Detalhes bibliográficos
| Ano de defesa: |
2014 |
| Autor(a) principal: |
Corrêa, Rubia Santos
 |
| Orientador(a): |
Madari, Beata Emoke
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| Banca de defesa: |
Madari, Beáta Emoke,
Evangelista , Adão Wagner Pêgo,
Maggiotto, Selma Regina |
| Tipo de documento: |
Dissertação
|
| Tipo de acesso: |
Acesso aberto |
| Idioma: |
por |
| Instituição de defesa: |
Universidade Federal de Goiás
|
| Programa de Pós-Graduação: |
Programa de Pós-graduação em Agronomia (EAEA)
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| Departamento: |
Escola de Agronomia e Engenharia de Alimentos - EAEA (RG)
|
| País: |
Brasil
|
| Palavras-chave em Português: |
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| Palavras-chave em Inglês: |
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| Área do conhecimento CNPq: |
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| Link de acesso: |
http://repositorio.bc.ufg.br/tede/handle/tede/5166
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Resumo: |
Climate changes is of global importance influencing local and international policy decisions. It is important that sectors and human activities that contribute to worsen the global warming scenario are identified. Nitrous oxide (N2O) is an important greenhouse gas, despite its low concentration in the atmosphere this gas stands out due to its long residence time and to potential for absorption of infrared radiation of its molecule and to its hence high of global warming potential. N2O in the atmosphere has the ability to absorb infrared radiation of the earth and increase the average temperature of the planet. As consequences we observe the effects of warming on many environmental disasters, changes in rainfall patterns, melting glaciers and other phenomena caused by climate disorders. The magnitudes of the gas fluxes coming from the farm system are relevant, highlighting the need to identify sources sinks of greenhouse gas emissions (GGE) in agriculture. In Brazil the most commonly used method for measuring the greenhouse gas is the static chamber. It is supposed that with this method the fluxes GGE are underestimated. In this work this hypothesis was tested by comparing the N2O fluxes obtained with manuals static chambers with those obtained by a micrometeorological method, the flux-gradient, and characterizing the dynamics of the flux of N2O in the Integrated Crop-Livestock system (ICL). The study was conducted at Embrapa Rice and Beans, in Santo Antônio de Goiás, in clay Rhodic Ferralsol typical, under ICL system the pasture phase. Initial studies have been made to define sampling times and best time to perform the sampling by the manual static chamber method. The sampling times used were 0, 15 and 30 minutes and the best period for routine sampling was around 10 am. In calculating fluxes, whenever possible the Hutchinson & Mosier function was used. When this function not was applied a simple linear function was used. The flux calculated by the linear function was considered when R2 was greater than or equal to 0.80. The measured fluxes by the two quantification methods manuals static chambers and flux-gradient were comparable, however in 69.77% of the assessed days the values positive obtained by the flux-gradient method were higher than those obtained by the manual static chamber method. As to the physical and chemical attributes of the soil, considering the entire period under study, in pasture soil, it was observed that N2O fluxes were positively correlated with the nitrate concentration, WFPS and the soil temperature. In the rainy season there was a positive correlation between N2O fluxes and WFPS of soil. In the dry season there was a positive correlation between N2O fluxes and the ammonium and nitrate concentrations of soil. During the study not was observed emission of N2O in of reference area, area this formed by a native forest fragment. |
