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Registro Completo |
Biblioteca(s): |
Embrapa Agropecuária Oeste; Embrapa Florestas. |
Data corrente: |
10/11/2014 |
Data da última atualização: |
06/03/2015 |
Tipo da produção científica: |
Artigo em Periódico Indexado |
Autoria: |
PIVA, J. T.; DIECKOW, J.; BAYER, C.; ZANATTA, J. A.; MORAES, A. de; TOMAZI, M.; PAULETTI, V.; BARTH, G.; PICCOLO, M. de C. |
Afiliação: |
JONATAS TIAGO PIVA, UFPR; JEFERSON DIECKOW, UFPR; CIMÉLIO BAYER, UFRGS; JOSILEIA ACORDI ZANATTA, CNPF; ANIBAL DE MORAES, UFPR; MICHELY TOMAZI, UFRGS; VOLNEI PAULETTI, UFPR; GABRIEL BARTH, Fundação ABC para Assistência Técnica Agropecuária; MARISA DE CASSIA PICCOLO, Centro de Energia Nuclear na Agricultura/USP. |
Título: |
Soil gaseous N2O and CH4 emissions and carbon pool due to integrated crop-livestock in a subtropical Ferralsol. |
Ano de publicação: |
2014 |
Fonte/Imprenta: |
Agriculture, Ecosystems and Environment, v. 190, p. 87-93, 2014. |
Idioma: |
Inglês |
Conteúdo: |
We assessed the impact of integrated crop-livestock (CL), with silage maize (Zea mays L.) in summerand grazed annual-ryegrass (Lolium multiflorum Lam.) in winter, and continuous crop (CC), with annual-ryegrass used only as cover-crop, on net greenhouse gas emission from soil (NetGHG-S) in a subtropicalFerralsol of a 3.5-year-old experiment in Brazil. Emissions from animal excreta in CL were estimated.Soil N2O fluxes after N application to maize were higher in CL (max. 181 g N2O-N m−2h−1) than in CC(max. 132 g N2O-N m−2h−1). The cumulative annual N2O emission from soil in CL surpassed that in CCby more than three-times (4.26 vs. 1.26 kg N2O-N ha−1, p < 0.01), possibly because of supplementary Napplication to grazed ryegrass in CL (N was not applied in cover-crop ryegrass of CC) and a certain degreeof soil compaction visually observed in the first few centimetres after grazing. The estimated annual N2Oemission from excreta in CL was 2.35 kg N2O-N ha−1. Cumulative annual CH4emission was not affectedsignificantly (1.65 in CL vs. 1.08 kg CH4-C ha−1in CC, p = 0.27). Soil organic carbon (OC) stocks were notaffected by soil use systems, neither in 0?20-cm (67.88 in CL vs. 67.20 Mg ha−1in CC, p = 0.62) or 0?100-cm (234.74 in CL vs. 234.61 Mg ha−1in CC, p = 0.97). The NetGHG-S was 0.652 Mg CO2-Ceqha−1year−1higher in CL than in CC. Crop-livestock emitted more N2O than CC and no soil OC sequestration occurredto offset that emission. Management of fertiliser- and excreta-N must be focused as a strategy to mitigate NO2 fluxes in CL. MenosWe assessed the impact of integrated crop-livestock (CL), with silage maize (Zea mays L.) in summerand grazed annual-ryegrass (Lolium multiflorum Lam.) in winter, and continuous crop (CC), with annual-ryegrass used only as cover-crop, on net greenhouse gas emission from soil (NetGHG-S) in a subtropicalFerralsol of a 3.5-year-old experiment in Brazil. Emissions from animal excreta in CL were estimated.Soil N2O fluxes after N application to maize were higher in CL (max. 181 g N2O-N m−2h−1) than in CC(max. 132 g N2O-N m−2h−1). The cumulative annual N2O emission from soil in CL surpassed that in CCby more than three-times (4.26 vs. 1.26 kg N2O-N ha−1, p < 0.01), possibly because of supplementary Napplication to grazed ryegrass in CL (N was not applied in cover-crop ryegrass of CC) and a certain degreeof soil compaction visually observed in the first few centimetres after grazing. The estimated annual N2Oemission from excreta in CL was 2.35 kg N2O-N ha−1. Cumulative annual CH4emission was not affectedsignificantly (1.65 in CL vs. 1.08 kg CH4-C ha−1in CC, p = 0.27). Soil organic carbon (OC) stocks were notaffected by soil use systems, neither in 0?20-cm (67.88 in CL vs. 67.20 Mg ha−1in CC, p = 0.62) or 0?100-cm (234.74 in CL vs. 234.61 Mg ha−1in CC, p = 0.97). The NetGHG-S was 0.652 Mg CO2-Ceqha−1year−1higher in CL than in CC. Crop-livestock emitted more N2O than CC and no soil OC sequestration occurredto offset tha... Mostrar Tudo |
Palavras-Chave: |
Aquecimento global; Dairy livestock; Fertilização; Global warming mitigation; Mitigação; Subtropical soil. |
Thesagro: |
Gado; Solo. |
Categoria do assunto: |
-- A Sistemas de Cultivo |
Marc: |
LEADER 02483naa a2200313 a 4500 001 1999593 005 2015-03-06 008 2014 bl uuuu u00u1 u #d 100 1 $aPIVA, J. T. 245 $aSoil gaseous N2O and CH4 emissions and carbon pool due to integrated crop-livestock in a subtropical Ferralsol. 260 $c2014 520 $aWe assessed the impact of integrated crop-livestock (CL), with silage maize (Zea mays L.) in summerand grazed annual-ryegrass (Lolium multiflorum Lam.) in winter, and continuous crop (CC), with annual-ryegrass used only as cover-crop, on net greenhouse gas emission from soil (NetGHG-S) in a subtropicalFerralsol of a 3.5-year-old experiment in Brazil. Emissions from animal excreta in CL were estimated.Soil N2O fluxes after N application to maize were higher in CL (max. 181 g N2O-N m−2h−1) than in CC(max. 132 g N2O-N m−2h−1). The cumulative annual N2O emission from soil in CL surpassed that in CCby more than three-times (4.26 vs. 1.26 kg N2O-N ha−1, p < 0.01), possibly because of supplementary Napplication to grazed ryegrass in CL (N was not applied in cover-crop ryegrass of CC) and a certain degreeof soil compaction visually observed in the first few centimetres after grazing. The estimated annual N2Oemission from excreta in CL was 2.35 kg N2O-N ha−1. Cumulative annual CH4emission was not affectedsignificantly (1.65 in CL vs. 1.08 kg CH4-C ha−1in CC, p = 0.27). Soil organic carbon (OC) stocks were notaffected by soil use systems, neither in 0?20-cm (67.88 in CL vs. 67.20 Mg ha−1in CC, p = 0.62) or 0?100-cm (234.74 in CL vs. 234.61 Mg ha−1in CC, p = 0.97). The NetGHG-S was 0.652 Mg CO2-Ceqha−1year−1higher in CL than in CC. Crop-livestock emitted more N2O than CC and no soil OC sequestration occurredto offset that emission. Management of fertiliser- and excreta-N must be focused as a strategy to mitigate NO2 fluxes in CL. 650 $aGado 650 $aSolo 653 $aAquecimento global 653 $aDairy livestock 653 $aFertilização 653 $aGlobal warming mitigation 653 $aMitigação 653 $aSubtropical soil 700 1 $aDIECKOW, J. 700 1 $aBAYER, C. 700 1 $aZANATTA, J. A. 700 1 $aMORAES, A. de 700 1 $aTOMAZI, M. 700 1 $aPAULETTI, V. 700 1 $aBARTH, G. 700 1 $aPICCOLO, M. de C. 773 $tAgriculture, Ecosystems and Environment$gv. 190, p. 87-93, 2014.
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Embrapa Florestas (CNPF) |
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Registros recuperados : 12 | |
1. |  | CAVIGLIONE, J. H. Zoneamento da pupunha do Estado do Paraná. In: ENCONTRO PARANAENSE SOBRE PALMITOS CULTIVADOS, 1., 2002, Pontal do Paraná. O agronegócio pupunha e palmeira real: anais. Colombo: Embrapa Florestas, 2004. (Embrapa Florestas. Documentos, 105). Editado por Alvaro Figueredo dos Santos. p. 67-73.Biblioteca(s): Embrapa Florestas. |
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2. |  | CURCIO, G. R.; BONNET, A.; CAVIGLIONE, J. H. Levantamento de solos no Subplanalto de Cascavel - PronaSolos, PR. Pesquisa Florestal Brasileira, Colombo, v. 39, (nesp), e201902043, 2019. p. 666. Edição especial dos resumos do IUFRO World Congress, 25., 2019, Curitiba.Tipo: Resumo em Anais de Congresso |
Biblioteca(s): Embrapa Florestas. |
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3. |  | BONNET, A.; CURCIO, G. R.; CAVIGLIONE, J. H. A qualidade das florestas em nascentes do subplanalto de Cascavel, Bacia Hidrográfica Paraná III, Paraná, Brasil. Pesquisa Florestal Brasileira, Colombo, v. 39, (nesp), e201902043, 2019. p. 624. Edição especial dos resumos do IUFRO World Congress, 25., 2019, Curitiba.Tipo: Resumo em Anais de Congresso |
Biblioteca(s): Embrapa Florestas. |
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5. |  | CURCIO, G. R.; BONNET, A.; OLIVEIRA, D. P. de; FERIANI, L. M.; QUEIROZ, L. H. R. de; CAVIGLIONE, J. H. Proposta metodológica para levantamentos interativos de solos e de vegetação no Paraná. Colombo: Embrapa Florestas, 2023. (Embrapa Florestas. Documentos, 387). Selo ODS 2, 6, 12 e 15.Biblioteca(s): Embrapa Florestas. |
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6. |  | BONNET, A.; CURCIO, G. R.; CAVIGLIONE, J. H.; KACHAROUSKI, M.; PETRY, A. L.; DEBRINO, M. A.; BRUSTOLON, R.; KODAMA, A. A vegetação nos aldeamentos indígenas Tekoha Añetete e Tekoha Itamarã, Diamante d’Oeste, Paraná. Colombo: Embrapa Florestas, 2020. 60 p. (Embrapa Florestas. Documentos, 337).Biblioteca(s): Embrapa Florestas. |
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10. |  | CURCIO, G. R.; BONNET, A.; CAVIGLIONE, J. H.; KACHAROUSKI, M.; PETRY, A. L.; DEBRINO, M. A.; BRUSTOLON, R.; FERLIN, D.; WIGO, M.; OLIVEIRA, D. P. de; FERRIANI, L. M. Levantamento semidetalhado e aptidão agrícola dos solos dos aldeamentos indígenas Tekoha Añetete e Tekoha Itamarã, Diamante d'Oeste, Paraná. Colombo: Embrapa Florestas, 2021. 254 p. (Embrapa Florestas. Documentos, 348).Biblioteca(s): Embrapa Florestas. |
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11. |  | HIGA, R. C. V.; WREGE, M. S.; RADIN, B.; BRAGA, H.; CAVIGLIONE, J. H.; BOGNOLA, I.; ROSOT, M. A. D.; GARRASTAZU, M. C.; CARAMORI, P. H.; OLIVEIRA, Y. M. M. de. Zoneamento climático: Pinus taeda no sul do Brasil. Colombo: Embrapa Florestas, 2008. 1 CD-ROM. (Embrapa Florestas. Documentos, 175).Biblioteca(s): Embrapa Florestas. |
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12. |  | SAMUEL-ROSA, A.; DALMOLIN, R. S. D.; GUBIANI, P. I.; OLIVEIRA, S. R. de M.; TEIXEIRA, W. G.; VIANA, J. H. M.; RIBEIRO, E.; TORNQUIST, C. G.; ANJOS, L. H. C. dos; SOUZA, J. J. E. L. de; OTTONI, M. V.; MEDEIROS, P. S. C. de; GRIS, D. J.; ROSIN, N. A.; BUENO, J. M. M.; SANTOS, H. G. dos; WEBER, E. J.; FLORES, C. A.; COSTA, E. M.; OLIVEIRA, R. P. de; FILIPPINI ALBA, J. M.; PEDROSO NETO, J. C.; PEDRON, F. de A.; CAVIGLIONE, J. H.; VALLADARES, G. S.; MIRANDA, C. S. S.; DEMATTÊ, J. A. M.; MARQUES JÚNIOR, J.; SIQUEIRA, D. S.; AQUINO, R. E. de; SILVERO, N. E. Q.; GENÚ, A. M.; BROETTO, T.; CANCIAN, L. C.; MIGUEL, P.; ZALAMENA, J.; DOTTO, A. C.; ALMEIDA, J. A. de; REICHERT.; CURCIO, G. R.; COLLIER, L. S.; CARVALHO JUNIOR, W. de; FONTANA, A.; OLIVEIRA, A. P. de; VOGELMANN, E. S.; MALLMANN, F. J. K.; VASQUES, G. de M.; LEPSCH, I. F.; FINK, J. R.; KER, J. C.; SILVA, L. S. da; FREITAS, P. L. de; BIELUCZYK, B.; TIECHER, T. Bringing together Brazilian soil scientists to share soil data. In: WORLD CONGRESS OF SOIL SCIENCE, 21., 2018, Rio de Janeiro. Soil science: beyond food and fuel: proceedings... Viçosa, MG: SBCS, 2018. v. 1, p. 63-64. WCSS 2018.Tipo: Resumo em Anais de Congresso |
Biblioteca(s): Embrapa Agricultura Digital; Embrapa Florestas; Embrapa Milho e Sorgo; Embrapa Solos. |
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Registros recuperados : 12 | |
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