Percolation of a CO2-enriched fluid in a limestone’s core: Evolutions of the hydraulic, electrical, chemical and structural properties
Percolation of CO2-rich fluids in limestones causes the dissolution (and eventual reprecipitation) of calcium carbonate minerals, which affect the rock microstructure and change the rock petrophysical properties (i.e., hydraulic, electrical, and elastic properties). In addition, microstructural chan...
| Main Authors: | , , , , , , |
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| Format: | Journal Article |
| Published: |
Wiley-Blackwell Publishing
2014
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| Online Access: | http://hdl.handle.net/20.500.11937/7476 |