- 1DAFNAE Dept., University of Padova, Viale dell’Università 16, Legnaro (PD) 35020, Italy (elysiajade.lewis@phd.unipd.it)
- 2Crop and Soil Sciences Dept., University of Georgia, 120 Carlton St., Athens, GA 30602, USA
- 3Regione Del Veneto, Direzione Agroambiente, Caccia e Pesca, U.O. Agroambiente, Via Torino 110, Mestre (VE), Italy
Agricultural soils are a significant source of nitrous oxide (N2O) emissions, primarily driven by denitrification and nitrification pathways. Recently, emissions appeared to be strictly related to soil structure characteristics, which may also play a substantial role in the emission pathways. Among these characteristics, the extent to which soil compaction impacts N2O emissions is still debated. To investigate this, a three-year lysimeter experiment was conducted to assess N2O emissions under five cultivation systems with four replicates each: bare soil (BS), conventional (CV), conventional + cover crop (CC), conservation with shallow soil compaction (0-25 cm, CA1), and conservation with deep soil compaction (25-45 cm, CA2). Maize and grain sorghum were grown as main crops, fertilized using solid digestate (300 kg N ha-1). Continuous automatic measurements of N2O emissions were collected using a non-steady state through-flow chamber system and an FTIR gas analyzer, capturing up to seven flux measurements for each chamber per day. Daily emissions were split into four periods per year. The relative importance of nitrification and denitrification to the flux of N2O was hinted at by concurrently measuring NOx emissions and the water-filled pore space (WFPS) and soil temperature measured in the 0-30 cm profile. Additionally, 280 soil samples per year were collected in the 30-days post-fertilization from 0-5 cm and 5-15 cm depths for pH analysis and monitoring ammonia and nitrate pool dynamics. A mixed-effects model was used to test sub-daily emissions. The most pronounced N2O emissions were observed during the initial two weeks following fertilization, with maximum observed emissions highest in CC (208 g ha-1 d-1) and lowest in CA2 (53 g ha-1 d-1) for 2023. Notably, CA2 consistently exhibited lower cumulative N2O emissions, suggesting a complex interaction between management practices and soil conditions. These findings highlight the importance of soil structure and cultivation system in managing N2O emissions.
How to cite: Lewis, E., Longo, M., Rocco, S., Dal Ferro, N., Cabrera, M., Lazzaro, B., and Morari, F.: From Fertilizer to Flux: Investigating N2O Emissions in Compacted Cultivation Systems, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-16508, https://doi.org/10.5194/egusphere-egu25-16508, 2025.