Percolation of a CO2-enriched fluid in a limestone’s core: Evolutions of the hydraulic, electrical, chemical and structural properties

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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...

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Bibliographic Details
Main Authors:	Vialle, Stephanie, Contraires, S., Zinzsner, B., Clavaud, J., Mahiouz, K., Zuddas, P., Zamora, M.
Format:	Journal Article
Published:	Wiley-Blackwell Publishing 2014
Online Access:	http://hdl.handle.net/20.500.11937/7476

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