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Greenhouse gas fluxes from an Australian subtropical cropland under long-term contrasting management regimes

机译:在长期对比管理制度下,澳大利亚亚热带农田的温室气体通量

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The long-term effects of conservation management practices on greenhouse gas fluxes from tropical/subtropical croplands remain to be uncertain. Using both manual and automatic sampling chambers, we measured N2O and CH4 fluxes at a long-term experimental site (1968-present) in Queensland, Australia from 2006 to 2009. Annual net greenhouse gas fluxes (NGGF) were calculated from the 3-year mean N2O and CH4 fluxes and the long-term soil organic carbon changes. N2O emissions exhibited clear daily, seasonal and interannual variations, highlighting the importance of whole-year measurement over multiple years for obtaining temporally representative annual emissions. Averaged over 3 years, annual N2O emissions from the unfertilized and fertilized soils (90 kg N ha(-1) yr(-1) as urea) amounted to 138 and 902 g N ha(-1), respectively. The average annual N2O emissions from the fertilized soil were 388 g N ha(-1) lower under no-till (NT) than under conventional tillage (CT) and 259 g N ha(-1) higher under stubble retention (SR) than under stubble burning (SB). Annual N2O emissions from the unfertilized soil were similar between the contrasting tillage and stubble management practices. The average emission factors of fertilizer N were 0.91%, 1.20%, 0.52% and 0.77% for the CT-SB, CT-SR, NT-SB and NT-SR treatments, respectively. Annual CH4 fluxes from the soil were very small (-200-300 g CH4 ha(-1) yr(-1)) with no significant difference between treatments. The NGGF were 277-350 kg CO2-e ha(-1) yr(-1) for the unfertilized treatments and 401-710 kg CO2-e ha(-1) yr(-1) for the fertilized treatments. Among the fertilized treatments, N2O emissions accounted for 52-97% of NGGF and NT-SR resulted in the lowest NGGF (401 kg CO2-e ha(-1) yr(-1) or 140 kg CO2-e t(-1) grain). Therefore, NT-SR with improved N fertilizer management practices was considered the most promising management regime for simultaneously achieving maximal yield and minimal NGGF.
机译:养护管理措施对热带/亚热带农田温室气体通量的长期影响尚不确定。使用手动和自动采样室,我们从2006年至2009年在澳大利亚昆士兰州的一个长期实验站点(1968年至今)中测量了N2O和CH4通量。从3年中计算出年净温室气体通量(NGGF)。 N2O和CH4的平均通量以及土壤中长期有机碳的变化。 N2O排放表现出明显的每日,季节性和年际变化,突显了多年进行全年测量对于获得具有时间代表性的年度排放的重要性。从三年平均来看,未施肥和施肥的土壤(尿素为90 kg N ha(-1)yr(-1))的年N2O排放分别为138 g和902 g N ha(-1)。免耕(NT)下施肥土壤的年均N2O排放量比常规耕作(CT)下低388 g N ha(-1),而茬茬(SR)下的残茬高出259 g N ha(-1)残茬燃烧(SB)。在不同的耕作和茬茬管理实践之间,未施肥土壤的年度N2O排放量相似。 CT-SB,CT-SR,NT-SB和NT-SR处理的肥料氮素平均排放因子分别为0.91%,1.20%,0.52%和0.77%。来自土壤的年CH4通量很小(-200-300 g CH4 ha(-1)yr(-1)),两次处理之间无显着差异。 NGGF对于未受精处理为277-350 kg CO2-e ha(-1)yr(-1),对于受精处理为401-710 kg CO2-e ha(-1)yr(-1)。在施肥处理中,N2O排放占NGGF的52-97%,而NT-SR导致NGGF最低(401 kg CO2-e ha(-1)yr(-1)或140 kg CO2-e t(-1 )。因此,具有改良氮肥管理实践的NT-SR被认为是同时实现最大产量和最小NGGF的最有前途的管理制度。

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