Methane fluxes from waterlogged and drained histosols of highland areas.

Detalhes bibliográficos
Autor(a) principal: RACHWAL, M. F. G.
Data de Publicação: 2014
Outros Autores: ZANATTA, J. A., DIECKOW, J., DENEGA, G. L., CURCIO, G. R., BAYER, C.
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Repositório Institucional da EMBRAPA (Repository Open Access to Scientific Information from EMBRAPA - Alice)
Texto Completo: http://www.alice.cnptia.embrapa.br/alice/handle/doc/989988
Resumo: 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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spelling Methane fluxes from waterlogged and drained histosols of highland areas.Gases de efeito estufaNível freáticoUmidade gravimétricaTemperatura do arPrecipitação pluviométricaÁguaSoil 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.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.RACHWAL, M. F. G.ZANATTA, J. A.DIECKOW, J.DENEGA, G. L.CURCIO, G. R.BAYER, C.2014-07-07T11:11:11Z2014-07-07T11:11:11Z2014-07-0720142015-02-18T11:11:11Zinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articleRevista Brasileira de Ciência do Solo, v. 38, p. 486-494, 2014.http://www.alice.cnptia.embrapa.br/alice/handle/doc/989988enginfo:eu-repo/semantics/openAccessreponame:Repositório Institucional da EMBRAPA (Repository Open Access to Scientific Information from EMBRAPA - Alice)instname:Empresa Brasileira de Pesquisa Agropecuária (Embrapa)instacron:EMBRAPA2017-08-16T00:43:29Zoai:www.alice.cnptia.embrapa.br:doc/989988Repositório InstitucionalPUBhttps://www.alice.cnptia.embrapa.br/oai/requestopendoar:21542017-08-16T00:43:29falseRepositório InstitucionalPUBhttps://www.alice.cnptia.embrapa.br/oai/requestcg-riaa@embrapa.bropendoar:21542017-08-16T00:43:29Repositório Institucional da EMBRAPA (Repository Open Access to Scientific Information from EMBRAPA - Alice) - Empresa Brasileira de Pesquisa Agropecuária (Embrapa)false
dc.title.none.fl_str_mv Methane fluxes from waterlogged and drained histosols of highland areas.
title Methane fluxes from waterlogged and drained histosols of highland areas.
spellingShingle Methane fluxes from waterlogged and drained histosols of highland areas.
RACHWAL, M. F. G.
Gases de efeito estufa
Nível freático
Umidade gravimétrica
Temperatura do ar
Precipitação pluviométrica
Água
title_short Methane fluxes from waterlogged and drained histosols of highland areas.
title_full Methane fluxes from waterlogged and drained histosols of highland areas.
title_fullStr Methane fluxes from waterlogged and drained histosols of highland areas.
title_full_unstemmed Methane fluxes from waterlogged and drained histosols of highland areas.
title_sort Methane fluxes from waterlogged and drained histosols of highland areas.
author RACHWAL, M. F. G.
author_facet RACHWAL, M. F. G.
ZANATTA, J. A.
DIECKOW, J.
DENEGA, G. L.
CURCIO, G. R.
BAYER, C.
author_role author
author2 ZANATTA, J. A.
DIECKOW, J.
DENEGA, G. L.
CURCIO, G. R.
BAYER, C.
author2_role author
author
author
author
author
dc.contributor.none.fl_str_mv 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.
dc.contributor.author.fl_str_mv RACHWAL, M. F. G.
ZANATTA, J. A.
DIECKOW, J.
DENEGA, G. L.
CURCIO, G. R.
BAYER, C.
dc.subject.por.fl_str_mv Gases de efeito estufa
Nível freático
Umidade gravimétrica
Temperatura do ar
Precipitação pluviométrica
Água
topic Gases de efeito estufa
Nível freático
Umidade gravimétrica
Temperatura do ar
Precipitação pluviométrica
Água
description 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.
publishDate 2014
dc.date.none.fl_str_mv 2014-07-07T11:11:11Z
2014-07-07T11:11:11Z
2014-07-07
2014
2015-02-18T11:11:11Z
dc.type.driver.fl_str_mv info:eu-repo/semantics/publishedVersion
info:eu-repo/semantics/article
format article
status_str publishedVersion
dc.identifier.uri.fl_str_mv Revista Brasileira de Ciência do Solo, v. 38, p. 486-494, 2014.
http://www.alice.cnptia.embrapa.br/alice/handle/doc/989988
identifier_str_mv Revista Brasileira de Ciência do Solo, v. 38, p. 486-494, 2014.
url http://www.alice.cnptia.embrapa.br/alice/handle/doc/989988
dc.language.iso.fl_str_mv eng
language eng
dc.rights.driver.fl_str_mv info:eu-repo/semantics/openAccess
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dc.source.none.fl_str_mv reponame:Repositório Institucional da EMBRAPA (Repository Open Access to Scientific Information from EMBRAPA - Alice)
instname:Empresa Brasileira de Pesquisa Agropecuária (Embrapa)
instacron:EMBRAPA
instname_str Empresa Brasileira de Pesquisa Agropecuária (Embrapa)
instacron_str EMBRAPA
institution EMBRAPA
reponame_str Repositório Institucional da EMBRAPA (Repository Open Access to Scientific Information from EMBRAPA - Alice)
collection Repositório Institucional da EMBRAPA (Repository Open Access to Scientific Information from EMBRAPA - Alice)
repository.name.fl_str_mv Repositório Institucional da EMBRAPA (Repository Open Access to Scientific Information from EMBRAPA - Alice) - Empresa Brasileira de Pesquisa Agropecuária (Embrapa)
repository.mail.fl_str_mv cg-riaa@embrapa.br
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