2008
DOI: 10.1590/s0103-84782008000700041
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Variação diária da emissão de metano em solo cultivado com arroz irrigado no Sul do Brasil

Abstract: 2049Variação diária da emissão de metano em solo cultivado com arroz irrigado no Sul do Brasil .

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Cited by 17 publications
(10 citation statements)
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“…These values are near to the range of 50 to 130kJ mol -1 reported by Neue & SASS (1994). COSTA et al (2008) reported Ea values in the range of 59 to 341kJ mol -1 in a conventional planting system in South of Table 1 -Average and ranges of air, water and soil temperatures at 2 cm, 5 cm and 10 cm of depth, and average methane emission rates observed in the 24h-campaigns in three growing seasons of flood-irrigated rice cropping, calculated by a curve fit to local regression model. The error corresponds to 95% confidence interval of the adjusted curve.…”
Section: Correlation Between Parameters and Ch 4 Emissionssupporting
confidence: 73%
See 1 more Smart Citation
“…These values are near to the range of 50 to 130kJ mol -1 reported by Neue & SASS (1994). COSTA et al (2008) reported Ea values in the range of 59 to 341kJ mol -1 in a conventional planting system in South of Table 1 -Average and ranges of air, water and soil temperatures at 2 cm, 5 cm and 10 cm of depth, and average methane emission rates observed in the 24h-campaigns in three growing seasons of flood-irrigated rice cropping, calculated by a curve fit to local regression model. The error corresponds to 95% confidence interval of the adjusted curve.…”
Section: Correlation Between Parameters and Ch 4 Emissionssupporting
confidence: 73%
“…In order to optimize efforts for gas measurements it is important to know the time representing the average daily emission for a given producing area, as well as the influence of some key environmental parameters associated with the emission fluxes, for example, soil, air and water temperatures. A number of studies reported positive correlations between CH 4 diurnal emission variations and soil temperature in paddy fields under different climate conditions (SCHüTz et al, 1990;YagI & MINaMI, 1990;SASS et al, 1991;COSTA et al, 2008). WANG et al (1997) argued that diel patterns of CH 4 emissions are determined by the interaction of the soil temperature and the partial pressure of CH 4 .…”
Section: Introductionmentioning
confidence: 99%
“…Each chamber top had a rubber septum sampling port, a stainless steel thermometer, and three battery operated fans to circulate and homogenize air within the chamber (Banker et al, 1995). Chamber closing and initial air sampling started at 9:00 am and were followed by five air samplings 5 min apart (Costa et al, 2008;Minamikawa et al, 2012). Air was drawn with polypropylene syringes, brought to the Laboratory of Soils and Biogeochemistry at UFRGS and analyzed for CH 4 and N 2 O concentrations on the same day with a Shimadzu (Shimadzu Corp.) gas chromatographer.…”
Section: Ghg Measurementsmentioning
confidence: 99%
“…The flux rate of GHG from air sampling at 9:00 am were assumed to be equivalent to mean daily flux rate (Costa et al, 2008). Gas production rate was subsequently converted to kg CH 4 ha À1 d À1 and g N 2 O ha À1 d À1 .…”
Section: Calculationsmentioning
confidence: 99%
“…A quantidade de N 2 O produzido em sistemas agrícolas é determinada pela disponibilidade de NO 3 - (Bouwman, 1996;Brown et al, 2000;Maggiotto et al, 2000), temperatura (Castaldi, 2000), pH (Daum & Schenk, 1998;Mogge et al, 1999), umidade (Zheng et al, 2000;Dobbie & Smith, 2003), além do material orgânico prontamente decomponível e das condições limitantes de difusão de O 2 (Mosier et al, 1991 Nesse contexto, o crescimento do setor agropecuário com a conversão da vegetação nativa em diferentes formas de uso da terra, é necessário conhecer as fontes emissoras dos GEE a fim de colaborar com um diagnóstico mais exato para as tomadas de decisões mitigadoras do aquecimento global. Contudo, a maioria dos estudos envolvendo o fluxo desses gases do solo para a atmosfera estão concentrados na região Sul do Brasil, comparando sistemas de cultivos (La Scala Junior et al, 2001;Costa et al, 2008a;Jantaia et al, 2008;Barreto et al, 2009;Gomes et al, 2009;Siqueira Neto et al, 2009;Escobar et al, 2010) e o fluxo de CH 4 em cultivos de arroz irrigado por inundação (Agostinetto et al, 2002;Costa et al, 2008b), assim como na Amazônia, comparando a transição floresta-pastagem (Steudler et al, 1996;Mellilo et al, 2001;Garcia-Montiel et al, 2002;Fernandes et al, 2002;Passianoto et al, 2003;Carmo et al, 2005;Neill et al, 2005;Wick et al, 2005).…”
Section: Introductionunclassified