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Registro Completo |
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Biblioteca(s): |
Embrapa Florestas. |
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Data corrente: |
07/07/2014 |
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Data da última atualização: |
18/02/2015 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
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Autoria: |
RACHWAL, M. F. G.; ZANATTA, J. A.; DIECKOW, J.; DENEGA, G. L.; CURCIO, G. R.; BAYER, C. |
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Afiliação: |
MARCOS FERNANDO GLUCK RACHWAL, CNPF; JOSILEIA ACORDI ZANATTA, CNPF; JEFERSON DIECKOW, UFPR; GENUIR LUIS DENEGA, Estudande de doutorado UFRGS; GUSTAVO RIBAS CURCIO, CNPF; CIMELIO BAYER, Professor UFRGS. |
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Título: |
Methane fluxes from waterlogged and drained histosols of highland areas. |
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Ano de publicação: |
2014 |
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Fonte/Imprenta: |
Revista Brasileira de Ciência do Solo, v. 38, p. 486-494, 2014. |
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Idioma: |
Inglês |
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Conteúdo: |
Soil can be either source or sink of methane (CH4), depending on the balance between methanogenesis and methanotrophy, which are determined by pedological, climatic and management factors. The objective of this study was to assess the impact of drainage of a highland Haplic Histosol on CH4 fluxes. Field research was carried out in Ponta Grossa (Paraná, Brazil) based on the measurement of CH4 fluxes by the static chamber method in natural and drained Histosol, over one year (17 sampling events). The natural Histosol showed net CH4 eflux, with rates varying from 238 ?g m-2 h-1 CH4, in cool/cold periods, to 2,850 ?g m-2 h-1 CH4, in warm/hot periods, resulting a cumulative emission of 116 kg ha-1 yr-1 CH4. In the opposite, the drained Histosol showed net influx of CH4 (-39 to -146 ?g m-2 h-1), which resulted in a net consumption of 9 kg ha-1 yr-1 CH4. The main driving factors of CH4 consumption in the drained soil were the lowering of the water-table (on average -57 cm, vs -7 cm in natural soil) and the lower water content in the 0-10 cm layer (average of 5.5 kg kg-1, vs 9.9 kg kg-1 in natural soil). Although waterlogged Histosols of highland areas are regarded as CH4 sources, they fulfill fundamental functions in the ecosystem, such as the accumulation of organic carbon (581 Mg ha-1 C to a depth of 1 m) and water (8.6 million L ha-1 = 860 mm to a depth of 1 m). For this reason, these soils must not be drained as an alternative to mitigate CH4 emission, but effectively preserved. |
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Palavras-Chave: |
Gases de efeito estufa; Nível freático; Precipitação pluviométrica; Temperatura do ar; Umidade gravimétrica. |
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Thesagro: |
Água. |
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Categoria do assunto: |
-- |
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URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/104734/1/2014-API-Rachwal-MethaneFluxes.pdf
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Marc: |
LEADER 02245naa a2200253 a 4500
001 1989988
005 2015-02-18
008 2014 bl uuuu u00u1 u #d
100 1 $aRACHWAL, M. F. G.
245 $aMethane fluxes from waterlogged and drained histosols of highland areas.$h[electronic resource]
260 $c2014
520 $aSoil can be either source or sink of methane (CH4), depending on the balance between methanogenesis and methanotrophy, which are determined by pedological, climatic and management factors. The objective of this study was to assess the impact of drainage of a highland Haplic Histosol on CH4 fluxes. Field research was carried out in Ponta Grossa (Paraná, Brazil) based on the measurement of CH4 fluxes by the static chamber method in natural and drained Histosol, over one year (17 sampling events). The natural Histosol showed net CH4 eflux, with rates varying from 238 ?g m-2 h-1 CH4, in cool/cold periods, to 2,850 ?g m-2 h-1 CH4, in warm/hot periods, resulting a cumulative emission of 116 kg ha-1 yr-1 CH4. In the opposite, the drained Histosol showed net influx of CH4 (-39 to -146 ?g m-2 h-1), which resulted in a net consumption of 9 kg ha-1 yr-1 CH4. The main driving factors of CH4 consumption in the drained soil were the lowering of the water-table (on average -57 cm, vs -7 cm in natural soil) and the lower water content in the 0-10 cm layer (average of 5.5 kg kg-1, vs 9.9 kg kg-1 in natural soil). Although waterlogged Histosols of highland areas are regarded as CH4 sources, they fulfill fundamental functions in the ecosystem, such as the accumulation of organic carbon (581 Mg ha-1 C to a depth of 1 m) and water (8.6 million L ha-1 = 860 mm to a depth of 1 m). For this reason, these soils must not be drained as an alternative to mitigate CH4 emission, but effectively preserved.
650 $aÁgua
653 $aGases de efeito estufa
653 $aNível freático
653 $aPrecipitação pluviométrica
653 $aTemperatura do ar
653 $aUmidade gravimétrica
700 1 $aZANATTA, J. A.
700 1 $aDIECKOW, J.
700 1 $aDENEGA, G. L.
700 1 $aCURCIO, G. R.
700 1 $aBAYER, C.
773 $tRevista Brasileira de Ciência do Solo$gv. 38, p. 486-494, 2014.
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Embrapa Florestas (CNPF) |
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| 1. |  | BARTHÈS, B. G.; KOUAKOUA, E.; LARRÉ-LARROUY, M.-C.; RAZAFIMBELO, T. M.; LUCA, E. F. de; AZONTONDE, A.; NEVES, C. S. V. J.; FREITAS, P. L. de; FELLER, C. L. Texture and sesquioxide effects on water-stable aggregates and organic matter in some tropical soils. Geoderma, Amsterdam, v. 143, n. 1/2, p. 14-25, Jan. 2008.| Tipo: Artigo em Periódico Indexado | Circulação/Nível: Internacional - A |
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