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<identifier>oai:HAL:hal-00963597v1</identifier>
<datestamp>2018-01-11</datestamp>
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<title lang=en>Experimental Characterization of Porosity Structure and Transport Property Changes in Limestone Undergoing Different Dissolution Regimes</title>
<creator>Luquot, Linda</creator>
<creator>RODRIGUEZ, Olivier</creator>
<creator>Gouze, Philippe</creator>
<contributor>Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<source>ISSN: 0169-3913</source>
<source>EISSN: 1573-1634</source>
<source>Transport in Porous Media</source>
<publisher>Springer Verlag</publisher>
<identifier>hal-00963597</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-00963597</identifier>
<source>https://hal.archives-ouvertes.fr/hal-00963597</source>
<source>Transport in Porous Media, Springer Verlag, 2014, 101 (3), pp.507-532. 〈10.1007/s11242-013-0257-4〉</source>
<identifier>DOI : 10.1007/s11242-013-0257-4</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1007/s11242-013-0257-4</relation>
<language>en</language>
<subject lang=en>Structural heterogeneities</subject>
<subject lang=en>CO2 storage</subject>
<subject lang=en>Permeability-porosity relationships</subject>
<subject>[SDU.STU.GP] Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]</subject>
<subject>[PHYS.PHYS.PHYS-GEO-PH] Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]</subject>
<subject>[SDE.MCG] Environmental Sciences/Global Changes</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>Limestone dissolution by CO2 -rich brine induces critical changes of the pore network geometrical parameters such as the pore size distribution, the connectivity, and the tortuosity which govern the macroscopic transport properties (permeability and dispersivity) that are required to parameterize the models, simulating the injection and the fate of CO2 . A set of four reactive core-flood experiments reproducing underground conditions ( T=100∘C and P=12 MPa) has been conducted for different CO2 partial pressures (0.034</description>
<date>2014-02</date>
</dc>
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