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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. |
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Registro Completo |
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Biblioteca(s): |
Embrapa Solos. |
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Data corrente: |
18/08/2015 |
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Data da última atualização: |
08/10/2021 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
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Autoria: |
MARQUES, F. A.; BUURMAN, P.; SCHELLEKENS, J.; VIDAL-TORRADO, P. |
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Afiliação: |
FLAVIO ADRIANO MARQUES, CNPS; PETER BUURMAN, WAGENINGEN UNIVERSITY; JUDITH SCHELLEKENS, ESALQ/USP; PABLO VIDAL-TORRADO, ESALQ/USP. |
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Título: |
Molecular chemistry in humic Ferralsols from Brazilian Cerrado and forest biomes indicates a major contribution from black carbon in the subsoil. |
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Ano de publicação: |
2015 |
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Fonte/Imprenta: |
Journal of Analytical and Applied Pyrolysis, v. 113, p. 518-528, May 2015. |
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DOI: |
https://doi.org/10.1016/j.jaap.2015.03.016 |
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Idioma: |
Inglês |
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Conteúdo: |
Soil organic matter (OM) stability plays an important role in the global carbon cycle. The molecular characterisation of soil OM may contribute to an understanding of the feedback mechanisms between soil OM and climate. Umbric Ferralsols with humic properties (humic Ferralsols) are characterised by a thick dark carbon-rich A horizon, and co-occur next to Umbric Ferralsols without humic characteristics. They are concentrated in south-eastern Brazil which suggests an environmental control. In order to understand OM stability in these soils, humic Ferralsols from three Brazilian biomes were studied, including Cerrado (savanna), subtropical forest and tropical forest. The studied soils were developed on several geological substrates, including basalt, gneiss, chamokites, phyllite and tertiary sediments. The molecular composition of the free light fraction (FLF), occluded light fraction (OLF) and 0.1 M NaOH extractable OM of samples from topsoil and subsoil from eight profiles was examined using analytical pyrolysis (pyrolysis-GC/MS). The light fraction reflects litter and charcoal, obtained by density fractionation before (FLF) and after (OLF) ultrasonic disruption; the NaOH extractable fraction (humic acid + fulvic acid) reflects more decomposed material. The chemical differences among soils from different Brazilian biomes were much smaller than the vertical gradient within each profile. The results showed that, within the light fractions, the content of which varied between 2% and 22% of the total carbon content (Ct), black carbon (BC) derived pyrolysis products showed a higher abundance in the topsoil. In the extractable OM, which varied between 46% and 88% of Ct, BC derived pyrolysis products showed a higher abundance in the subsoil. This suggests a continuous input of BC and an increase in the degree of decomposition with depth. Pyrolysis products associated with BC contributed up to 10% to the extractable pyrolysable fraction in the subsoil. The results suggest that degradation of charcoal, which is translocated to the subsoil by macroscopic soil organisms, results in a relative high contribution from naphthalene, 2-ethenylnaphthalene, phenanthrene, benzene, dibenzofuran and benzonitrile (subsoil) compared to (other) polyaromatic hydrocarbons (PAHs; C1-, C2- and C3-naphthalenes and fluorene) in relatively fresh charcoal (topsoil). The results highlight the importance of the subsoil in studies of the long term effects of fire on soil OM and suggest that BC is an important factor that underlies carbon stability in humic Ferralsols. MenosSoil organic matter (OM) stability plays an important role in the global carbon cycle. The molecular characterisation of soil OM may contribute to an understanding of the feedback mechanisms between soil OM and climate. Umbric Ferralsols with humic properties (humic Ferralsols) are characterised by a thick dark carbon-rich A horizon, and co-occur next to Umbric Ferralsols without humic characteristics. They are concentrated in south-eastern Brazil which suggests an environmental control. In order to understand OM stability in these soils, humic Ferralsols from three Brazilian biomes were studied, including Cerrado (savanna), subtropical forest and tropical forest. The studied soils were developed on several geological substrates, including basalt, gneiss, chamokites, phyllite and tertiary sediments. The molecular composition of the free light fraction (FLF), occluded light fraction (OLF) and 0.1 M NaOH extractable OM of samples from topsoil and subsoil from eight profiles was examined using analytical pyrolysis (pyrolysis-GC/MS). The light fraction reflects litter and charcoal, obtained by density fractionation before (FLF) and after (OLF) ultrasonic disruption; the NaOH extractable fraction (humic acid + fulvic acid) reflects more decomposed material. The chemical differences among soils from different Brazilian biomes were much smaller than the vertical gradient within each profile. The results showed that, within the light fractions, the content of which varied between 2%... Mostrar Tudo |
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Palavras-Chave: |
Black carbon; Floresta Atlântica; Pastagem do Cerrado; Pirólise. |
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Thesagro: |
Carbono; Latossolo; Subsolo. |
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Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
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Marc: |
LEADER 03403naa a2200253 a 4500
001 2022152
005 2021-10-08
008 2015 bl uuuu u00u1 u #d
024 7 $ahttps://doi.org/10.1016/j.jaap.2015.03.016$2DOI
100 1 $aMARQUES, F. A.
245 $aMolecular chemistry in humic Ferralsols from Brazilian Cerrado and forest biomes indicates a major contribution from black carbon in the subsoil.$h[electronic resource]
260 $c2015
520 $aSoil organic matter (OM) stability plays an important role in the global carbon cycle. The molecular characterisation of soil OM may contribute to an understanding of the feedback mechanisms between soil OM and climate. Umbric Ferralsols with humic properties (humic Ferralsols) are characterised by a thick dark carbon-rich A horizon, and co-occur next to Umbric Ferralsols without humic characteristics. They are concentrated in south-eastern Brazil which suggests an environmental control. In order to understand OM stability in these soils, humic Ferralsols from three Brazilian biomes were studied, including Cerrado (savanna), subtropical forest and tropical forest. The studied soils were developed on several geological substrates, including basalt, gneiss, chamokites, phyllite and tertiary sediments. The molecular composition of the free light fraction (FLF), occluded light fraction (OLF) and 0.1 M NaOH extractable OM of samples from topsoil and subsoil from eight profiles was examined using analytical pyrolysis (pyrolysis-GC/MS). The light fraction reflects litter and charcoal, obtained by density fractionation before (FLF) and after (OLF) ultrasonic disruption; the NaOH extractable fraction (humic acid + fulvic acid) reflects more decomposed material. The chemical differences among soils from different Brazilian biomes were much smaller than the vertical gradient within each profile. The results showed that, within the light fractions, the content of which varied between 2% and 22% of the total carbon content (Ct), black carbon (BC) derived pyrolysis products showed a higher abundance in the topsoil. In the extractable OM, which varied between 46% and 88% of Ct, BC derived pyrolysis products showed a higher abundance in the subsoil. This suggests a continuous input of BC and an increase in the degree of decomposition with depth. Pyrolysis products associated with BC contributed up to 10% to the extractable pyrolysable fraction in the subsoil. The results suggest that degradation of charcoal, which is translocated to the subsoil by macroscopic soil organisms, results in a relative high contribution from naphthalene, 2-ethenylnaphthalene, phenanthrene, benzene, dibenzofuran and benzonitrile (subsoil) compared to (other) polyaromatic hydrocarbons (PAHs; C1-, C2- and C3-naphthalenes and fluorene) in relatively fresh charcoal (topsoil). The results highlight the importance of the subsoil in studies of the long term effects of fire on soil OM and suggest that BC is an important factor that underlies carbon stability in humic Ferralsols.
650 $aCarbono
650 $aLatossolo
650 $aSubsolo
653 $aBlack carbon
653 $aFloresta Atlântica
653 $aPastagem do Cerrado
653 $aPirólise
700 1 $aBUURMAN, P.
700 1 $aSCHELLEKENS, J.
700 1 $aVIDAL-TORRADO, P.
773 $tJournal of Analytical and Applied Pyrolysis$gv. 113, p. 518-528, May 2015.
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Registro original: |
Embrapa Solos (CNPS) |
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Biblioteca |
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Origem |
Tipo/Formato |
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Registro |
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Registro Completo
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Biblioteca(s): |
Embrapa Agroindústria de Alimentos. |
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Data corrente: |
02/02/2009 |
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Data da última atualização: |
08/05/2009 |
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Tipo da produção científica: |
Resumo em Anais de Congresso |
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Autoria: |
NEVES JUNIOR, A. C. V.; SOARES, A. G.; FONSECA, M. J. de O.; MACHADO, E. G.; COSTA, M. G. S.; VIANA, P. R. N. |
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Afiliação: |
Augusto César Vieira Neves Junior, UFRRJ; Antonio Gomes Soares, CTAA; Marcos José de Oliveira Fonseca, CTAA; Eduardo Gabrig Machado, UFRRJ; Márcio Gama Santos Costa, UFRRJ; Paulo Roberto Nascimento Viana, Universidade Estácio de Sá. |
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Título: |
Características da produção de goiaba no distrito de Xerén, município de Duque de Caxias-RJ. |
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Ano de publicação: |
2008 |
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Fonte/Imprenta: |
In: REUNIÃO ANUAL DA SOCIEDADE INTERAMERICANA DE HORTICULTURA TROPICAL, 54., 2008, Vitória, CE. Livro de resumos... Fortaleza: Embrapa Agroindústria Tropical, 2008. P.252. |
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Idioma: |
Português |
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Palavras-Chave: |
Distrito de Xerém; Produção de goiaba. |
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Categoria do assunto: |
-- |
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Marc: |
LEADER 00721naa a2200193 a 4500
001 1416807
005 2009-05-08
008 2008 bl --- 0-- u #d
100 1 $aNEVES JUNIOR, A. C. V.
245 $aCaracterísticas da produção de goiaba no distrito de Xerén, município de Duque de Caxias-RJ.
260 $c2008
653 $aDistrito de Xerém
653 $aProdução de goiaba
700 1 $aSOARES, A. G.
700 1 $aFONSECA, M. J. de O.
700 1 $aMACHADO, E. G.
700 1 $aCOSTA, M. G. S.
700 1 $aVIANA, P. R. N.
773 $tIn: REUNIÃO ANUAL DA SOCIEDADE INTERAMERICANA DE HORTICULTURA TROPICAL, 54., 2008, Vitória, CE. Livro de resumos... Fortaleza: Embrapa Agroindústria Tropical, 2008. P.252.
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Embrapa Agroindústria de Alimentos (CTAA) |
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