Step propagation controls pore shape evolution when mineral walls dissolve under saturation gradients
- 31 May 2024
- journal article
- research article
- Published by Elsevier in Geochimica et Cosmochimica Acta
- Vol. 379, 219-232
Abstract
No abstract availableKeywords
This publication has 72 references indexed in Scilit:
- Simulation of mineral dissolution at the pore scale with evolving fluid-solid interfaces: review of approaches and benchmark problem setComputational Geosciences, 2020
- Chemical mechanisms of dissolution of calcite by HCl in porous media: Simulations and experimentAdvances in Water Resources, 2018
- Evaluation of Macroscopic Porosity‐Permeability Relationships in Heterogeneous Mineral Dissolution and Precipitation ScenariosWater Resources Research, 2017
- Mineralogical and transport controls on the evolution of porous media texture using direct numerical simulationWater Resources Research, 2017
- Effects of pore-scale precipitation on permeability and flowAdvances in Water Resources, 2016
- Pore‐scale simulation of carbonate dissolution in micro‐CT imagesJournal of Geophysical Research: Solid Earth, 2016
- Porosity and permeability development in compacting chalks during flooding of nonequilibrium brines: Insights from long‐term experimentJournal of Geophysical Research: Solid Earth, 2015
- Pore‐scale study of dissolution‐induced changes in hydrologic properties of rocks with binary mineralsWater Resources Research, 2014
- Permeability evolution due to dissolution and precipitation of carbonates using reactive transport modeling in pore networksWater Resources Research, 2013
- Surface chemistry, etch pits and mineral-water reactionsGeochimica et Cosmochimica Acta, 1986