Permeability, porosity, and mineral surface area changes in basalt cores induced by reactive transport of CO2-rich brine
Four reactive flow-through laboratory experiments (two each at 0.1 ml/min and 0.01 ml/min flow rates) at 150°C and 150 bar (15 MPa) are conducted on intact basalt cores to assess changes in porosity, permeability, and surface area caused by CO2-rich fluid-rock interaction. Permeability decreases sli...
| Main Authors: | , , , , , |
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| Format: | Journal article |
| Published: |
Wiley
2017
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