An experimental study of basaltic glass-H2O-CO2 interaction at 22 and 50°C: Implications for subsurface storage of CO2
A novel high pressure column flow reactor was used to investigate the evolution of solute chemistry along a 2.3 m flow path during pure water- and CO2-charged water–basaltic glass interaction experiments at 22 and 50 °C and 10−5.7 to 22 bars partial pressure of CO2. Experimental results and geochemi...
| Main Authors: | , , , |
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| Format: | Journal Article |
| Published: |
Pergamon
2014
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| Online Access: | http://hdl.handle.net/20.500.11937/4798 |