Tese
Estimativas das trocas líquidas de carbono em duas áreas de cultivo de arroz irrigado na região central do RS
Fecha
2012-07-26Registro en:
CARNEIRO, Janaína Viário. Estimates of net carbon exchange in two areas of irrigated rice in the central region of the RS. 2012. 97 f. Tese (Doutorado em Física) - Universidade Federal de Santa Maria, Santa Maria, 2012.
Autor
Carneiro, Janaína Viário
Institución
Resumen
The turbulent fluxes of carbon dioxide (CO2 ) were investigated in two sites of
irrigated rice in southern Brazil, using the eddy covariance technique over 385 days
of analysis at the site of Paraiso do Sul and 683 days in site Cachoeira do Sul also
used the model of filling the gaps in order to estimate the net ecosystem exchange
CO2 -C (NEE). Throughout the growing season, rice fields, both for the site of
Paraiso do Sul to the site of Cachoeira do Sul, acted as carbon sinks (C). During
fallow periods, these fields were the source of C. The NEE accumulated at the site of
Cachoeira do Sul was similar in both cycles and practically equal to the estimated
site of Paraiso do Sul. The GPP accumulated during the crop cycle 2010-2011, the
rice field of Cachoeira do Sul, was less than 12% of the 2011-2012 cycle and higher
than 15% of the site of Paraiso do Sul. The Re accumulated was similar at the site of
Paraíso do Sul in the 2010-2011 cycle Cachoeira do Sul, but less than the 2011-
2012 cycle. The values of NEE, GPP and R e for the site of Paraíso do Sul were -
270.53 gCm2 , -821.19gCm2 and 527.59gCm2 , respectively. To the site of
Cachoeira do Sul, were -282,53 gCm2 , -933,40gCm2 and 597,05gCm2 for NEE,
GPP and Re , respectively, in the 2010-2011 cycle. For the 2011-2012 cycle in the
rice field of Cachoeira do Sul, the values of NEE, GPP and Re were -279,69gCm2 , -
1062,64gCm2 and 716,58gCm2 , respectively. The total C accumulated over the
period analyzed for the site of Paraíso do Sul was -45,90gCm2 , considering this
area of rice cultivation, as a sink for C. While the growing area of Cachoeira do Sul was considered a source of C (19,94 gCm2 ). Showing by this that long periods of
fallow contribute significantly to the accumulated fluxes due to constant presence of
vegetation. The contribution of this work will assist in the investigation of CO2 in
these ecosystems.