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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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Registro original: |
Embrapa Solos (CNPS) |
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Origem |
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Registro |
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Registro Completo
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Biblioteca(s): |
Embrapa Clima Temperado. |
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Data corrente: |
15/05/1996 |
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Data da última atualização: |
17/07/2017 |
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Tipo da produção científica: |
Autoria/Organização/Edição de Livros |
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Autoria: |
SALLES, L. A. B. |
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Afiliação: |
Luiz Antonio B. Salles. |
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Título: |
Bioecologia e controle da mosca-das-frutas sul-americana. |
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Ano de publicação: |
1995 |
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Fonte/Imprenta: |
Pelotas: EMBRAPA-CPACT, 1995. |
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Páginas: |
58 p. |
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ISBN: |
85-5941-01-4 |
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Idioma: |
Português |
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Conteúdo: |
Anatrepha fraterculus (Wiedemann, 1830) (Diptera: Tephritidae) e conhecida pelo nome vulgar de moscar-das-frutas sul-americana (Stone, 1942). E originaria das americas, provavelmente da America do Sul, onde ocorre em um grande numero de locais e possui ampla gama de hospedeiros (Aluja, 1994), fatos que indicam a sua adaptacao ao meio ambiente. E uma especie basicamente neotropica, ocorrendo nos Estados Unidos (Texas) Mexico, America Central e America do Sul, entre as latitudes 27N e 35S. Como praga de importancia economica, restringe-se atualmente aos paises do Cone Sul, notadamente a Argentina, Brasil, Paraguai e Uruguai. No Peru e Equador, essa especie tambem e considerada uma praga importante, todavia nao se conhece o nivel de importancia economica. |
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Palavras-Chave: |
Bioecologia; Biologic control; Biology; Brasil; Centro de Pesquisa Agropecuária de Clima Temperado; Controle; EMBRAPA; Fruit fly; Identification; Injuries; Insect; Mosca-da-fruta; Mosca-das-frutas; Mosca-dasfrutas; Pelotas RS; RS; Sul. |
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Thesagro: |
Anastrepha Fraterculus; Biologia; Controle Biológico; Dano; Ecologia; Entomologia; Hospedeiro; Identificação; Inseticida; Inseto; Isca; Mosca das Frutas; Praga. |
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Thesaurus NAL: |
biological control; ecology; entomology. |
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Categoria do assunto: |
--
O Insetos e Entomologia |
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URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/92940/1/digitalizar0042.pdf
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Marc: |
LEADER 02012nam a2200517 a 4500
001 1742993
005 2017-07-17
008 1995 bl uuuu 00u1 u #d
100 1 $aSALLES, L. A. B.
245 $aBioecologia e controle da mosca-das-frutas sul-americana.
260 $aPelotas: EMBRAPA-CPACT$c1995
300 $a58 p.
520 $aAnatrepha fraterculus (Wiedemann, 1830) (Diptera: Tephritidae) e conhecida pelo nome vulgar de moscar-das-frutas sul-americana (Stone, 1942). E originaria das americas, provavelmente da America do Sul, onde ocorre em um grande numero de locais e possui ampla gama de hospedeiros (Aluja, 1994), fatos que indicam a sua adaptacao ao meio ambiente. E uma especie basicamente neotropica, ocorrendo nos Estados Unidos (Texas) Mexico, America Central e America do Sul, entre as latitudes 27N e 35S. Como praga de importancia economica, restringe-se atualmente aos paises do Cone Sul, notadamente a Argentina, Brasil, Paraguai e Uruguai. No Peru e Equador, essa especie tambem e considerada uma praga importante, todavia nao se conhece o nivel de importancia economica.
650 $abiological control
650 $aecology
650 $aentomology
650 $aAnastrepha Fraterculus
650 $aBiologia
650 $aControle Biológico
650 $aDano
650 $aEcologia
650 $aEntomologia
650 $aHospedeiro
650 $aIdentificação
650 $aInseticida
650 $aInseto
650 $aIsca
650 $aMosca das Frutas
650 $aPraga
653 $aBioecologia
653 $aBiologic control
653 $aBiology
653 $aBrasil
653 $aCentro de Pesquisa Agropecuária de Clima Temperado
653 $aControle
653 $aEMBRAPA
653 $aFruit fly
653 $aIdentification
653 $aInjuries
653 $aInsect
653 $aMosca-da-fruta
653 $aMosca-das-frutas
653 $aMosca-dasfrutas
653 $aPelotas RS
653 $aRS
653 $aSul
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Embrapa Clima Temperado (CPACT) |
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