Please use this identifier to cite or link to this item: http://hdl.handle.net/2440/121034
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Type: Journal article
Title: Coupled reactive flow and dissolution with changing reactive surface and porosity
Author: Altree-Williams, A.
Brugger, J.
Pring, A.
Bedrikovetsky, P.
Citation: Chemical Engineering Science, 2019; 206:289-304
Publisher: Elsevier
Issue Date: 2019
ISSN: 0009-2509
1873-4405
Statement of
Responsibility: 
A. Altree-Williams, J. Brugger, A. Pring, P. Bedrikovetsky
Abstract: Mineral dissolution flows in porous media occur in numerous industrial and natural processes. We investigate the effects of varying rock-liquid interface on mineral dissolution transport in porous media. The one-dimensional mineral-dissolution flow problem that accounts for varying reacting interface and porosity is essentially non-linear. However, a novel exact solution is derived. The exact solution reveals a four-zone structure of the flow pattern with typical mineral concentration curves in all zones. The exact solution allows for a simplified inverse solver, facilitating determination of the surface function from laboratory reactive flow tests. Accounting for surface area evolution in the governing system of equations allows for significant improvement of matching the experimental data if compared with the constant-surface model. Moreover, the comparison between the analytical model and laboratory data reveals high agreement. The values of equilibrium mineral concentration as obtained from the matching and by thermodynamic calculations exhibit close agreement.
Keywords: Reactive flow; mineral dissolution; porous media; mathematical model; exact solution; reactive surface
Rights: © 2019 Elsevier Ltd. All rights reserved.
RMID: 0030119650
DOI: 10.1016/j.ces.2019.05.016
Grant ID: http://purl.org/au-research/grants/arc/DP140102765
http://purl.org/au-research/grants/arc/LP150100626
http://purl.org/au-research/grants/arc/LP160101497
Appears in Collections:Chemical Engineering publications

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