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Biogeosciences An interactive open-access journal of the European Geosciences Union
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Volume 11, issue 14
Biogeosciences, 11, 3721–3728, 2014
https://doi.org/10.5194/bg-11-3721-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
Biogeosciences, 11, 3721–3728, 2014
https://doi.org/10.5194/bg-11-3721-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.

Technical note 17 Jul 2014

Technical note | 17 Jul 2014

Technical Note: Simple formulations and solutions of the dual-phase diffusive transport for biogeochemical modeling

J. Y. Tang and W. J. Riley J. Y. Tang and W. J. Riley
  • Department of Climate and Carbon Sciences, Earth Sciences Division, Lawrence Berkeley National Lab (LBL), Berkeley, CA, USA

Abstract. Representation of gaseous diffusion in variably saturated near-surface soils is becoming more common in land biogeochemical models, yet the formulations and numerical solution algorithms applied vary widely. We present three different but equivalent formulations of the dual-phase (gaseous and aqueous) tracer diffusion transport problem that is relevant to a wide class of volatile tracers in land biogeochemical models. Of these three formulations (i.e., the gas-primary, aqueous-primary, and bulk-tracer-based formulations), we contend that the gas-primary formulation is the most convenient for modeling tracer dynamics in biogeochemical models. We then provide finite volume approximation to the gas-primary equation and evaluate its accuracy against three analytical models: one for steady-state soil CO2 dynamics, one for steady-state soil CH4 dynamics, and one for transient tracer diffusion from a constant point source into two different sequentially aligned medias. All evaluations demonstrated good accuracy of the numerical approximation. We expect our result will standardize an efficient mechanistic numerical method for solving relatively simple, multi-phase, one-dimensional diffusion problems in land models.

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