Carbon capture and storage (CCS) is an important component
in many
national net-zero strategies. Ensuring that CO2 can be
safely and economically stored in geological systems is critical.
To date, CCS research has focused on the physiochemical behavior of
CO2, yet there has been little consideration of the subsurface
microbial impact on CO2 storage. However, recent discoveries
have shown that microbial processes (e.g., methanogenesis) can be
significant. Importantly, methanogenesis may modify the fluid composition
and the fluid dynamics within the storage reservoir. Such changes
may subsequently reduce the volume of CO2 that can be stored
and change the mobility and future trapping systematics of the evolved
supercritical fluid. Here, we review the current knowledge of how
microbial methanogenesis could impact CO2 storage, including
the potential scale of methanogenesis and the range of geologic settings
under which this process operates. We find that methanogenesis is
possible in all storage target types; however, the kinetics and energetics
of methanogenesis will likely be limited by H2 generation.
We expect that the bioavailability of H2 (and thus potential
of microbial methanogenesis) will be greatest in depleted hydrocarbon
fields and least within saline aquifers. We propose that additional
integrated monitoring requirements are needed for CO2 storage
to trace any biogeochemical processes including baseline, temporal,
and spatial studies. Finally, we suggest areas where further research
should be targeted in order to fully understand microbial methanogenesis
in CO2 storage sites and its potential impact.