Dr. Juerg M. Matter (University of Southampton)
Mineralisation of CO2 via CO2-fluid rock reactions has been proposed as the most permanent solution for geologic CO2 storage. However, as of today, it was unclear how fast CO2 is converted to carbonate minerals in-situ in geologic storage reservoirs. The CarbFix I project in Iceland was designed to verify in-situ CO2 mineralisation in an unconventional storage reservoir in basaltic rocks. Two injection tests were conducted at a pilot injection site near the Hellisheidi geothermal powerplant, SE of Reykjavik. 175 tons of pure CO2 and 73 tons of a CO2+H2S mixture were injection from January to March 2012 and in June 2012, respectively. The gases were injected fully dissolved in groundwater into a permeable basalt formation between 400 and 800 m depth using a novel CO2 injection system. Using conservative (SF6, SF5CF3) and reactive (14C) tracers, we quantitatively monitored and detected dissolved and chemically transformed CO2. Tracer breakthrough curves obtained from the first monitoring well indicate that the injected solution arrived in a fast short pulse and a late broad peak. Mass balance calculations using the tracer data reveal that up to 95% of the injected CO2 has been mineralized over a period of two years. This is supported by multiple evidence of carbonate precipitation found in core samples and on the submersible pump in the monitoring well.