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Registro Completo |
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Biblioteca(s): |
Embrapa Instrumentação; Embrapa Solos; Embrapa Unidades Centrais. |
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Data corrente: |
22/11/2002 |
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Data da última atualização: |
17/07/2014 |
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Autoria: |
VAZ, C. M. P.; NAIME, J. M.; SILVA, A. M. da. |
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Título: |
Analisador granulométrico de solos. |
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Ano de publicação: |
1996 |
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Fonte/Imprenta: |
São Carlos, SP: Embrapa Instrumentação Agropecuária, 1996. |
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Páginas: |
5 p. |
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Série: |
(Embrapa Instrumentação Agropecuária. Comunicado Técnico, 5). |
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Idioma: |
Português |
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Notas: |
Entrada padronizada: MACEDO, A. |
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Palavras-Chave: |
Analisador granulométrico; Granulométrico; Solos. |
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Categoria do assunto: |
-- |
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URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/CNPDIA/9835/1/CT05_96.pdf
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Marc: |
LEADER 00592nam a2200193 a 4500
001 1027076
005 2014-07-17
008 1996 bl uuuu u0uu1 u #d
100 1 $aVAZ, C. M. P.
245 $aAnalisador granulométrico de solos.
260 $aSão Carlos, SP: Embrapa Instrumentação Agropecuária$c1996
300 $a5 p.
490 $a(Embrapa Instrumentação Agropecuária. Comunicado Técnico, 5).
500 $aEntrada padronizada: MACEDO, A.
653 $aAnalisador granulométrico
653 $aGranulométrico
653 $aSolos
700 1 $aNAIME, J. M.
700 1 $aSILVA, A. M. da
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Registro original: |
Embrapa Instrumentação (CNPDIA) |
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 | Acesso ao texto completo restrito à biblioteca da Embrapa Milho e Sorgo. Para informações adicionais entre em contato com cnpms.biblioteca@embrapa.br. |
Registro Completo
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Biblioteca(s): |
Embrapa Milho e Sorgo. |
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Data corrente: |
29/12/2001 |
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Data da última atualização: |
07/06/2018 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
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Autoria: |
ROSCOE, R.; BUURMAN, P.; VELTHORST, E. J.; VASCONCELLOS, C. A. |
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Afiliação: |
EMBRAPA-CNPMS. |
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Título: |
Soil organic matter dynamics in density and particle size fractions as revealed by the 13C/12C isotopic ratio in a cerrdo's oxisol. |
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Ano de publicação: |
2001 |
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Fonte/Imprenta: |
Geoderma, Amsterdam, v. 104, p. 185-202, 2001. |
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Idioma: |
Inglês |
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Conteúdo: |
In order to better understand the dynamics of soil organic matter (SOM) in Oxisols and the impact of converting native cerrado (savannah) into pasture, we studied the dynamics of different physically separated SOM pools at different depths in a cerrado oxisol (Typic Haplustox), under natural conditions and after 23 years cultivated pasture (Brachiaria spp.) via the replacement of the native C (C3-derived) by pasture C (C4-derived). Organic C stocks of the original cerrado (15+/- 3 kg m-2) and pasture (17 +/- 3 kg m-2) were not significantly different, which was attributed to the high biomass production of the tropical grasses and the protective effects of the high clay content (> 800 g kg-2). We observed that 89-91% of the total organic C accumulated in the clay + silt fraction. The replacement of cerrado-derived C by pasture-derived C was in average 36%, 34%, and 19% for Ap, AB1, and Bw2 horizons, respectively, suggesting a fast turnover rate of organic C regardless of the high clay content. The replacement decreased in the order: free low-density organic matter (LDOM) > heavy fractions (sand, silt, clay) > occluded-LDOM. The lower replacement of the occluded-LDOM compared to the heavy fractions was attributed to protection inside aggregates and to a possible accumulation of C3-derived charcoal (black carbon). After 23 years of pasture, about 50% of the total organic C in the free-LDOM in the topsoil was still from cerrado, indicating that a significant part of this fraction was relatively recalcitrant. Charcoal fragments observed in the fraction suggested that the recalcitrance was probably due to charred material. MenosIn order to better understand the dynamics of soil organic matter (SOM) in Oxisols and the impact of converting native cerrado (savannah) into pasture, we studied the dynamics of different physically separated SOM pools at different depths in a cerrado oxisol (Typic Haplustox), under natural conditions and after 23 years cultivated pasture (Brachiaria spp.) via the replacement of the native C (C3-derived) by pasture C (C4-derived). Organic C stocks of the original cerrado (15+/- 3 kg m-2) and pasture (17 +/- 3 kg m-2) were not significantly different, which was attributed to the high biomass production of the tropical grasses and the protective effects of the high clay content (> 800 g kg-2). We observed that 89-91% of the total organic C accumulated in the clay + silt fraction. The replacement of cerrado-derived C by pasture-derived C was in average 36%, 34%, and 19% for Ap, AB1, and Bw2 horizons, respectively, suggesting a fast turnover rate of organic C regardless of the high clay content. The replacement decreased in the order: free low-density organic matter (LDOM) > heavy fractions (sand, silt, clay) > occluded-LDOM. The lower replacement of the occluded-LDOM compared to the heavy fractions was attributed to protection inside aggregates and to a possible accumulation of C3-derived charcoal (black carbon). After 23 years of pasture, about 50% of the total organic C in the free-LDOM in the topsoil was still from cerrado, indicating that a significant part of this fractio... Mostrar Tudo |
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Palavras-Chave: |
Carbono organico; Densidade; Factionation; Fragmentacao; Isotop; Organic carbon; Particlesize; Particula; Savanna. |
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Thesagro: |
Cerrado; Isótopo; Matéria Orgânica; Solo; Tamanho. |
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Thesaurus NAL: |
density; organic matter; soil. |
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Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
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Marc: |
LEADER 02623naa a2200361 a 4500
001 1485178
005 2018-06-07
008 2001 bl uuuu u00u1 u #d
100 1 $aROSCOE, R.
245 $aSoil organic matter dynamics in density and particle size fractions as revealed by the 13C/12C isotopic ratio in a cerrdo's oxisol.$h[electronic resource]
260 $c2001
520 $aIn order to better understand the dynamics of soil organic matter (SOM) in Oxisols and the impact of converting native cerrado (savannah) into pasture, we studied the dynamics of different physically separated SOM pools at different depths in a cerrado oxisol (Typic Haplustox), under natural conditions and after 23 years cultivated pasture (Brachiaria spp.) via the replacement of the native C (C3-derived) by pasture C (C4-derived). Organic C stocks of the original cerrado (15+/- 3 kg m-2) and pasture (17 +/- 3 kg m-2) were not significantly different, which was attributed to the high biomass production of the tropical grasses and the protective effects of the high clay content (> 800 g kg-2). We observed that 89-91% of the total organic C accumulated in the clay + silt fraction. The replacement of cerrado-derived C by pasture-derived C was in average 36%, 34%, and 19% for Ap, AB1, and Bw2 horizons, respectively, suggesting a fast turnover rate of organic C regardless of the high clay content. The replacement decreased in the order: free low-density organic matter (LDOM) > heavy fractions (sand, silt, clay) > occluded-LDOM. The lower replacement of the occluded-LDOM compared to the heavy fractions was attributed to protection inside aggregates and to a possible accumulation of C3-derived charcoal (black carbon). After 23 years of pasture, about 50% of the total organic C in the free-LDOM in the topsoil was still from cerrado, indicating that a significant part of this fraction was relatively recalcitrant. Charcoal fragments observed in the fraction suggested that the recalcitrance was probably due to charred material.
650 $adensity
650 $aorganic matter
650 $asoil
650 $aCerrado
650 $aIsótopo
650 $aMatéria Orgânica
650 $aSolo
650 $aTamanho
653 $aCarbono organico
653 $aDensidade
653 $aFactionation
653 $aFragmentacao
653 $aIsotop
653 $aOrganic carbon
653 $aParticlesize
653 $aParticula
653 $aSavanna
700 1 $aBUURMAN, P.
700 1 $aVELTHORST, E. J.
700 1 $aVASCONCELLOS, C. A.
773 $tGeoderma, Amsterdam$gv. 104, p. 185-202, 2001.
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