Emissões de CO2 do solo sob preparo convencional e plantio direto em latossolo vermelho do Rio Grande do Sul

• Ano de defesa: 2008
• Autor(a) principal: Chavez, Luis Fernando
• Tipo de documento: Dissertação
• Tipo de acesso: Acesso aberto
• Idioma: por
• Instituição de defesa: Universidade Federal de Santa Maria; BR; Agronomia; UFSM; Programa de Pós-Graduação em Ciência do Solo
• Palavras-chave em Português: Efluxo de CO2 do solo; Manejo do solo; Temperatura do solo; Umidade do solo; Soil CO2 efflux; Soil management; Soil temperature; Soil moisture; CNPQ::CIENCIAS AGRARIAS::AGRONOMIA
• Link de acesso: http://repositorio.ufsm.br/handle/1/5476

Climatic change is associated with the increase of greenhouse gases (GHG) concentration, including carbon dioxide (CO2). Among the most important strategies to decrease global warming are decrease emissions and increase biological capture of CO2 through carbon sequestration in the ecosystems. Therefore, soils are fundamental to this strategy because depending in its use and management, they could act as a carbon source or sink. A study was conducted in a Rhodic Hapludox, in a long-term (22 years) experiment, to evaluate CO2-C emissions from soil produced by management practices and its dependence on soil temperature and moisture. CO2-C emissions were intensively analysed with two soil cameras, a dynamic camera (Licor-6400-09) fabricated by LI-COR Company and a static camera (PVC camera) during an evaluation period of 30 days. A intensive cropping system were used in both tillage systems. Results suggest that tillage systems produced differences in the CO2-C emission. No-till system had the highest CO2-C efflux from soil, being 22% higher than the conventional tillage. In conventional tillage highest peaks of CO2-C emissions were verified after soil tillage with disk harrow and chisel plow, nevertheless they were of short duration. CO2-C emissions were influenced by variations in soil temperature and moisture. Higher CO2-C emissions from soil in the no-till system were related to higher soil carbon stocks, presence of soybean residues in the surface, higher contents of particulate organic carbon and higher microbial biomass that together with the higher soil moisture compared to conventional tillage explained the higher efflux. The CO2-C efflux in the long-term no-till reflected the higher soil quality in this system. These results suggest that in the long-term no-till system due to high biologic activity and high soil moisture, soybean residues won t increase soil organic matter content.