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On breakdown of macroscopic models of mixing-controlled heterogeneous reactions in porous media

Journal Article · · Advances in Water Resources, 32(11):1664-1673
Reactive transport in porous media is a complex nonlinear phenomenon that involves both homogeneous (bio-)chemical reactions between species dissolved in a fluid and heterogeneous reactions that occur on liquid-solid interfaces. We establish conditions under which macroscopic reaction-diffusion equations (RDEs) provide an adequate averaged description of pore-scale processes. These conditions are represented by a phase diagram in a two-dimensional space, which is spanned by Damkohler number and a scale-separation parameter. This phase diagram shows that highly localized phenomena in porous media, including precipitation on (and/or dissolution of) a porous matrix, do not lend themselves to macroscopic (upscaled) descriptions. To compute the predictive errors resulting from the use of macroscopic RDEs to describe such phenomena, we upscaled the pore-scale RDEs to the continuum (macroscopic) scale and used pore-scale numerical simulations to verify various upscaling assumptions.
Research Organization:
Pacific Northwest National Laboratory (PNNL), Richland, WA (US)
Sponsoring Organization:
USDOE
DOE Contract Number:
AC05-76RL01830
OSTI ID:
967196
Report Number(s):
PNNL-SA-64544; KP1702030
Journal Information:
Advances in Water Resources, 32(11):1664-1673, Journal Name: Advances in Water Resources, 32(11):1664-1673 Journal Issue: 11 Vol. 32
Country of Publication:
United States
Language:
English

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