Global warming induced by increasing greenhouse gas concentrations in the atmosphere is a matter of great environmental concern. Nitrous oxide (N 2 O) is an important long-living greenhouse gas that has attracted considerable attention during the past few decades because of its contribution to global warming and ozone depletion [1][2][3] Water management has been recognized as one of the most important practices affecting N 2 O emissions [6][7]. Many researchers have found that peak N 2 O emissions were observed during the drying period after soil watering, caused either by precipitation or irrigation. For instance, Ding [8] found that rainfall and irrigation typically enhance soil N 2 O peak emissions from maize-wheat rotation soils. Yao et al. [9] showed that pulse emissions of N 2 O occurred during repeated drying and wetting cycles in rice-wheat rotation systems. Peng et al. [10] reported that maximum N 2 O emissions were measured eight days after irrigation and applying base fertilizer in winter wheat croplands.In addition, some previous studies have confirmed that the peak N 2 O emissions can be observed in a specific water-filled pore space (WFPS) range. In a field trial, Pol. J. Environ. Stud. Vol. 25, No. 6 (2016), 2623-2631
AbstractTo reveal the impact of vertical non-uniform distribution of soil moisture on nitrous oxide (N 2 O) emissions, incubated experiments were conducted from April to August 2013 on silty clay and sandy loam with four watering regimes [surface watering (SW) and subsurface watering application to levels 12, 15, and 18 cm below soil surface (SUW12, SUW15, SUW18)]. Short-term pulse emissions of N 2 O from both soils during the drying process were observed. The soil water-filled pore space (WFPS) at 0-12 cm depths for peak N 2 O fluxes in SW and SUW soils fell within 34-66%, 22-72%, 25-35%, and 19-39% for silty clay and sandy loam, respectively. Our results also suggest that the N 2 O fluxes from soil of sily clay with higher N content are much higher than that from sandy loam, and N 2 O were more easily influenced by soil moisture in SW soils than in SUW soils. However, more research is needed to identify an ideal soil-wetting pattern and the way to realize the ideal soil-wetting pattern, especially on soil with plant growth and fertilization.