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| 1. |  | BALBINO, L. C.; BRUAND, A.; BROSSARD, M.; GRIMALDI, M.; HAJNOS, M.; GUIMARAES, M. F. Changes in porosity and microaggregation in clayey Ferralsols of the Brazilian Cerrado on clearing for pasture. European Journal of Soil Science, v. 53, n. 2, p. 219-230, June 2002.| Biblioteca(s): Embrapa Arroz e Feijão. |
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| Registros recuperados : 2 | |
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 | Acesso ao texto completo restrito à biblioteca da Embrapa Cerrados. Para informações adicionais entre em contato com cpac.biblioteca@embrapa.br. |
Registro Completo
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Biblioteca(s): |
Embrapa Cerrados. |
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Data corrente: |
29/08/2002 |
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Data da última atualização: |
29/08/2002 |
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Autoria: |
BALBINO, L. C.; BRUAND, A.; BROSSARD, M.; GRIMALDI, M.; HAJNOS, M.; GUIMARAES, M. F. |
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Título: |
Changes in porosity and microaggregation in clayey Ferralsols of the Brazilian Cerrado on clearing for pasture. |
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Ano de publicação: |
2002 |
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Fonte/Imprenta: |
European Journal of Soil Science, v. 53, p. 219-230, Jun. 2002. |
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Idioma: |
Inglês |
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Conteúdo: |
Ferrasols have a macrostructure that is weak to moderate and a strong microstructure consisting of near spherical microaggregates. We have studied the evolution of the structure under changing land use in two Ferralsols under a native Cerrado and under pasture after recent clearing by measuring bulk density. We studied the microaggregates characteristics and resulting porosity using scanning electron microscopy and mercury porosimetry, respectively. Microaggregates 50-300 um in diameter are attributed to termites. They were in a much closer arrangement from the surface to 1 m depth under pasture than under Cerrado. Larger microaggregates, 500-1000 um in diameter, that are closely packed, resulted from earthworm activity. They were more numerous under pasture than under Cerrado. Thus within a few years, clearing and grazing have caused a dramatic decrease in microstructure that is one of the rare favourable characteristics of Ferralsols of agriculture. This evolution that affects the subsoil to 80-90 cm cannot be attributed to compaction by mechanical deforestation alone but seems to result from a change in the faunal activity in the faunal activity in the soil. Finally, the packing of the clay particles within the microaggregates was similar whatever the type microaggregate
and land use. Our results accord with ealier studies showing that the porosity resulting from clay packing varies little in Ferralsols in which the fine material is mainly kaolinite. |
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Palavras-Chave: |
Land clearing; Soil structures. |
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Thesagro: |
Cerrado; Desmatamento; Estrutura do Solo; Ferralsolo; Pastagem; Porosidade; Solo Argiloso. |
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Thesaurus NAL: |
clay soils; deforestation; Ferralsols; pastures; porosity. |
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Categoria do assunto: |
-- |
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Marc: |
LEADER 02413naa a2200349 a 4500
001 1565113
005 2002-08-29
008 2002 bl --- 0-- u #d
100 1 $aBALBINO, L. C.
245 $aChanges in porosity and microaggregation in clayey Ferralsols of the Brazilian Cerrado on clearing for pasture.
260 $c2002
520 $aFerrasols have a macrostructure that is weak to moderate and a strong microstructure consisting of near spherical microaggregates. We have studied the evolution of the structure under changing land use in two Ferralsols under a native Cerrado and under pasture after recent clearing by measuring bulk density. We studied the microaggregates characteristics and resulting porosity using scanning electron microscopy and mercury porosimetry, respectively. Microaggregates 50-300 um in diameter are attributed to termites. They were in a much closer arrangement from the surface to 1 m depth under pasture than under Cerrado. Larger microaggregates, 500-1000 um in diameter, that are closely packed, resulted from earthworm activity. They were more numerous under pasture than under Cerrado. Thus within a few years, clearing and grazing have caused a dramatic decrease in microstructure that is one of the rare favourable characteristics of Ferralsols of agriculture. This evolution that affects the subsoil to 80-90 cm cannot be attributed to compaction by mechanical deforestation alone but seems to result from a change in the faunal activity in the faunal activity in the soil. Finally, the packing of the clay particles within the microaggregates was similar whatever the type microaggregate and land use. Our results accord with ealier studies showing that the porosity resulting from clay packing varies little in Ferralsols in which the fine material is mainly kaolinite.
650 $aclay soils
650 $adeforestation
650 $aFerralsols
650 $apastures
650 $aporosity
650 $aCerrado
650 $aDesmatamento
650 $aEstrutura do Solo
650 $aFerralsolo
650 $aPastagem
650 $aPorosidade
650 $aSolo Argiloso
653 $aLand clearing
653 $aSoil structures
700 1 $aBRUAND, A.
700 1 $aBROSSARD, M.
700 1 $aGRIMALDI, M.
700 1 $aHAJNOS, M.
700 1 $aGUIMARAES, M. F.
773 $tEuropean Journal of Soil Science$gv. 53, p. 219-230, Jun. 2002.
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