Improvement of remeshed Lagrangian methods for the simulation of dissolution processes at pore-scale. (December 2020)

• Record Type: Journal Article
• Authors: Etancelin, Jean-Matthieu; Moonen, Peter; Poncet, Philippe
• Is Part Of: Advances in water resources. Volume 146(2020)
• Publication Date: 2020-12
• Subjects: Three-dimensional flows -- Digital rock physics -- Reactive flows -- Dissolution process -- Lagrangian methods -- Porous media; Hydrology -- Periodicals; Hydrodynamics -- Periodicals; Hydraulic engineering -- Periodicals; 551.48
• DOI: 10.1016/j.advwatres.2020.103780
• Languages: English
• ISSNs: 0309-1708

Abstract

Highlights: Focus on hybrid methods using grids and Lagrangian tracking, to reconcile accurate remeshing and sign-preservation. How to choose a remeshing kernel, and how to adapt diffusion to adjust the discrepency introduced by the remeshing. Various two-scale porous media are investigated at rocks pore scale. Abstract: This article shows how to consistently and accurately manage the Lagrangian formulation of chemical reaction equations coupled with the superficial velocity formalism introduced in the late 80s by Quintard and Whitaker. Lagrangian methods prove very helpful in problems in which transport effects are strong or dominant, but they need to be periodically put back in a regular lattice, a process called remeshing. In the context of digital rock physics, we need to ensure positive concentrations and regularity to accurately handle stagnation point neighborhoods. These two conditions lead to the use of kernels resulting in extra-diffusion, which can be prohibitively high when the diffusion coefficient is small. This is the case especially for reactive porous media, and the phenomenon is reinforced in porous rock matrices due to Archie's law. This article shows how to overcome this difficulty in the context of a two-scale porosity model applied in the Darcy-Brinkman-Stokes equations, and how to obtain simultaneous sign preservation, regularity and accurate diffusion, and apply it to dissolution processes at the pore scale of actual rocks.