This RiMG (Reviews in Mineralogy & Geochemistry) volume includes contributions that review experimental, characterization, and modeling advances in our understanding of pore-scale geochemical processes. The volume had its origins in a special theme session at the 2015 Goldschmidt Conference in Prague. From a diversity of pore-scale topics that ranged from multi-scale characterization to modeling, this work summarizes the state-of-the-science in this subject. Topics include: modification of thermodynamics and kinetics in small pores. chemo-mechanical processes and how they affect porosity evolution in geological media. small angle neutron scattering (SANS) techniques. how isotopic gradients across fluid–mineral boundaries can develop and how...
[1] This study examined the effects of variations in mineral spatial distributions on reaction rates...
The critical zone is the thin outer layer supporting life on earth. It is a compartment in which man...
Fluid flow in transforming porous rocks, fracture networks, and granular media is a very active inte...
Reactive transport models that describe mineral reactions in porous media rely on laboratory measur...
Recent technical advances have demonstrated the importance of pore-scale geochemical processes for g...
Reactivity of minerals is controlled by chemical processes at mineral-fluid interfaces acting at ...
Reactive transport models that describe mineral reactions in porous media rely on laboratory measure...
When Irvin Fatt wrote his classical paper on pore-network modeling (Fatt 1956), he would probably n...
The reservoir quality of sedimentary rocks is closely related to diagenesis, a process involving pos...
In geochemically reacting environments, the mineral dissolution and precipitation alters the structu...
Prediction of the fate and environmental impacts of groundwater contaminants requires the identifica...
When Irvin Fatt wrote his classical paper on pore-network modeling (Fatt 1956), he would probably no...
In geochemically reacting environments, the mineral dissolution and precipitation alters the structu...
Microorganisms capable of biomineralization can catalyze mineral precipitation by modifying local ph...
The scale-dependence of geochemical reaction rates hinders their use in continuum scale models inten...
[1] This study examined the effects of variations in mineral spatial distributions on reaction rates...
The critical zone is the thin outer layer supporting life on earth. It is a compartment in which man...
Fluid flow in transforming porous rocks, fracture networks, and granular media is a very active inte...
Reactive transport models that describe mineral reactions in porous media rely on laboratory measur...
Recent technical advances have demonstrated the importance of pore-scale geochemical processes for g...
Reactivity of minerals is controlled by chemical processes at mineral-fluid interfaces acting at ...
Reactive transport models that describe mineral reactions in porous media rely on laboratory measure...
When Irvin Fatt wrote his classical paper on pore-network modeling (Fatt 1956), he would probably n...
The reservoir quality of sedimentary rocks is closely related to diagenesis, a process involving pos...
In geochemically reacting environments, the mineral dissolution and precipitation alters the structu...
Prediction of the fate and environmental impacts of groundwater contaminants requires the identifica...
When Irvin Fatt wrote his classical paper on pore-network modeling (Fatt 1956), he would probably no...
In geochemically reacting environments, the mineral dissolution and precipitation alters the structu...
Microorganisms capable of biomineralization can catalyze mineral precipitation by modifying local ph...
The scale-dependence of geochemical reaction rates hinders their use in continuum scale models inten...
[1] This study examined the effects of variations in mineral spatial distributions on reaction rates...
The critical zone is the thin outer layer supporting life on earth. It is a compartment in which man...
Fluid flow in transforming porous rocks, fracture networks, and granular media is a very active inte...