Abstract:
To understand the influence of nitrate nitrogen (NO
3--N) application on N
2O emissions from different soil types during the freezing process, a lab-simulated experiment was conducted to investigate N
2O production from black, fluvo-aquic and loess soils receiving different concentrations of NO
3--N:control (0), 80,0 and 500 mg/kg soil. The application of NO
3--N significantly increased N
2O emissions from the black and fluvo-aquic soils (P<0.05). Compared to the control treatment, the application of NO
3--N with 200 mg/kg soil increased N
2O emissions from the black and fluvo-aquic soils by 849% and 676%, respectively. However, N
2O emissions from the 500 mg/kg NO
3--N treatment soil were reduced by 39.3% and 21.2% compared to 200 mg/kg NO
3--N treatment soil in the black and fluvo-aquic soils, respectively. As the freezing proceeded, the N
2O fluxes from the black and fluvo-aquic soils gradually approached zero. Although there was no significant N
2O flux found from the loess soil, N
2O uptake occurred frequently in the soil. Multi-factor variance analysis showed that soil pH and soil C-to-N ratio were the most important factors driving N
2O emissions. The results implied that management strategies aiming to mitigate N
2O emissions from soil should avoid NO
3--N fertilizer application in black and fluvo-aquic soils during late autumn fertilization. Further studies to investigate the comprehensive relationship between N
2O emissions and variable field conditions involving climate, plants and soil conditions would be useful to expand this research.