DOE PAGES title logo U.S. Department of Energy
Office of Scientific and Technical Information

Title: Dissolution of periodic arrays of grains: Upscaling of pore-scale simulations with fast reactions

Journal Article · · Chemical Geology

Upscaling methods are frequently used to derive transport equations at the macroscopic scale from more fundamental equations formulated at the pore scale. These methods typically give a suitable structure for the macroscopic equations and can also provide explicit expressions for the constitutive parameters, such as permeability and dispersion coefficients. Introducing chemical reactions complicates upscaling in at least two important ways. First, the interplay between chemical reactions and transport processes introduces a new length scale, which can be much smaller than the convective or dispersive length scales. A small reactive length scale breaks one of the key assumptions in upscaling; that there is a significant separation in length between the pore-scale and macro-scale processes. The second complication is that if reactions take place at mineral surfaces (dissolution or precipitation) then the pore space itself is evolving in time. In this paper we suggest ways in which these difficulties can be approached, based on analysis of pore-scale simulation data. First, we noticed that the concentration field in successive unit cells has an almost identical spatial variation, with a single scaling factor for each unit cell that is proportional to the incoming reactant flux. Using pore-scale simulations to determine the mass transfer coefficient in a few unit cells, we can calculate the concentration field in the whole domain, even when dissolution is entirely transport limited. Second, we have noticed a time-dependent mapping of the grain shapes from different unit cells. From these observations, we can deduce constitutive relations where the only time-varying parameter is the porosity. Here, we show that a model based on these ideas can quantitatively account for the pore-scale simulation data.

Research Organization:
Univ. of Florida, Gainesville, FL (United States)
Sponsoring Organization:
National Science Centre of Poland (NCN); USDOE Office of Science (SC), Basic Energy Sciences (BES); USDOE Office of Science (SC), Basic Energy Sciences (BES). Chemical Sciences, Geosciences & Biosciences Division
Grant/Contract Number:
SC0018676
OSTI ID:
1873386
Journal Information:
Chemical Geology, Journal Name: Chemical Geology Vol. 592; ISSN 0009-2541
Publisher:
ElsevierCopyright Statement
Country of Publication:
United States
Language:
English

References (29)

Three-dimensional simulations of fracture dissolution: FRACTURE DISSOLUTION IN 3-D journal September 2016
Interacting length scales in the reactive-infiltration instability: REACTIVE-INFILTRATION INSTABILITY journal June 2013
Transport in ordered and disordered porous media II: Generalized volume averaging journal February 1994
Flow in porous media I: A theoretical derivation of Darcy's law journal January 1986
Transport in ordered and disordered porous media III: Closure and comparison between theory and experiment journal April 1994
Simulation of mineral dissolution at the pore scale with evolving fluid-solid interfaces: review of approaches and benchmark problem set journal January 2020
Multiblock Pore-Scale Modeling and Upscaling of Reactive Transport: Application to Carbon Sequestration journal August 2012
Large-Scale Model for the Dissolution of Heterogeneous Porous Formations: Theory and Numerical Validation journal June 2021
The quasi-stationary state approximation to coupled mass transport and fluid-rock interaction in a porous medium journal January 1988
Taylor dispersion in porous media: Analysis by multiple scale expansions journal January 1995
Upscaling geochemical reaction rates using pore-scale network modeling journal September 2006
Influence of the flow rate on dissolution and precipitation features during percolation of CO2-rich sulfate solutions through fractured limestone samples journal October 2015
Time-dependent shapes of a dissolving mineral grain: Comparisons of simulations with microfluidic experiments journal May 2020
An overview of structurally-controlled dolostone-limestone transitions in the stratigraphic record journal September 2021
Mineral replacement in long-term flooded porous carbonate rocks journal January 2020
Dissolution and deformation in fractured carbonates caused by flow of CO2-rich brine under reservoir conditions journal June 2013
Applicability regimes for macroscopic models of reactive transport in porous media journal March 2011
Effective surface and boundary conditions for heterogeneous surfaces with mixed boundary conditions journal January 2016
Flow-controlled reactions in rock fabrics journal March 1990
Mineral dissolution and wormholing from a pore-scale perspective journal August 2017
Dissolution of a cylindrical disk in Hele-Shaw flow: a conformal-mapping approach journal October 2020
Upscaling pore-scale reactive transport equations using a multiscale continuum formulation: PORE-SCALE REACTIVE TRANSPORT EQUATIONS journal December 2007
The Development of Wormholes in Laboratory‐Scale Fractures: Perspectives From Three‐Dimensional Simulations journal October 2018
Massive serpentinite carbonation at Linnajavri, N-Norway: Massive serpentinite carbonation at Linnajavri, N-Norway journal July 2012
Rigorous Upscaling of the Reactive Flow through a Pore, under Dominant Peclet and Damkohler Numbers journal January 2006
Reactive Flows in Porous Media: Challenges in Theoretical and Numerical Methods journal June 2021
Core-scale description of porous media dissolution during acid injection - Part I: theoretical development journal January 2004
Core-scale description of porous media dissolution during acid injection - part II: calculation of the effective properties journal January 2006
Heat and Mass Transfer in Tubes: An Analysis Using the Method of Volume Averaging journal January 2002