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Registro Completo |
Biblioteca(s): |
Embrapa Cerrados. |
Data corrente: |
08/06/2009 |
Data da última atualização: |
24/02/2010 |
Tipo da produção científica: |
Artigo em Periódico Indexado |
Autoria: |
RODRIGUES, L. N.; RAMOS, A. E.; SCHAEDLER, H. A. R.; LOPES, A. V.; FIGUEIREDO, G. C. de. |
Afiliação: |
Lineu Neiva Rodrigues, CPAC; Alba Evangelista Ramos; Hugo Américo Rubert Schaedler, Ibama; Alan Vaz Lopes, ANA; Gilberto Cotta de Figueiredo. |
Título: |
Aspectos legais a serem considerados na construção de pequenas barragens. |
Ano de publicação: |
2008 |
Fonte/Imprenta: |
Item, Brasília, v. 80, p.53-55, 2008. |
Idioma: |
Português |
Conteúdo: |
Barragens ou reservatórios de água são infraestruturas adequadas para situações hidrológicas onde a disponibilidade hídrica é muito variável durante o ano, como é observado, por exemplo, no Cerrado brasileiro. Nesta região, o volume de água dos rios durante a estação chuvosa é maior do que a demanda de água, podendo o excesso ser armazenado para suprir o déficit hídrico durante a seca, quando a demanda é geralmente, maior que a oferta. |
Thesagro: |
Barragem; Reservatório de Água. |
Categoria do assunto: |
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Marc: |
LEADER 00993naa a2200193 a 4500 001 1558194 005 2010-02-24 008 2008 bl --- 0-- u #d 100 1 $aRODRIGUES, L. N. 245 $aAspectos legais a serem considerados na construção de pequenas barragens. 260 $c2008 520 $aBarragens ou reservatórios de água são infraestruturas adequadas para situações hidrológicas onde a disponibilidade hídrica é muito variável durante o ano, como é observado, por exemplo, no Cerrado brasileiro. Nesta região, o volume de água dos rios durante a estação chuvosa é maior do que a demanda de água, podendo o excesso ser armazenado para suprir o déficit hídrico durante a seca, quando a demanda é geralmente, maior que a oferta. 650 $aBarragem 650 $aReservatório de Água 700 1 $aRAMOS, A. E. 700 1 $aSCHAEDLER, H. A. R. 700 1 $aLOPES, A. V. 700 1 $aFIGUEIREDO, G. C. de 773 $tItem, Brasília$gv. 80, p.53-55, 2008.
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Embrapa Cerrados (CPAC) |
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Registro Completo
Biblioteca(s): |
Embrapa Florestas. |
Data corrente: |
17/08/2012 |
Data da última atualização: |
20/02/2015 |
Tipo da produção científica: |
Artigo em Periódico Indexado |
Circulação/Nível: |
A - 1 |
Autoria: |
BAYER, C.; GOMES, J.; VIEIRA, F. C. B; ZANATTA, J. A.; PICCOLO, M. de C.; DIECKOW, J. |
Afiliação: |
CIMÉLIO BAYER, UFRGS; JULIANA GOMES, UFRGS; FREDERICO COSTA BEBER VIEIRA, UNIVERSIDADE FEDERAL DO PAMPA; JOSILEIA ACORDI ZANATTA, CNPF; MARISA DE CÁSSIA PICOLLO, CENTRO DE ENERGIA NUCLEAR DA AGRICULTURA; JEFERSON DIECKOW, UFPR. |
Título: |
Methane emission from soil under long-term no-till cropping systems. |
Ano de publicação: |
2012 |
Fonte/Imprenta: |
Soil & Tillage Research, v. 124, p. 1-7, 2012. |
Idioma: |
Inglês |
Conteúdo: |
Methane (CH4) emission from agricultural soils increases dramatically as a result of deleterious effect of soil disturbance and nitrogen fertilization on methanotrophic organisms; however, few studies have attempted to evaluate the potential of long-term conservation management systems to mitigate CH4 emissions in tropical and subtropical soils. This study aimed to evaluate the long-term effect (>19 years) of no-till grass- and legume-based cropping systems on annual soil CH4 fluxes in a formerly degraded Acrisol in Southern Brazil. Air sampling was carried out using static chambers and CH4 analysis by gas chromatography. Analysis of historical data set of the experiment evidenced a remarkable effect of high C- and N-input cropping systems on the improvement of biological, chemical, and physical characteristics of this no-tilled soil. Soil CH4 fluxes, which represent a net balance between consumption () and production (+) of CH4 in soil, varied from 40 2 to +62 78 mg C m2 h1. Mean weighted contents of ammonium (NH4+–N) and dissolved organic carbon (DOC) in soil had a positive relationship with accumulated soil CH4 fluxes in the post-management period (r2 = 0.95, p = 0.05), suggesting an additive effect of these nutrients in suppressing CH4 oxidation and stimulating methanogenesis, respectively, in legumebased cropping systems with high biomass input. Annual CH4 fluxes ranged from 50 610 to +994 105 g C ha1, which were inversely related to annual biomass-C input (r2 = 0.99, p = 0.003), with the exception of the cropping system containing pigeon pea, a summer legume that had the highest biologically fixed N input (>300 kg ha1 yr1). Our results evidenced a small effect of conservation management systems on decreasing CH4 emissions from soil, despite their significant effect restoring soil quality. We hypothesized that soil CH4 uptake strength has been off-set by an injurious effect of biologically fixed N in legume-based cropping systems on soil methanotrophic microbiota, and by the methanogenesis increase as a result of the O2 depletion in niches of high biological activity in the surface layer of the no-tillage soil. MenosMethane (CH4) emission from agricultural soils increases dramatically as a result of deleterious effect of soil disturbance and nitrogen fertilization on methanotrophic organisms; however, few studies have attempted to evaluate the potential of long-term conservation management systems to mitigate CH4 emissions in tropical and subtropical soils. This study aimed to evaluate the long-term effect (>19 years) of no-till grass- and legume-based cropping systems on annual soil CH4 fluxes in a formerly degraded Acrisol in Southern Brazil. Air sampling was carried out using static chambers and CH4 analysis by gas chromatography. Analysis of historical data set of the experiment evidenced a remarkable effect of high C- and N-input cropping systems on the improvement of biological, chemical, and physical characteristics of this no-tilled soil. Soil CH4 fluxes, which represent a net balance between consumption () and production (+) of CH4 in soil, varied from 40 2 to +62 78 mg C m2 h1. Mean weighted contents of ammonium (NH4+–N) and dissolved organic carbon (DOC) in soil had a positive relationship with accumulated soil CH4 fluxes in the post-management period (r2 = 0.95, p = 0.05), suggesting an additive effect of these nutrients in suppressing CH4 oxidation and stimulating methanogenesis, respectively, in legumebased cropping systems with high biomass input. Annual CH4 fluxes ranged from 50 610 to +994 105 g C ha1, which were inversely related to annual biomass-C input (r2 = 0.99, p... Mostrar Tudo |
Palavras-Chave: |
Emissão de gás. |
Thesagro: |
Agricultura; Metano. |
Categoria do assunto: |
-- |
URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/64094/1/Josileia-STR-Methane.pdf
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Marc: |
LEADER 02751naa a2200217 a 4500 001 1931501 005 2015-02-20 008 2012 bl uuuu u00u1 u #d 100 1 $aBAYER, C. 245 $aMethane emission from soil under long-term no-till cropping systems.$h[electronic resource] 260 $c2012 520 $aMethane (CH4) emission from agricultural soils increases dramatically as a result of deleterious effect of soil disturbance and nitrogen fertilization on methanotrophic organisms; however, few studies have attempted to evaluate the potential of long-term conservation management systems to mitigate CH4 emissions in tropical and subtropical soils. This study aimed to evaluate the long-term effect (>19 years) of no-till grass- and legume-based cropping systems on annual soil CH4 fluxes in a formerly degraded Acrisol in Southern Brazil. Air sampling was carried out using static chambers and CH4 analysis by gas chromatography. Analysis of historical data set of the experiment evidenced a remarkable effect of high C- and N-input cropping systems on the improvement of biological, chemical, and physical characteristics of this no-tilled soil. Soil CH4 fluxes, which represent a net balance between consumption () and production (+) of CH4 in soil, varied from 40 2 to +62 78 mg C m2 h1. Mean weighted contents of ammonium (NH4+–N) and dissolved organic carbon (DOC) in soil had a positive relationship with accumulated soil CH4 fluxes in the post-management period (r2 = 0.95, p = 0.05), suggesting an additive effect of these nutrients in suppressing CH4 oxidation and stimulating methanogenesis, respectively, in legumebased cropping systems with high biomass input. Annual CH4 fluxes ranged from 50 610 to +994 105 g C ha1, which were inversely related to annual biomass-C input (r2 = 0.99, p = 0.003), with the exception of the cropping system containing pigeon pea, a summer legume that had the highest biologically fixed N input (>300 kg ha1 yr1). Our results evidenced a small effect of conservation management systems on decreasing CH4 emissions from soil, despite their significant effect restoring soil quality. We hypothesized that soil CH4 uptake strength has been off-set by an injurious effect of biologically fixed N in legume-based cropping systems on soil methanotrophic microbiota, and by the methanogenesis increase as a result of the O2 depletion in niches of high biological activity in the surface layer of the no-tillage soil. 650 $aAgricultura 650 $aMetano 653 $aEmissão de gás 700 1 $aGOMES, J. 700 1 $aVIEIRA, F. C. B 700 1 $aZANATTA, J. A. 700 1 $aPICCOLO, M. de C. 700 1 $aDIECKOW, J. 773 $tSoil & Tillage Research$gv. 124, p. 1-7, 2012.
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