Soil gas fluxes of N2O, CH4 and CO2 beneath Lolium perenne under elevated CO2: The Swiss free air carbon dioxide enrichment experiment

By Phil Ineson, P. Coward, U. Hartwig. Plant and Soil, 2004

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The microbial aspect of climate change (2016, unknown): “(Phillips et al. 2001; Ineson et al. 1998).”
Agroecosystem responses to combinations of elevated CO2, ozone, and global climate change (2003, background): “In ryegrass plots maintained under high N input, elevated CO 2 increased (+27%), the output of N2O following the application of ammonium nitrate, thought to be the consequence of enhanced root-derived available soil C, acting as an energy source for denitrification ( Ineson et al., 1998).”
Potential of legume-based grassland–livestock systems in Europe: a review (2013, background): “Thus, large peaks of N 2 O emissions are measured in grasslands immediately after N-fertilizer applications (Ineson et al. , 1998; Klumpp et al. , 2011).”