. |
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Título: |
Clay mineralogy and genesis of fragipan in soils from Southeast Brazil. |
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Ano de publicação: |
2015 |
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Fonte/Imprenta: |
Catena, v. 135, p. 22-28, Dec. 2015. |
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DOI: |
http://dx.doi.org/10.1016/j.catena.2015.06.016 |
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Idioma: |
Inglês |
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Conteúdo: |
Fragipan horizon has a hard consistencywhen dry but is brittle when moist. Such a horizon restricts root growth and water infiltration due to the low volume of macropores and discontinuous voids. In Rio de Janeiro state in Brazil, neighboring soils were developed from different materials (sediments and granite/gneiss) and were subject to the same environmental conditions; one manifested fragipan characteristics in the subsurface and the other did not. The main objective of this study was to characterize and quantify clay minerals and relate their properties to the genesis of fragipan horizons. The fragipan in the studied soils show high bulk density (1.67 g cm?3) and low average macroporosity (0.03 cm cm?3), total porosity (0.42 cm cm?3) and hydraulic conductivity (1.43 cm h?1). Sequential and interrelated causes favored the formation of fragipan horizons: 1) face to face adjustment of kaolinite (Ka) filling of larger spaces occurring between sand grains, favored by low goethite contents and the absence of hematite and gibbsite; and 2) mineral binding and cementation of sand, silt and clay fractions by amorphous materials. Higher amounts of goethite and lower amounts of amorphous materials in the clay fraction were associated with horizons with higher total porosity. |
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Palavras-Chave: |
Brasil; Gênese; Mineralogia de argila; Sul. |
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Thesagro: |
Solo. |
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Categoria do assunto: |
-- |
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Marc: |
LEADER 01951naa a2200241 a 4500
001 2025720
005 2016-02-01
008 2015 bl uuuu u00u1 u #d
024 7 $ahttp://dx.doi.org/10.1016/j.catena.2015.06.016$2DOI
100 1 $aRAMOS, M. R.
245 $aClay mineralogy and genesis of fragipan in soils from Southeast Brazil.$h[electronic resource]
260 $c2015
520 $aFragipan horizon has a hard consistencywhen dry but is brittle when moist. Such a horizon restricts root growth and water infiltration due to the low volume of macropores and discontinuous voids. In Rio de Janeiro state in Brazil, neighboring soils were developed from different materials (sediments and granite/gneiss) and were subject to the same environmental conditions; one manifested fragipan characteristics in the subsurface and the other did not. The main objective of this study was to characterize and quantify clay minerals and relate their properties to the genesis of fragipan horizons. The fragipan in the studied soils show high bulk density (1.67 g cm?3) and low average macroporosity (0.03 cm cm?3), total porosity (0.42 cm cm?3) and hydraulic conductivity (1.43 cm h?1). Sequential and interrelated causes favored the formation of fragipan horizons: 1) face to face adjustment of kaolinite (Ka) filling of larger spaces occurring between sand grains, favored by low goethite contents and the absence of hematite and gibbsite; and 2) mineral binding and cementation of sand, silt and clay fractions by amorphous materials. Higher amounts of goethite and lower amounts of amorphous materials in the clay fraction were associated with horizons with higher total porosity.
650 $aSolo
653 $aBrasil
653 $aGênese
653 $aMineralogia de argila
653 $aSul
700 1 $aMELO, V. F.
700 1 $aUHLMANN, A.
700 1 $aDEDECEK, R. A.
700 1 $aCURCIO, G. R.
773 $tCatena$gv. 135, p. 22-28, Dec. 2015.
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