摘要

Agricultural soils are primarily responsible for the global anthropogenic nitrous oxide (N2O) emissions due to excessive use of N fertilizers. Along with fertilizer, it may also be excelled by the seasonal precipitation pattern of monsoon climate in Southern China. To estimate N2O emissions of native and agricultural soils in subtropical ecosystem surrounding Three Gorges Dam, a 4 years campaign was started to determine the temporal N2O fluxes from seven sites of four land use types (one vegetable field, three uplands, two orchards and one pine forest). The mean annual budget of N2O emissions was 0.13-5.27 kg N2O-N ha(-1) year(-1). Pine forest had significantly lower N2O emissions than agriculture land uses. Tilled orchard had significantly lower N2O emissions than non-tilled orchard. Generally, among agriculture land uses, maximum N2O emissions were observed from vegetable field followed by orchards and uplands. Among all land uses, N2O emissions were significantly correlated with amount of N fertilizer applied. Every year, the climate was warm and wet from April through September (the hot-humid season) and became cool and dry from October through March (the cool-dry season). N2O fluxes and environmental variables (soil temperature, water-filled pore space (WFPS), soil NO3--N and NH4+-N contents) had significant seasonal variabilities. Driven by seasonality of soil temperature, WFPS, soil NO3--N and NH4+-N contents, N2O fluxes were significantly higher in the hot-humid season than in the cool-dry season. The relationship between N2O fluxes and all the environmental variables were presented in one linear model of variation which explained 72-97% of N2O flux variability among different land uses. We conclude that N2O fluxes from different land uses are strongly under control of different climatic predictors along with soil nutrient status, which interact in conjunction with each other to supply the readily available substrates for the N2O flux from the subtropical soils.