International audienceWe studied experimentally the dissolution of a porous limestone core during CO2-enriched water injection. We measured the changes in porosity and permeability arising from modifications of the pore network geometry and the fluid-rock interface. A methodology based on periodic X-ray microtomography imaging was implemented to record the evolution of the time- and scale-dependent microstructures with a spatial resolution of 4.91 μm. Two processes were successively involved in the rapid permeability increase of the sample, as documented from microscale to core-scale measurements..
To determine the effect of dissolution on pore network development in carbonate rocks, dissolution e...
Percolation of CO2-rich fluids in limestones causes the dissolution (and eventual reprecipitation) o...
Limestone dissolution by CO2 -rich brine induces critical changes of the pore network geometrical pa...
International audienceWe studied experimentally the dissolution of a porous limestone core during CO...
International audienceWe studied experimentally the dissolution of a porous limestone core during CO...
We studied experimentally the dissolution of a porous limestone core during CO2-enriched water injec...
We studied experimentally the dissolution of a porous limestone core during CO2-enriched water injec...
International audienceA reactive flow-through experiment by carbon dioxide-saturated water at the pa...
A reactive flow-through experiment by carbon dioxide-saturated water at the partial pressure of 0.1 ...
A reactive flow-through experiment by carbon dioxide-saturated water at the partial pressure of 0.1 ...
A reactive flow-through experiment by carbon dioxide-saturated water at the partial pressure of 0.1 ...
The injection of CO2-rich fluids in carbonate rocks results in an evolution of the pore space, with ...
International audienceA CO2-rich brine core-flood experiment in calcite limestone for conditions rep...
Rock dissolution induces changes in texture (porosity, pore-size distribution, or tortuosity) which ...
Rock dissolution induces changes in texture (porosity, pore-size distribution, or tortuosity) which ...
To determine the effect of dissolution on pore network development in carbonate rocks, dissolution e...
Percolation of CO2-rich fluids in limestones causes the dissolution (and eventual reprecipitation) o...
Limestone dissolution by CO2 -rich brine induces critical changes of the pore network geometrical pa...
International audienceWe studied experimentally the dissolution of a porous limestone core during CO...
International audienceWe studied experimentally the dissolution of a porous limestone core during CO...
We studied experimentally the dissolution of a porous limestone core during CO2-enriched water injec...
We studied experimentally the dissolution of a porous limestone core during CO2-enriched water injec...
International audienceA reactive flow-through experiment by carbon dioxide-saturated water at the pa...
A reactive flow-through experiment by carbon dioxide-saturated water at the partial pressure of 0.1 ...
A reactive flow-through experiment by carbon dioxide-saturated water at the partial pressure of 0.1 ...
A reactive flow-through experiment by carbon dioxide-saturated water at the partial pressure of 0.1 ...
The injection of CO2-rich fluids in carbonate rocks results in an evolution of the pore space, with ...
International audienceA CO2-rich brine core-flood experiment in calcite limestone for conditions rep...
Rock dissolution induces changes in texture (porosity, pore-size distribution, or tortuosity) which ...
Rock dissolution induces changes in texture (porosity, pore-size distribution, or tortuosity) which ...
To determine the effect of dissolution on pore network development in carbonate rocks, dissolution e...
Percolation of CO2-rich fluids in limestones causes the dissolution (and eventual reprecipitation) o...
Limestone dissolution by CO2 -rich brine induces critical changes of the pore network geometrical pa...