Micro-continuum simulations on heterogeneous rock images show initial flow heterogeneity controls dynamic dissolution regimes, producing time-varying permeability-porosity power-law exponents up to 40.9 and effective reaction rates suppressed by 1-3 orders of magnitude below uniform predictions.
\ Navarre-Sitchler, A
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Dynamic Evolution of Pore-scale Heterogeneity and Transport Conditions Control Mineral Dissolution Regimes
Micro-continuum simulations on heterogeneous rock images show initial flow heterogeneity controls dynamic dissolution regimes, producing time-varying permeability-porosity power-law exponents up to 40.9 and effective reaction rates suppressed by 1-3 orders of magnitude below uniform predictions.