Locating and developing ideal sites for large-scale capture
and
storage of carbon dioxide has become increasingly necessary due to
increasing global emissions and warming. Mafic–ultramafic rocks
present a unique geologic setting as they can trap injected CO2 in pore space, mineralize that CO2 to permanently
store it as carbonate minerals, and simultaneously release critical
minerals. However, these reservoirs are undercharacterized relative
to sedimentary carbon storage settings. In this study, we execute
a methodology for determining carbonation and critical mineral recovery
potential in mafic–ultramafic reservoirs. Using an olivine-rich
basalt from the island of Hawai’i, we performed petrologic
and geochemical analyses to determine its chemistry, mineralogy, and
pore network architecture. We use this data to first quantify the
nonreactive storage resource potential and determine the bulk storage
of 50 MMT of CO2 in the pore space of a basalt volume test
case, along with realistic P10, P50, and P90 scenarios for that same
volume. Then, using the chemistry and mineralogy, we both estimate
the total mineralization and critical mineral recovery potential,
as well as more realistic values based on dissolution–precipitation
reactions at the surface areas of pores. This storage resource estimate
methodology can assist in accelerating the global commercialization
of geologic carbon storage and critical mineral recovery.