Abstract
Solute dispersion in fluid flow results from the interaction between advection and diffusion. The relative contributions of these two mechanisms to mass transport are characterized by the reduced velocity , also referred to as the Péclet number. In the absence of diffusion (i.e., when the solute diffusion coefficient and ), divergence-free laminar flow of an incompressible fluid results in a zero-transverse dispersion coefficient , both in ordered and random two-dimensional porous media. We demonstrate by numerical simulations that a more realistic realization of the condition using and letting the fluid flow velocity approach infinity leads to completely different results for ordered and random two-dimensional porous media. With increasing reduced velocity, approaches an asymptotic value in ordered two-dimensional porous media but grows linearly in disordered (random) structures depending on the geometrical disorder of a structure: a higher degree of heterogeneity results in a stronger growth of with . The obtained results reveal that disorder in the geometrical structure of a two-dimensional porous medium leads to a growth of with even in a uniform pore-scale advection field; however, lateral diffusion is a prerequisite for this growth. By contrast, in ordered two-dimensional porous media the presence of lateral diffusion leads to a plateau for the transverse dispersion coefficient with increasing .
7 More- Received 27 February 2017
DOI:https://doi.org/10.1103/PhysRevE.95.063108
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