4.7 Article

Hot spots of N and C impact nitric oxide, nitrous oxide and nitrogen gas emissions from a UK grassland soil

Journal

GEODERMA
Volume 305, Issue -, Pages 336-345

Publisher

ELSEVIER
DOI: 10.1016/j.geoderma.2017.06.007

Keywords

Denitrification; Flow-through system; Isotopes; Nitrogen cycle; Greenhouse gas (GHG) emissions

Categories

Funding

  1. Biotechnology and Biological Sciences Research Council (BBSRC)
  2. BBSRC [BB/K001051/1]
  3. Spanish Ministry of Science and Innovation [AGL2009-08412-AGR]
  4. BBSRC [BBS/E/C/000I0310, BB/K001051/1] Funding Source: UKRI
  5. Biotechnology and Biological Sciences Research Council [BBS/E/C/000I0310, BB/K001051/1] Funding Source: researchfish

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Agricultural soils are a major source of nitric- (NO) and nitrous oxide (N2O), which are produced and consumed by biotic and abiotic soil processes. The dominant sources of NO and N2O are microbial nitrification and de nitrification, and emissions of NO and N2O generally increase after fertiliser application. The present study investigated the impact of N-source distribution on emissions of NO and N2O from soil and the significance of denitrification, rather than nitrification, as a source of NO emissions. To eliminate spatial variability and changing environmental factors which impact processes and results, the experiment was conducted under highly controlled conditions. A laboratory incubation system (DENIS) was used, allowing simultaneous measurement of three N-gases (NO, N2O, N-2) emitted from a repacked soil core, which was combined with N-15-enrichment isotopic techniques to determine the source of N emissions. It was found that the areal distribution of N and C significantly affected the quantity and timing of gaseous emissions and N-15-analysis showed that N2O emissions resulted almost exclusively from the added amendments. Localised higher concentrations, so-called hot spots, resulted in a delay in N2O and N-2 emissions causing a longer residence time of the applied N-source in the soil, therefore minimising NO emissions while at the same time being potentially advantageous for plant-uptake of nutrients. If such effects are also observed for a wider range of soils and conditions, then this will have major implications for fertiliser application protocols to minimise gaseous N emissions while maintaining fertilisation efficiency.

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