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Separating N2O production and consumption in intact agricultural soil cores at different moisture contents and depths.
Button, Erik S; Marsden, Karina A; Nightingale, Philip D; Dixon, Elizabeth R; Chadwick, David R; Jones, David L; Cárdenas, Laura M.
Afiliación
  • Button ES; School of Natural Sciences Bangor University Bangor Gwynedd UK.
  • Marsden KA; School of Natural Sciences Bangor University Bangor Gwynedd UK.
  • Nightingale PD; Plymouth Marine Laboratory, Prospect Pl, Marine Biogeochemical Observations Plymouth Devon UK.
  • Dixon ER; Rothamsted Research North Wyke, Net Zero and Resilient Farming Okehampton Devon UK.
  • Chadwick DR; School of Natural Sciences Bangor University Bangor Gwynedd UK.
  • Jones DL; School of Natural Sciences Bangor University Bangor Gwynedd UK.
  • Cárdenas LM; Centre for Sustainable Farming Systems, Food Futures Institute Murdoch Western Australia Australia.
Eur J Soil Sci ; 74(2): e13363, 2023.
Article en En | MEDLINE | ID: mdl-38529015
ABSTRACT
Agricultural soils are a major source of the potent greenhouse gas and ozone depleting substance, N2O. To implement management practices that minimize microbial N2O production and maximize its consumption (i.e., complete denitrification), we must understand the interplay between simultaneously occurring biological and physical processes, especially how this changes with soil depth. Meaningfully disentangling of these processes is challenging and typical N2O flux measurement techniques provide little insight into subsurface mechanisms. In addition, denitrification studies are often conducted on sieved soil in altered O2 environments which relate poorly to in situ field conditions. Here, we developed a novel incubation system with headspaces both above and below the soil cores and field-relevant O2 concentrations to better represent in situ conditions. We incubated intact sandy clay loam textured agricultural topsoil (0-10 cm) and subsoil (50-60 cm) cores for 3-4 days at 50% and 70% water-filled pore space, respectively. 15N-N2O pool dilution and an SF6 tracer were injected below the cores to determine the relative diffusivity and the net N2O emission and gross N2O emission and consumption fluxes. The relationship between calculated fluxes from the below and above soil core headspaces confirmed that the system performed well. Relative diffusivity did not vary with depth, likely due to the preservation of preferential flow pathways in the intact cores. Gross N2O emission and uptake also did not differ with depth but were higher in the drier cores, contrary to expectation. We speculate this was due to aerobic denitrification being the primary N2O consuming process and simultaneously occurring denitrification and nitrification both producing N2O in the drier cores. We provide further evidence of substantial N2O consumption in drier soil but without net negative N2O emissions. The results from this study are important for the future application of the 15N-N2O pool dilution method and N budgeting and modelling, as required for improving management to minimize N2O losses.
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Texto completo: 1 Colección: 01-internacional Banco de datos: MEDLINE Idioma: En Revista: Eur J Soil Sci Año: 2023 Tipo del documento: Article

Texto completo: 1 Colección: 01-internacional Banco de datos: MEDLINE Idioma: En Revista: Eur J Soil Sci Año: 2023 Tipo del documento: Article