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Effective parameters in heterogeneous and homogeneous transport models with kinetic sorption
Author(s) -
Reichle R.,
Kinzelbach W.,
Kinzelbach H.
Publication year - 1998
Publication title -
water resources research
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.863
H-Index - 217
eISSN - 1944-7973
pISSN - 0043-1397
DOI - 10.1029/97wr03518
Subject(s) - sorption , porosity , porous medium , thermodynamics , retardation factor , dispersion (optics) , kinetic energy , plume , partition coefficient , materials science , statistical physics , mathematics , physics , chemistry , classical mechanics , chromatography , adsorption , column chromatography , optics , composite material
Transport of dissolved tracers undergoing kinetic sorption in saturated porous media is described on the basis of a dual‐porosity model with heterogeneous and cross‐correlated sorption parameters, i.e., distribution coefficient and exchange rate. The approach is a conceptual model for reactive transport in a medium with spatially varying reaction capacity, given by the distribution coefficient, and spatially varying accessibility, given by the exchange rate. We treat the sorption parameters as a stochastic process and apply a perturbation approach. From the ensemble‐averaged spatial moments of a plume, we analytically derive formal expressions for time‐dependent effective transport parameters. For vanishing microdispersion the calculations are carried out up to second order for the effective transport velocity u eff ( t ) and the effective dispersion coefficient D eff ( t ). For large times the effective retardation is determined by the ensemble‐averaged distribution coefficient, whereas the effective dispersion is related to the sorption parameters in a more complicated way depending on the variability of the exchange rate and of the distribution coefficient. Effective sorption parameters are given. For comparison we derive exact expressions for u eff ( t ) and D eff ( t ) in a homogeneous triple‐porosity model. Unlike the simpler homogeneous dual‐porosity model, the triple‐porosity model yields a satisfactory description of the time‐dependent dispersion of the heterogeneous model. The appropriate sorption parameters for the triple‐porosity model are given as functions of the stochastic parameters.