Article ID Journal Published Year Pages File Type
4546989 Journal of Contaminant Hydrology 2011 9 Pages PDF
Abstract

We consider transport of a solute that undergoes a nonlinear heterogeneous reaction: after reaching a threshold concentration value, it precipitates on the solid matrix to form a crystalline solid. The relative importance of three key pore-scale transport mechanisms (advection, molecular diffusion, and reaction) is quantified by the Péclet (Pe) and Damköhler (Da) numbers. We use multiple-scale expansions to upscale a pore-scale advection–diffusion equation with reactions entering through a boundary condition on the fluid–solid interface, and to establish sufficient conditions under which macroscopic advection–dispersion-reaction equations provide an accurate description of the pore-scale processes. These conditions are summarized by a phase diagram in the (Pe, Da)-space, parameterized with a scale-separation parameter that is defined as the ratio of characteristic lengths associated with the pore- and macro-scales.

Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Earth-Surface Processes
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