Notes
The mass of CO₂ that escapes from the storage system must include a consideration of both observed leakage and potential future leakage. For terrestrial geologic storage, fugitive emissions can be directly monitored during and after the injection period, though this is more challenging for subseafloor reservoirs. If geologic storage results in functionally stable form on a short timescale — for example, via subsurface mineralization — fugitive emissions associated with the full lifetime of storage may be estimated based on direct observations of the storage reservoir. If, however, the integrity of geologic storage requires ongoing monitoring and maintenance, for example with the injection of supercritical CO₂, the potential for future fugitive emissions must be modeled. For alternative storage systems, like mineralization in concrete, it is possible to directly measure the conversion of input CO₂ into a functionally stable form and therefore the fugitive emissions from the storage system.