4.5 Article

Combined physical and chemical nonequilibrium transport model: Analytical solution, moments, and application to colloids

Journal

JOURNAL OF CONTAMINANT HYDROLOGY
Volume 110, Issue 3-4, Pages 87-99

Publisher

ELSEVIER SCIENCE BV
DOI: 10.1016/j.jconhyd.2009.09.004

Keywords

Physical nonequilibrium; Chemical nonequilibrium; Preferential flow; Model; Analytical solution; Moments

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The transport of solutes and colloids in porous media is influenced by a variety of physical and chemical nonequilibrium processes. A combined physical-chemical nonequilibrium (PCNE) model was therefore used to describe general mass transport. The model partitions the pore space into mobile and immobile flow regions with first-order mass transfer between these two regions (i.e, physical nonequilibrium or PNE). Partitioning between the aqueous and solid phases can either proceed as an equilibrium or a first-order process (i.e, chemical nonequilibrium or CNE) for both the mobile and immobile regions. An analytical solution for the PCNE model is obtained using iterated Laplace transforms. This solution complements earlier semi-analytical and numerical approaches to model solute transport with the PCNE model. The impact of selected model parameters on solute breakthrough curves is illustrated. As is well known, nonequilibrium results in earlier solute breakthrough with increased tailing. The PCNE model allows greater flexibility to describe this trend; for example, a closer resemblance between solute input and effluent pulse. Expressions for moments and transfer functions are presented to facilitate the analytical use of the PCNE model. Contours of mean breakthrough time, variance, and spread of the colloid breakthrough curves as a function of PNE and CNE parameters demonstrate the utility of a model that accounts for both physical and chemical nonequilibrium processes. The model is applied to describe representative colloid breakthrough curves in Ottawa sands reported by Bradford et al. (2002). An equilibrium model provided a good description of breakthrough curves for the bromide tracer but could not adequately describe the colloid data. A considerably better description was provide by the simple CNE model but the best description, especially for the larger 3.2-mu m colloids, was provided by the PCNE model. Published by Elsevier B.V.

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