modeling approach of the relationship between nitrous oxide fluxes from soils and the water-filled pore space

Nitrous oxide (N₂O) fluxes can increase significantly following small increases in soil water-filled pore space (WFPS). Thus, it is essential to improve our knowledge of this crucial relationship to better model N₂O emissions by soils. We studied how much the addition of a gas transport and a gas–li...

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Bibliographic Details
Published in:Biogeochemistry 2015-02, Vol.122 (2-3), p.395-408
Main Authors: Rabot, E, Cousin, I, Hénault, C
Format: Article
Language:English
Subjects:
Biogeochemistry
Biogeosciences
Continental interfaces, environment
diffusivity
Drying
Earth and Environmental Science
Earth Sciences
Ecosystems
Emissions
Environmental Chemistry
Life Sciences
Mathematical models
Moisture content
Nitrous oxide
Pollution monitoring
Sciences of the Universe
Sensitivity analysis
soil
Soil sciences
Soil surfaces
Soil water
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Summary:Nitrous oxide (N₂O) fluxes can increase significantly following small increases in soil water-filled pore space (WFPS). Thus, it is essential to improve our knowledge of this crucial relationship to better model N₂O emissions by soils. We studied how much the addition of a gas transport and a gas–liquid equilibrium module to the model of N₂O emissions NOE could improve simulation results. A sensitivity analysis of the modified model (NOEGTE: gas transport and equilibrium) was first performed, and then the model was tested with published data of a wetting–drying experiment. Simulated N₂O fluxes plotted against WFPS appeared to be bell-shaped during the 7 days simulated, combining the effects of the low N₂O production for WFPS  0.95. The WFPS generating the maximum simulated N₂O fluxes shifted with time, from 0.76 after 12 h, to 0.79 after 168 h, because of an increase over time of the gas concentration gradient between the soil surface and the atmosphere. NOEGTEappeared able to capture the pattern of N₂O emissions monitored in the experimental data. In particular, N₂O peaks during drying were well reproduced in terms of timing, but their magnitudes were often overestimated. They were attributed to the increasing gas diffusivity and N₂O exchanges from the liquid phase to the gaseous phase.
ISSN:0168-2563
1573-515X
DOI:10.1007/s10533-014-0048-1