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Registro Completo |
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Biblioteca(s): |
Embrapa Rondônia. |
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Data corrente: |
22/01/2015 |
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Data da última atualização: |
22/01/2015 |
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Autoria: |
WADT, P. G. S.; MARCOLAN, A. L.; MATOSO, S. C. G.; PEREIRA, M. G. (ed.). |
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Afiliação: |
PAULO GUILHERME SALVADOR WADT, CPAF-AC; ALAERTO LUIZ MARCOLAN, CPAF-RO; STELLA CRISTIANI GONÇALVES MATOSO, IFRO; MARCOS GERVASIO PEREIRA, UNIVERSIDADE FEDERAL RURAL DO RIO DE JANEIRO. |
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Título: |
Manejo dos solos e a sustentabilidade da produção agrícola na Amazônia Ocidental: II Reunião de Ciência do Solo da Amazônia Ocidental. |
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Ano de publicação: |
2014 |
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Fonte/Imprenta: |
Porto Velho: AICSA, 2014. |
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Páginas: |
289 p. |
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ISBN: |
978-15-032933-04 |
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Idioma: |
Português |
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Notas: |
Registra parte das palestras e conferências realizadas durante a II Reunião de Ciência do Solo da Amazônia Ocidental. |
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Palavras-Chave: |
Amazônia Ocidental. |
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Thesagro: |
Manejo do Solo; Pedologia; Produção Agrícola. |
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Categoria do assunto: |
K Ciência Florestal e Produtos de Origem Vegetal |
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Marc: |
LEADER 00772nam a2200217 a 4500
001 2006400
005 2015-01-22
008 2014 bl uuuu 00u1 u #d
020 $a978-15-032933-04
100 1 $aWADT, P. G. S.
245 $aManejo dos solos e a sustentabilidade da produção agrícola na Amazônia Ocidental$bII Reunião de Ciência do Solo da Amazônia Ocidental.
260 $aPorto Velho: AICSA$c2014
300 $a289 p.
500 $aRegistra parte das palestras e conferências realizadas durante a II Reunião de Ciência do Solo da Amazônia Ocidental.
650 $aManejo do Solo
650 $aPedologia
650 $aProdução Agrícola
653 $aAmazônia Ocidental
700 1 $aMARCOLAN, A. L.
700 1 $aMATOSO, S. C. G.
700 1 $aPEREIRA, M. G.
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Registro original: |
Embrapa Rondônia (CPAF-RO) |
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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: |
11/10/2021 |
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Data da última atualização: |
11/10/2021 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
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Autoria: |
BOULET, R.; FRITSCH, E.; FILIZOLA, H. F.; ARAUJO FILHO, J. C. de; LEPRUN, J. C.; BARRETTO, F.; BALAN, E.; TESSIER, D. |
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Afiliação: |
R. BOULET, USP/ORSTOM; E. FRITSCH, USP/ORSTOM; HELOISA FERREIRA FILIZOLA, CNPMA; JOSE COELHO DE ARAUJO FILHO, CNPS; J. C. LEPRUN, ORSTOM; F. BARRETTO; E. BALAN, USP/ORSTOM; D. TESSIER, INRA. |
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Título: |
Iron bands, fragipans and duripans in the Northeastern plateaus of Brazil: properties and genesis. |
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Ano de publicação: |
1998 |
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Fonte/Imprenta: |
Canadian Journal of Soil Science, v. 78, n. 3, p. 519-530, Aug. 1998. |
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DOI: |
https://doi.org/10.4141/S98-030 |
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Idioma: |
Inglês |
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Conteúdo: |
Iron bands, fragipans and duripans are common in yellow low-activity clay soils developed from the Barreiras Group in coastal plateaus of northeastern Brazil. Such indurated horizons are found in depressions of the plateaus where sugar cane growth is greatly reduced. Little research has being done on the nature of their bonding agents and their genesis. Research carried out in arid zones has frequently attributed duripan consistency to amorphous silica; however, duripans in northeast Brazil occur under higher rainfall (1500-2000 mm). The objective of this work was to study the nature and distribution of soil features in a plateau to better understand the processes associated with soil hardening. Two transects, across a small and a large depression, were investigated using field soil characterisation, micromorphological techniques, and mineralogical and geochemical analyses. The formation of the indurated horizons studied is due to two sequential processes: development of aquic conditions and incipient podzolization. Such processes have affected the upper part of a thin (<0.6 m in small depressions) or thick (>0.6 m in large depressions) compact clay horizon, showing horizontal plans likely inherited from the sediment. Onset of aquatic conditions formed the first fragipans overlying iron bands. Later, aquic conditions are combined with incipient podzolization to produce bleached loose horizons overlying duripans and iron bands. As the bonding agents in the duripans are organo-metallic complexes, these duripans appear to be very different from those described in arid environments. MenosIron bands, fragipans and duripans are common in yellow low-activity clay soils developed from the Barreiras Group in coastal plateaus of northeastern Brazil. Such indurated horizons are found in depressions of the plateaus where sugar cane growth is greatly reduced. Little research has being done on the nature of their bonding agents and their genesis. Research carried out in arid zones has frequently attributed duripan consistency to amorphous silica; however, duripans in northeast Brazil occur under higher rainfall (1500-2000 mm). The objective of this work was to study the nature and distribution of soil features in a plateau to better understand the processes associated with soil hardening. Two transects, across a small and a large depression, were investigated using field soil characterisation, micromorphological techniques, and mineralogical and geochemical analyses. The formation of the indurated horizons studied is due to two sequential processes: development of aquic conditions and incipient podzolization. Such processes have affected the upper part of a thin (<0.6 m in small depressions) or thick (>0.6 m in large depressions) compact clay horizon, showing horizontal plans likely inherited from the sediment. Onset of aquatic conditions formed the first fragipans overlying iron bands. Later, aquic conditions are combined with incipient podzolization to produce bleached loose horizons overlying duripans and iron bands. As the bonding agents in the duripans are organo... Mostrar Tudo |
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Palavras-Chave: |
Barreiras Group; Duripans; Iron bands; Organo-metallic complexes. |
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Thesaurus NAL: |
Clay soils; Fragipans; Soil morphology; Ultisols. |
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Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
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Marc: |
LEADER 02521naa a2200313 a 4500
001 2135232
005 2021-10-11
008 1998 bl uuuu u00u1 u #d
024 7 $ahttps://doi.org/10.4141/S98-030$2DOI
100 1 $aBOULET, R.
245 $aIron bands, fragipans and duripans in the Northeastern plateaus of Brazil$bproperties and genesis.$h[electronic resource]
260 $c1998
520 $aIron bands, fragipans and duripans are common in yellow low-activity clay soils developed from the Barreiras Group in coastal plateaus of northeastern Brazil. Such indurated horizons are found in depressions of the plateaus where sugar cane growth is greatly reduced. Little research has being done on the nature of their bonding agents and their genesis. Research carried out in arid zones has frequently attributed duripan consistency to amorphous silica; however, duripans in northeast Brazil occur under higher rainfall (1500-2000 mm). The objective of this work was to study the nature and distribution of soil features in a plateau to better understand the processes associated with soil hardening. Two transects, across a small and a large depression, were investigated using field soil characterisation, micromorphological techniques, and mineralogical and geochemical analyses. The formation of the indurated horizons studied is due to two sequential processes: development of aquic conditions and incipient podzolization. Such processes have affected the upper part of a thin (<0.6 m in small depressions) or thick (>0.6 m in large depressions) compact clay horizon, showing horizontal plans likely inherited from the sediment. Onset of aquatic conditions formed the first fragipans overlying iron bands. Later, aquic conditions are combined with incipient podzolization to produce bleached loose horizons overlying duripans and iron bands. As the bonding agents in the duripans are organo-metallic complexes, these duripans appear to be very different from those described in arid environments.
650 $aClay soils
650 $aFragipans
650 $aSoil morphology
650 $aUltisols
653 $aBarreiras Group
653 $aDuripans
653 $aIron bands
653 $aOrgano-metallic complexes
700 1 $aFRITSCH, E.
700 1 $aFILIZOLA, H. F.
700 1 $aARAUJO FILHO, J. C. de
700 1 $aLEPRUN, J. C.
700 1 $aBARRETTO, F.
700 1 $aBALAN, E.
700 1 $aTESSIER, D.
773 $tCanadian Journal of Soil Science$gv. 78, n. 3, p. 519-530, Aug. 1998.
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