Organic fertility inputs synergistically increase denitrification‐derived nitrous oxide emissions in agroecosystems
Debasish Saha, Jason P. Kaye, Arnab Bhowmik, Mary Ann Bruns, John M. Wallace, Armen R. Kemanian
Abstract
Abstract Soil fertility in organic agriculture relies on microbial cycling of nutrient inputs from legume cover crops and animal manure. However, large quantities of labile carbon (C) and nitrogen (N) in these amendments may promote the production and emission of nitrous oxide (N 2 O) from soils. Better ecological understanding of the N 2 O emission controls may lead to new management strategies to reduce these emissions. We measured soil N 2 O emission for two growing seasons in four corn–soybean–winter grain rotations with tillage, cover crop, and manure management variations typical of organic agriculture in temperate and humid North America. To identify N 2 O production pathways and mitigation opportunities, we supplemented N 2 O flux measurements with determinations of N 2 O isotopomer composition and microbiological genomic DNA abundances in microplots where we manipulated cover crop and manure additions. The N input from legume‐rich cover crops and manure prior to corn planting made the corn phase the main source of N 2 O emissions, averaging 9.8 kg/ha of N 2 O‐N and representing 80% of the 3‐yr rotations’ total emissions. Nitrous oxide emissions increased sharply when legume cover crop and manure inputs exceeded 1.8 and 4 Mg/ha (dry matter), respectively. Removing the legume aboveground biomass before corn planting to prevent co‐location of fresh biomass and manure decreased N 2 O emissions by 60% during the corn phase. The co‐occurrence of peak N 2 O emission and high carbon dioxide emission suggests that oxygen (O 2 ) consumption likely caused hypoxia and bacterial denitrification. This interpretation is supported by the N 2 O site preference values trending towards denitrification during peak emissions with limited N 2 O reduction, as revealed by the N 2 O δ 15 N and δ 18 O and the decrease in clade I nosZ gene abundance following incorporation of cover crops and manure. Thus, accelerated microbial O 2 consumption seems to be a critical control of N 2 O emissions in systems with large additions of decomposable C and N substrates. Because many agricultural systems rely on combined fertility inputs from legumes and manures, our research suggests that controlling the rate and timing of organic input additions, as well as preventing the co‐location of legume cover crops and manure, could mitigate N 2 O emissions.