Topography Controls N2O Emissions Differently during Early and Late Corn Growing Season

Topography affects soil hydrological, pedological, and biochemical processes and may influence nitrous oxide (N2O) emissions into the atmosphere. While N2O emissions from agricultural fields are mainly measured at plot scale and on flat topography, intrafield topographical and crop growth variability alter soil processes and might impact N2O emissions. The objective of this study was to examine the impact of topographical variations on crop growth period dependent soil N2O emissions at the field scale. A field experiment was conducted at two agricultural farms (Baggs farm: BF and Research North: RN) with undulating topography. Dominant slope positions (upper, middle, lower and toeslope) were identified based on elevation difference. Soil and gas samples were collected from four replicated locations within each slope position over the whole corn growing season (May&ndash:October 2019) to measure soil physio-chemical properties and N2O emissions. The N2O emissions at BF ranged from &minus:0.27 &plusmn: 0.42 to 255 &plusmn: 105 g ha&minus:1 d&minus:1. Higher cumulative emissions were observed from the upper slope (1040 &plusmn: 487 g ha&minus:1) during early growing season and from the toeslope (371 &plusmn: 157 g ha&minus:1) during the late growing season with limited variations during the mid growing season. Similarly, at RN farm, (emissions ranged from &minus:0.50 &plusmn: 0.83 to 70 &plusmn: 15 g ha&minus:1 d&minus:1), the upper slope had higher cumulative emissions during early (576 &plusmn: 132 g ha&minus:1) and mid (271 &plusmn: 51 g ha&minus:1) growing season, whereas no impact of slope positions was observed during late growing season. Topography controlled soil and environmental properties differently at different crop growth periods: thus, intrafield variability must be considered in estimating N2O emissions and emission factor calculation from agricultural fields. However, due to large spatial variations in N2O emissions, further explorations into site-specific analysis of individual soil properties and their impact on N2O emissions using multiyear data might help to understand and identify hotspots of N2O emissions.