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Registro Completo |
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Biblioteca(s): |
Embrapa Florestas. |
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Data corrente: |
08/02/2013 |
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Data da última atualização: |
19/02/2015 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
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Autoria: |
PIVA, J. T.; DIECKOW, J.; BAYER, C.; ZANATTA, J. A.; MORAES, A. de; PAULETTI, V.; TOMAZI, M.; PERGHER, M. |
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Afiliação: |
Jonatas Thiago Piva, UFPR; Jeferson Dieckow, UFPR; Cimélio Bayer, UFRGS; JOSILEIA ACORDI ZANATTA, CNPF; Anibal de Moraes, UFPR; Volnei Pauletti, Fundação ABC para Assistência e Divulgação Técnica Agropecuária; MICHELY TOMAZI, CPAO; Maico Pergher, UFPR. |
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Título: |
No-till reduces global warming potential in a subtropical Ferralsol. |
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Ano de publicação: |
2012 |
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Fonte/Imprenta: |
Plant and Soil, v. 361, p. 359-373, 2012. |
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Idioma: |
Inglês |
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Conteúdo: |
Aims For tropical and subtropical soils, information is scarce regarding the global warming potential (GWP) of no-till (NT) agriculture systems. Soil organic carbon (OC) sequestration is promoted by NT agriculture, but this may be offset by increased nitrous oxide (N2O) emissions. We assessed the GWP of a NT as compared to conventional tillage (CT) in a subtropical Brazilian Ferralsol. Methods From September 2008 to September 2009 we used static chambers and chromatographic analyses to assess N2O and methane (CH4) soil fluxes in an area previously used for 3–4 years as a fieldexperiment. The winter cover crop was ryegrass (Lolium multiflorum Lam.) while in summer it was silage maize (Zea mays L.). Results The accumulated N2O emission for NT was about half that of CT (1.26 vs 2.42 kg N ha?1 year?1, P00.06). Emission peaks for N2O occurred for a month after CT, presumably induced by mineralization of residual nitrogen. In both systems, the highest N2O flux occurred after sidedressing maize with inorganic nitrogen, although the flux was lower in NT than CT (132 vs 367 ?g N m?2 h?1, P00.05), possibly because some of the sidedressed nitrogen was immobilized by ryegrass residues on the surface of the NT soil. Neither water-filled pore space (WFPS) nor inorganic nitrogen (NH4+ and NO3?) correlated with N2O fluxes, although at some specific periods relationships were observed with inorganic nitrogen. Soils subjected to CT or NT both acted as CH4 sinks during most of the experiment, although a CH4 peak in May (autumn) led to overall CH4 emissions of 1.15 kg CH4-C ha?1 year?1 for CT and 1.08 kg CH4-C ha?1 year?1 for NT (P00.90). The OC stock in the 0–20 cm soil layer was slightly higher for NT than for CT (67.20 vs 66.49 Mg ha?1, P00.36). In the 0–100 cm layer, the OC stock was significantly higher for NT as compared to CT (234.61 vs 231.95 Mg ha?1, P00.01), indicating that NT resulted in the sequestration of OC at a rate of 0.76 Mg ha?1 year?1. The CO2 equivalent cost of agronomic practices was similar for CT (1.72 Mg CO2eq ha?1 year?1) andNT(1.62MgCO2eq ha?1 year?1). However, NT reduced the GWP relative to CT (?0.55 vs 2.90 Mg CO2eq ha?1 year?1), with the difference of ?3.45 Mg CO2eq ha?1 year?1 (negative value implies mitigation) being driven mainly by OC sequestration. The greenhouse gas intensity (GHGI, equivalent to GWP/silage yield) was lower for NT than CT (?31.7 vs 171.1 kg CO2eq Mg?1 for silage maize). Conclusion As compared to CT, greenhouse gas emissions from a subtropical soil can be mitigated by NT by lowering N2O emissions and, principally, sequestration of CO2-C. MenosAims For tropical and subtropical soils, information is scarce regarding the global warming potential (GWP) of no-till (NT) agriculture systems. Soil organic carbon (OC) sequestration is promoted by NT agriculture, but this may be offset by increased nitrous oxide (N2O) emissions. We assessed the GWP of a NT as compared to conventional tillage (CT) in a subtropical Brazilian Ferralsol. Methods From September 2008 to September 2009 we used static chambers and chromatographic analyses to assess N2O and methane (CH4) soil fluxes in an area previously used for 3–4 years as a fieldexperiment. The winter cover crop was ryegrass (Lolium multiflorum Lam.) while in summer it was silage maize (Zea mays L.). Results The accumulated N2O emission for NT was about half that of CT (1.26 vs 2.42 kg N ha?1 year?1, P00.06). Emission peaks for N2O occurred for a month after CT, presumably induced by mineralization of residual nitrogen. In both systems, the highest N2O flux occurred after sidedressing maize with inorganic nitrogen, although the flux was lower in NT than CT (132 vs 367 ?g N m?2 h?1, P00.05), possibly because some of the sidedressed nitrogen was immobilized by ryegrass residues on the surface of the NT soil. Neither water-filled pore space (WFPS) nor inorganic nitrogen (NH4+ and NO3?) correlated with N2O fluxes, although at some specific periods relationships were observed with inorganic nitrogen. Soils subjected to CT or NT both acted as CH4 sinks during most of the experiment, ... Mostrar Tudo |
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Palavras-Chave: |
Aquecimento global. |
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Thesagro: |
Plantio Direto; Solo. |
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Categoria do assunto: |
-- |
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Marc: |
LEADER 03261naa a2200241 a 4500
001 1948897
005 2015-02-19
008 2012 bl uuuu u00u1 u #d
100 1 $aPIVA, J. T.
245 $aNo-till reduces global warming potential in a subtropical Ferralsol.$h[electronic resource]
260 $c2012
520 $aAims For tropical and subtropical soils, information is scarce regarding the global warming potential (GWP) of no-till (NT) agriculture systems. Soil organic carbon (OC) sequestration is promoted by NT agriculture, but this may be offset by increased nitrous oxide (N2O) emissions. We assessed the GWP of a NT as compared to conventional tillage (CT) in a subtropical Brazilian Ferralsol. Methods From September 2008 to September 2009 we used static chambers and chromatographic analyses to assess N2O and methane (CH4) soil fluxes in an area previously used for 3–4 years as a fieldexperiment. The winter cover crop was ryegrass (Lolium multiflorum Lam.) while in summer it was silage maize (Zea mays L.). Results The accumulated N2O emission for NT was about half that of CT (1.26 vs 2.42 kg N ha?1 year?1, P00.06). Emission peaks for N2O occurred for a month after CT, presumably induced by mineralization of residual nitrogen. In both systems, the highest N2O flux occurred after sidedressing maize with inorganic nitrogen, although the flux was lower in NT than CT (132 vs 367 ?g N m?2 h?1, P00.05), possibly because some of the sidedressed nitrogen was immobilized by ryegrass residues on the surface of the NT soil. Neither water-filled pore space (WFPS) nor inorganic nitrogen (NH4+ and NO3?) correlated with N2O fluxes, although at some specific periods relationships were observed with inorganic nitrogen. Soils subjected to CT or NT both acted as CH4 sinks during most of the experiment, although a CH4 peak in May (autumn) led to overall CH4 emissions of 1.15 kg CH4-C ha?1 year?1 for CT and 1.08 kg CH4-C ha?1 year?1 for NT (P00.90). The OC stock in the 0–20 cm soil layer was slightly higher for NT than for CT (67.20 vs 66.49 Mg ha?1, P00.36). In the 0–100 cm layer, the OC stock was significantly higher for NT as compared to CT (234.61 vs 231.95 Mg ha?1, P00.01), indicating that NT resulted in the sequestration of OC at a rate of 0.76 Mg ha?1 year?1. The CO2 equivalent cost of agronomic practices was similar for CT (1.72 Mg CO2eq ha?1 year?1) andNT(1.62MgCO2eq ha?1 year?1). However, NT reduced the GWP relative to CT (?0.55 vs 2.90 Mg CO2eq ha?1 year?1), with the difference of ?3.45 Mg CO2eq ha?1 year?1 (negative value implies mitigation) being driven mainly by OC sequestration. The greenhouse gas intensity (GHGI, equivalent to GWP/silage yield) was lower for NT than CT (?31.7 vs 171.1 kg CO2eq Mg?1 for silage maize). Conclusion As compared to CT, greenhouse gas emissions from a subtropical soil can be mitigated by NT by lowering N2O emissions and, principally, sequestration of CO2-C.
650 $aPlantio Direto
650 $aSolo
653 $aAquecimento global
700 1 $aDIECKOW, J.
700 1 $aBAYER, C.
700 1 $aZANATTA, J. A.
700 1 $aMORAES, A. de
700 1 $aPAULETTI, V.
700 1 $aTOMAZI, M.
700 1 $aPERGHER, M.
773 $tPlant and Soil$gv. 361, p. 359-373, 2012.
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Embrapa Florestas (CNPF) |
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Biblioteca(s): |
Embrapa Café. |
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Data corrente: |
13/12/2011 |
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Data da última atualização: |
13/12/2011 |
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Tipo da produção científica: |
Artigo em Anais de Congresso |
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Autoria: |
PEREIRA, S. P.; BARTHOLO, G. F.; GUIMARÃES, P. T. G.; ALVES, J. D.; GUIMARÃES, R. J. |
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Afiliação: |
SÉRGIO PARREIRAS PEREIRA, IAC; GABRIEL FERREIRA BARTHOLO, SAPC; PAULO TÁCITO GONTIJO GUIMARÃES, EPAMIG; JOSÉ DONIZETI ALVES, UFLA; RUBENS JOSÉ GUIMARÃES, UFLA. |
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Título: |
Consequências da redução de espaçamentos entre as linhas e entre as plantas na linha de plantio sobre os componentes vegetativos de cafeeiros (Coffea arabica L.) cultivar Catuaí. |
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Ano de publicação: |
2005 |
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Fonte/Imprenta: |
In: SIMPÓSIO DE PESQUISA DOS CAFÉS DO BRASIL, 4., 2005, Londrina. Anais... Brasília, DF: Embrapa Café, 2005. |
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Idioma: |
Português |
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Conteúdo: |
O experimento foi instalado na Fazenda Experimental da EPAMIG em Machado, sul de Minas Gerais, em 1992, com o objetivo de avaliar as conseqüências da redução de espaçamentos entre as linhas e entre as plantas na linha de plantio sobre a produção e a fenologia do cafeeiro. O delineamento experimental utilizado foi um fatorial 4 x 3 com parcela subdividida, sendo quatro distâncias entre as linhas (2,0? 2,5? 3,0 e 3,5 m) e três distâncias entre as plantas na linha de plantio (0,5? 0,75? 1,0 m), e totalizando 12 tratamentos dispostos em blocos ao acaso em três repetições. Em julho de 2002, logo após a colheita e antes da primeira recepa, foram avaliadas as características relativas à arquitetura dos cafeeiros (altura da planta, diâmetro da copa, altura dos ramos plagiotrópicos baixeiros e diâmetro do caule). O adensamento entre linhas proporciona plantas mais altas, com inserção dos primeiros ramos plagiotrópicos mais altos, menores comprimento e diâmetro da copa. O adensamento entre linhas não afeta o diâmetro do caule. Já o adensamento das plantas na linha de plantio linha proporciona também plantas mais altas e com inserção dos primeiros ramos plagiotrópicos mais altos, não influencia o comprimento da copa e apresenta diâmetros da copa e do caule menores. |
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Palavras-Chave: |
Cafeeiro. |
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Thesagro: |
Arquitetura; Espaçamento. |
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Categoria do assunto: |
-- |
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URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/50093/1/Consequencias-da-reducao.pdf
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Marc: |
LEADER 02041nam a2200193 a 4500
001 1909492
005 2011-12-13
008 2005 bl uuuu u00u1 u #d
100 1 $aPEREIRA, S. P.
245 $aConsequências da redução de espaçamentos entre as linhas e entre as plantas na linha de plantio sobre os componentes vegetativos de cafeeiros (Coffea arabica L.) cultivar Catuaí.$h[electronic resource]
260 $aIn: SIMPÓSIO DE PESQUISA DOS CAFÉS DO BRASIL, 4., 2005, Londrina. Anais... Brasília, DF: Embrapa Café$c2005
520 $aO experimento foi instalado na Fazenda Experimental da EPAMIG em Machado, sul de Minas Gerais, em 1992, com o objetivo de avaliar as conseqüências da redução de espaçamentos entre as linhas e entre as plantas na linha de plantio sobre a produção e a fenologia do cafeeiro. O delineamento experimental utilizado foi um fatorial 4 x 3 com parcela subdividida, sendo quatro distâncias entre as linhas (2,0? 2,5? 3,0 e 3,5 m) e três distâncias entre as plantas na linha de plantio (0,5? 0,75? 1,0 m), e totalizando 12 tratamentos dispostos em blocos ao acaso em três repetições. Em julho de 2002, logo após a colheita e antes da primeira recepa, foram avaliadas as características relativas à arquitetura dos cafeeiros (altura da planta, diâmetro da copa, altura dos ramos plagiotrópicos baixeiros e diâmetro do caule). O adensamento entre linhas proporciona plantas mais altas, com inserção dos primeiros ramos plagiotrópicos mais altos, menores comprimento e diâmetro da copa. O adensamento entre linhas não afeta o diâmetro do caule. Já o adensamento das plantas na linha de plantio linha proporciona também plantas mais altas e com inserção dos primeiros ramos plagiotrópicos mais altos, não influencia o comprimento da copa e apresenta diâmetros da copa e do caule menores.
650 $aArquitetura
650 $aEspaçamento
653 $aCafeeiro
700 1 $aBARTHOLO, G. F.
700 1 $aGUIMARÃES, P. T. G.
700 1 $aALVES, J. D.
700 1 $aGUIMARÃES, R. J.
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