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1. | | SORDI, A.; DIECKOW, J.; PIVA, J. T.; ALBUQUERQUE, M. A.; BAYER, C.; TOMAZI, M. Emissão de óxido nitroso a partir de urina e esterco de bovinos em pastagem. In: CONGRESSO BRASILEIRO DE CIÊNCIA DO SOLO, 33., 2011, Uberlândia. Solos nos biomas brasileiros: sustentabilidade e mudanças climáticas: anais. [Uberlândia]: SBCS: UFU, ICIAG, 2011. 1 CD-ROM. Biblioteca(s): Embrapa Agropecuária Oeste. |
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2. | | PIVA, J. T.; DIECKOW, J.; BAYER, C.; PAULETTI, V.; ZANATTA, J. A.; MORAES, A. Emissão de CO2, N2O E CH4 de um latossolo manejado sob integração lavoura-pecuária e plantio direto. In: CONGRESSO BRASILEIRO DE CIÊNCIA DO SOLO, 32., 2009, Fortaleza. O solo e a produção de bioenergia: perspectivas e desafios. Viçosa, MG: Sociedade Brasileira de Ciência do Solo; Fortaleza: UFC, 2009. 1 CD-ROM. Trabalho publicado também em Resumos do CONGRESSO BRASILEIRO DE CIÊNCIA DO SOLO, 32., 2009, Fortaleza. Biblioteca(s): Embrapa Agropecuária Oeste. |
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4. | | BRATTI, F.; RIBEIRO, R. H.; ZANATTA, J. A.; PIVA, J. T.; BAYER, C.; DIECKOW, J. Uso do nabo forrageiro como estratégia para mitigar as emissões de n2o em pastagens de aveia preta no subtrópico brasileiro. In: SIMPÓSIO BRASILEIRO DE AGROPECUÁRIA SUSTENTÁVEL, 10.; CONGRESSO INTERNACIONAL DE AGROPECUÁRIA SUSTENTÁVEL, 7., 2020, Viçosa, MG. Anais... Viçosa, MG: Universidade Federal de Viçosa, 2020. p. 351-354. SIMBRAS. Biblioteca(s): Embrapa Florestas. |
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5. | | PERGHER, M.; PIVA, J. T.; PORFIRIO-DA-SILVA, V.; MORAES, A. de; DIECKOW, J.; PONTES, L. da S. Atributos físicos de solo manejado em sistemas integrados de produção. In: REUNIÃO PARANAENSE DE CIÊNCIA DO SOLO, 2., 2011, Curitiba. Resumos. Curitiba: Universidade Federal do Paraná; Sociedade Paranaense de Ciência do Solo, 2011. p. 50. Biblioteca(s): Embrapa Florestas. |
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6. | | ROCHA, K. F.; CASSOL, L. C.; PIVA, J. T.; ARRUDA, J. H.; MINATO, E. A.; FAVERSANI, J. C. Épocas de aplicação de nitrogênio na cultura do milho num Latossolo Vermelho muito argiloso sob plantio direto. Revista Brasileira de Milho e Sorgo, Sete Lagoas, v. 13, n. 3, p. 273-284, 2014. Biblioteca(s): Embrapa Milho e Sorgo. |
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7. | | PIVA, J. T.; DIECKOW, J.; BAYER, C.; ZANATTA, J. A.; MORAES, A. de; PAULETTI, V.; TOMAZI, M.; PERGHER, M. No-till reduces global warming potential in a subtropical Ferralsol. Plant and Soil, v. 361, p. 359-373, 2012. Biblioteca(s): Embrapa Florestas. |
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8. | | RAMALHO, B.; ALBUQUERQUE, M. A.; DIECKOW, J.; BAYER, C.; PIVA, J. T.; MOLIN, R.; PERGHER, M.; ZANATTA, J. A.; ROSA, C. M. da. Emissão de N2O em Latossolo sob sistemas de culturas com gramíneas e leguminosas. In: REUNIÃO BRASILEIRA DE MANEJO E CONSERVAÇÃO DO SOLO E DA ÁGUA, 19., 2012, Lages. Conservação do solo e da água no Brasil: preceitos e ações no ensino, na pesquisa e na extensão: anais. s.l.: SBCS, 2012. 1 CD-ROM. 4 p. Biblioteca(s): Embrapa Florestas. |
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9. | | PIVA, J. T.; MORAES, A. de; DIECKOW, J.; PORFIRIO-DA-SILVA, V.; BAYER, C.; PONTES, L. da S.; SORDI, A.; ALBUQUERQUE, M. A.; PERGHER, M. Fluxo de CO2, CH4 e N2O do solo em sistemas integrados (lavoura, pecuária e floresta) nos Campos Gerais do Paraná. In: REUNIÃO PARANAENSE DE CIÊNCIA DO SOLO, 2., 2011, Curitiba. Resumos. Curitiba: Universidade Federal do Paraná; Sociedade Paranaense de Ciência do Solo, 2011. p. 19. Biblioteca(s): Embrapa Florestas. |
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10. | | SORDI, A.; DIECKOW, J.; BAYER, C.; ALBUQUERQUE, M. A.; PIVA, J. T.; ZANATTA, J. A.; TOMAZI, M.; ROSA, C. M. da; MORAES, A. de. Nitrous oxide emission factors for urine and dung patchesin a subtropical Brazilian pastureland. Agriculture, Ecosystems and Environment, v. 190, p. 94-103, 2014. Biblioteca(s): Embrapa Florestas. |
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11. | | SORDI, A.; DIECKOW, J.; BAYER, C.; ALBUQUERQUE, M. A.; PIVA, J. T.; ZANATTA, J. A.; TOMAZI, M.; ROSA, C. M. da; MORAES, A. de. Nitrous oxide emission factors for urine and dung patchesin a subtropical Brazilian pastureland. Agriculture, Ecosystems and Environment, v. 190, p. 94-103, 2014. Biblioteca(s): Embrapa Agropecuária Oeste. |
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12. | | SORDI, A.; DIECKOW, J.; BAYER, C.; ALBURQUERQUE, M. A.; PIVA, J. T.; ZANATTA, J. A.; TOMAZI, M.; ROSA, C. M. da; MORAES, A. de. Nitrous oxide emission factors for urine and dung patches in a subtropical Brazilian pastureland. Agriculture, Ecosystems and Environment, Amsterdan, v. 181, 2013. Biblioteca(s): Embrapa Agropecuária Oeste. |
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13. | | PIVA, J. T.; DIECKOW, J.; BAYER, C.; ZANATTA, J. A.; MORAES, A. de; TOMAZI, M.; PAULETTI, V.; BARTH, G.; PICCOLO, M. de C. Soil gaseous N2O and CH4 emissions and carbon pool due to integrated crop-livestock in a subtropical Ferralsol. Agriculture, Ecosystems and Environment, v. 190, p. 87-93, 2014. Biblioteca(s): Embrapa Agropecuária Oeste; Embrapa Florestas. |
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14. | | MONTEIRO, A. L. G.; SILVA, C. J. A. da; BERNDT, A.; RIBEIRO FILHO, H. M. N.; RUGGIERI, A. C.; BAYER, C.; CARVALHO, P. C. de F.; DEISS, L.; PIVA, J. T.; GENRO, T. C. M. Emissões de gases de efeito estufa (GEE) em sistemas de produção de cordeiros para carne no sul do Brasil. In: SOTTA, E. D.; SAMPAIO, F. G.; COSTA, M. de S. N. (org.). Coletânea de fatores de emissão e remoção de gases de efeito estufa da pecuária brasileira. Brasília, DF: MAPA: SENAR, 2020. p.34-35. Biblioteca(s): Embrapa Pecuária Sudeste; Embrapa Pecuária Sul. |
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15. | | MORAES, A. de; PELISSARI, A.; CARVALHO, P. C. de; ANGHINONI, I.; LUSTOSA, S. B. C. L.; BALBINOT JUNIOR, A. A.; LANG, C. R.; ASSMANN, T. S.; ASSMANN, T. S.; ASSMANN, A.; PIVA, J. T.; SCHUSTER, M. Z.; KUNRATH, T. R.; MARTINS, A. P. Avanços técnico-científicos em SIPA no subtrópico brasileiro. In: CONGRESSO BRASILEIRO DE SISTEMAS INTEGRADOS DE PRODUÇÃO AGROPECUÁRIA, 1.; ENCONTRO DE INTEGRAÇÃO LAVOURA-PECUÁRIA NO SUL DO BRASIL, 4., Pato Branco, 2017, Palestras: intensificação com sustentabilidade. Cascavel: UTFPR, 2017. p. 102-124. ISBN do livro no todo: 978-85-99584-10-1. Biblioteca(s): Embrapa Soja. |
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Registros recuperados : 15 | |
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Registro Completo
Biblioteca(s): |
Embrapa Agropecuária Oeste. |
Data corrente: |
18/12/2014 |
Data da última atualização: |
18/12/2014 |
Tipo da produção científica: |
Artigo em Periódico Indexado |
Circulação/Nível: |
A - 1 |
Autoria: |
SORDI, A.; DIECKOW, J.; BAYER, C.; ALBUQUERQUE, M. A.; PIVA, J. T.; ZANATTA, J. A.; TOMAZI, M.; ROSA, C. M. da; MORAES, A. de. |
Afiliação: |
ANDRÉ SORDI, Programa de Pós-Graduação em Ciência do Solo, UFPR; Jeferson Dieckow, UFPR; Cimélio Bayer, UFRGS; MÁRCIO AMARAL ALBUQUERQUE, Programa de pós-graduação em Ciência do Solo, UFPR; JONATAS THIAGO PIVA, UFSC; JOSILEIA ACORDI ZANATTA, CNPF; MICHELY TOMAZI, CPAO; CARLA MACHADO DA ROSA, UFRGS; Anibal de Moraes, UFPR. |
Título: |
Nitrous oxide emission factors for urine and dung patchesin a subtropical Brazilian pastureland. |
Ano de publicação: |
2014 |
Fonte/Imprenta: |
Agriculture, Ecosystems and Environment, v. 190, p. 94-103, 2014. |
DOI: |
http://dx.doi.org/10.1016/j.agee.2013.09.004 |
Idioma: |
Inglês |
Conteúdo: |
tCattle urine and dung (faeces) patches are nitrous oxide (N2O) sources in pasturelands with impactsin the global N2O budget, but specific information about those emissions are still missing for Braziliansubtropical and tropical regions. We conducted a sequence of 3 field-trials (summer, winter and spring,90 days each) to evaluate the N2O emission and emission factor (EF) after the deposition of 3 volumes ofcattle urine or 3 weights of dung (½, 1 and 1½ time the mean urination volume or defecation weight ofFriesian cows) on a free-drained Cambisol of a subtropical pastureland of Brazil. The N2O emission peaks(3198 g N2O-N m−2h−1after urine in summer was the highest) occurred on average 17 ± 9 days afterapplication (DAA), both for urine and dung, and dropped to the background levels 41 ± 10 DAA of urineand 49 ± 10 DAA of dung. The highest contents of NH4+-N in soil (200?250 mg N kg−1) occurred one dayafter urine application and 10?14 days later for dung (100?200 mg N kg−1). Nitrate peaks occurred from23 to 26 DAA in urine patches (∼40?50 mg N kg−1) and 19?50 DAA in dung patches (∼40?50 mg N kg−1).The N2O emission peaks for urine coincided with soil NH4+-N peak in winter but with soil NO3−-N peakin spring. For dung, the emission peak seemed to be more associated with soil NO3−-N than to NH4+-N,either in winter or spring (inorganic-N was not assessed in summer). It was not possible to concludewhether nitrification or denitrification was the dominant process in N2O production, but it seemed thatboth played relevant roles. The EF for urine, averaged across the seasons, diminished with increments inurine volume, from 0.33% in ½ volume to 0.19% in 1½ volume, possibly because urine percolated deeperinto the soil and proportionally less N remained available for N2O production in the top layer. The EFfor dung was 0.19%, 0.12% and 0.14% for ½, 1 and 1½ weight, respectively, showing no clear trend withincrement in dung weight. The lowest EFs for urine and dung occurred in winter, possibly because oflowest temperatures and soil water-filled pore space. The average EF for dung (0.15%) was lower thanthat of urine (0.26%), because urea-N of urine is more readily available for the hydrolysis than organicN forms of dung. This result suggests that these two excreta should be addressed separately in nationalgreenhouse gases inventories or communications. Our results suggest that the default 2% EF proposed inIPCC Guidelines for cattle excreta are overestimated for subtropical Brazil. MenostCattle urine and dung (faeces) patches are nitrous oxide (N2O) sources in pasturelands with impactsin the global N2O budget, but specific information about those emissions are still missing for Braziliansubtropical and tropical regions. We conducted a sequence of 3 field-trials (summer, winter and spring,90 days each) to evaluate the N2O emission and emission factor (EF) after the deposition of 3 volumes ofcattle urine or 3 weights of dung (½, 1 and 1½ time the mean urination volume or defecation weight ofFriesian cows) on a free-drained Cambisol of a subtropical pastureland of Brazil. The N2O emission peaks(3198 g N2O-N m−2h−1after urine in summer was the highest) occurred on average 17 ± 9 days afterapplication (DAA), both for urine and dung, and dropped to the background levels 41 ± 10 DAA of urineand 49 ± 10 DAA of dung. The highest contents of NH4+-N in soil (200?250 mg N kg−1) occurred one dayafter urine application and 10?14 days later for dung (100?200 mg N kg−1). Nitrate peaks occurred from23 to 26 DAA in urine patches (∼40?50 mg N kg−1) and 19?50 DAA in dung patches (∼40?50 mg N kg−1).The N2O emission peaks for urine coincided with soil NH4+-N peak in winter but with soil NO3−-N peakin spring. For dung, the emission peak seemed to be more associated with soil NO3−-N than to NH4+-N,either in winter or spring (inorganic-N was not assessed in summer). It was not possible to concludewhether nitrification or d... Mostrar Tudo |
Palavras-Chave: |
Fator de emissão; Óxido nitroso; Volume de urina. |
Thesagro: |
Gado; Nitrato; Pastagem. |
Categoria do assunto: |
-- |
Marc: |
LEADER 03449naa a2200301 a 4500 001 2003235 005 2014-12-18 008 2014 bl --- 0-- u #d 024 7 $ahttp://dx.doi.org/10.1016/j.agee.2013.09.004$2DOI 100 1 $aSORDI, A. 245 $aNitrous oxide emission factors for urine and dung patchesin a subtropical Brazilian pastureland.$h[electronic resource] 260 $c2014 520 $atCattle urine and dung (faeces) patches are nitrous oxide (N2O) sources in pasturelands with impactsin the global N2O budget, but specific information about those emissions are still missing for Braziliansubtropical and tropical regions. We conducted a sequence of 3 field-trials (summer, winter and spring,90 days each) to evaluate the N2O emission and emission factor (EF) after the deposition of 3 volumes ofcattle urine or 3 weights of dung (½, 1 and 1½ time the mean urination volume or defecation weight ofFriesian cows) on a free-drained Cambisol of a subtropical pastureland of Brazil. The N2O emission peaks(3198 g N2O-N m−2h−1after urine in summer was the highest) occurred on average 17 ± 9 days afterapplication (DAA), both for urine and dung, and dropped to the background levels 41 ± 10 DAA of urineand 49 ± 10 DAA of dung. The highest contents of NH4+-N in soil (200?250 mg N kg−1) occurred one dayafter urine application and 10?14 days later for dung (100?200 mg N kg−1). Nitrate peaks occurred from23 to 26 DAA in urine patches (∼40?50 mg N kg−1) and 19?50 DAA in dung patches (∼40?50 mg N kg−1).The N2O emission peaks for urine coincided with soil NH4+-N peak in winter but with soil NO3−-N peakin spring. For dung, the emission peak seemed to be more associated with soil NO3−-N than to NH4+-N,either in winter or spring (inorganic-N was not assessed in summer). It was not possible to concludewhether nitrification or denitrification was the dominant process in N2O production, but it seemed thatboth played relevant roles. The EF for urine, averaged across the seasons, diminished with increments inurine volume, from 0.33% in ½ volume to 0.19% in 1½ volume, possibly because urine percolated deeperinto the soil and proportionally less N remained available for N2O production in the top layer. The EFfor dung was 0.19%, 0.12% and 0.14% for ½, 1 and 1½ weight, respectively, showing no clear trend withincrement in dung weight. The lowest EFs for urine and dung occurred in winter, possibly because oflowest temperatures and soil water-filled pore space. The average EF for dung (0.15%) was lower thanthat of urine (0.26%), because urea-N of urine is more readily available for the hydrolysis than organicN forms of dung. This result suggests that these two excreta should be addressed separately in nationalgreenhouse gases inventories or communications. Our results suggest that the default 2% EF proposed inIPCC Guidelines for cattle excreta are overestimated for subtropical Brazil. 650 $aGado 650 $aNitrato 650 $aPastagem 653 $aFator de emissão 653 $aÓxido nitroso 653 $aVolume de urina 700 1 $aDIECKOW, J. 700 1 $aBAYER, C. 700 1 $aALBUQUERQUE, M. A. 700 1 $aPIVA, J. T. 700 1 $aZANATTA, J. A. 700 1 $aTOMAZI, M. 700 1 $aROSA, C. M. da 700 1 $aMORAES, A. de 773 $tAgriculture, Ecosystems and Environment$gv. 190, p. 94-103, 2014.
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