This work aimed for implementing PHREEQC for assessing
the interactions
between CO2, brine, and the aquifer minerals, with more
focus on implementing equilibrium and kinetic batch modeling for understanding
the properties changes up to the stable equilibrium state induced
by injecting a fixed partial pressure CO2 into a carbonate
aquifer. Equilibrium modeling suggested a slight reduction in porosity
up to equilibrium driven mainly by chalcedony precipitation, where
mineral trapping was mainly from dawsonite precipitation in addition
to a small amount from dolomite precipitation. Running a kinetic model
for 10,000 years showed that the later precipitation of secondary
minerals made the porosity decrease to a value of 11.77%. Mineralogy
has a profound effect. Carbonate mineral dissolution provides more
bicarbonate ions to the solution to reach a higher equilibrium pH.
Calcite, though it affected mineral trapping slightly, allowed quick
mineralization with its quick dissolution in addition to inducing
less effect on other minerals reaction rates when its volume fraction
increased. This resulted in less porosity reduction in the long term.
Conversely, albite affected mineral trapping significantly due to
its direct effect on dawsonite precipitation. However, more effect
would be induced on system storage in the long term as more chalcedony
would form with a higher albite fraction.