2007
DOI: 10.1029/2006wr005206
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Coupling between geochemical reactions and multicomponent gas and solute transport in unsaturated media: A reactive transport modeling study

Abstract: [1] The two-way coupling that exists between biogeochemical reactions and vadose zone transport processes, in particular gas phase transport, determines the composition of soil gas. To explore these feedback processes quantitatively, multicomponent gas diffusion and advection are implemented into an existing reactive transport model that includes a full suite of geochemical reactions. Multicomponent gas diffusion is described on the basis of the dusty gas model, which accounts for all relevant gas diffusion me… Show more

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Cited by 107 publications
(89 citation statements)
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“…57 can be replaced with the Nernst-Planck equation. Equations 56 and 57 can be expanded to consider transport in phases other that the liquid by adding the corresponding accumulation and transport terms [35,36].…”
Section: Reactive Transport Equationsmentioning
confidence: 99%
“…57 can be replaced with the Nernst-Planck equation. Equations 56 and 57 can be expanded to consider transport in phases other that the liquid by adding the corresponding accumulation and transport terms [35,36].…”
Section: Reactive Transport Equationsmentioning
confidence: 99%
“…This requirement is not currently enforced in TMVOC, but was implemented in the code for this work. As noted above, equimolar flux is a reasonable assumption for multicomponent gas transport in high permeability landfill cover soils [Molins and Mayer, 2007b].…”
Section: A) Gas Flow In Landfillsmentioning
confidence: 99%
“…Both models fitted the data well producing nearly identical results, which implied that both Knudsen and nonequimolar diffusion were minor. Simulations using Fick's law in the ADM framework also produced very small errors in this landfill cover soil [Molins and Mayer, 2007b;Molins and Mayer, 2007a].…”
Section: A) Gas Flow In Landfillsmentioning
confidence: 99%
“…(2011) Advective fluxes, on the other hand, may be induced by soil-atmosphere barometric pressure gradients causing bulk movement of gasses into or out of soils Poulsen 2003;Massman 2006;Redecker 2015). Pressure gradients may also be induced by reactions; for example the simple stoichiometry of CH 4 oxidation results in a net decrease in pore-gas volume, while the production of CO 2 and CH 4 result in a net increase in pore-gas volume (Molins and Mayer 2007). The direction of flow depends on whether soilatmosphere pressure gradients are positive (atmospheric pressure > pore-gas pressure) or negative (atmospheric pressure < pore-gas pressure) (Elberling et al 1998).…”
Section: Mass Transport Of Pore Gas In Unsaturated Reclamation Cover mentioning
confidence: 99%