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Experimental dissolution of dolomite by CO2-charged brine at 100°C and 150bar: Evolution of porosity, permeability, and reactive surface area
A. Luhmann
,
X. Kong
,
B. Tutolo
,
N. Garapati
,
B. Bagley
,
M. Saar
,
W. Seyfried
2014
Chemical Geology
DOI: 10.1016/j.chemgeo.2014.05.001
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No abstract is available for this publication.