The
wettability behavior of reservoir rocks plays a vital role
in determining CO2 storage capacity and containment security.
Several experimental studies characterized the wettability of CO2/brine/rock systems for a wide range of realistic conditions.
To develop a fundamental understanding of the molecular mechanisms
responsible for such observations, the results of molecular dynamics
simulations, conducted at atomistic resolution, are reported here
for representative systems in a wide range of pressure and temperature
conditions. Several force fields are considered, achieving good agreement
with experimental data for the structure of interfacial water but
only partial agreement in terms of contact angles. In general, the
results suggest that, at the conditions chosen, water strongly wet
calcite, resulting in water contact angles either too low to be determined
accurately with the algorithms implemented here or up to ∼46°,
depending on the force field implemented. These values are in agreement
with some, but not all experimental data available in the literature,
some of which report contact angles as high as 90°. One supercritical
CO2 droplet was simulated in proximity of the wet calcite
surface. The results show pronounced effects due to salinity, which
are also dependent on the force field implemented to describe the
solid substrate. When the force field predicts complete water wettability,
increasing NaCl salinity seems to slightly increase the calcite affinity
for CO2, monotonically as the NaCl concentration increases,
because of the preferential adsorption of salt ions at the water–rock
interface. When the other force field was implemented, it was not
possible to quantify salt effects, but the simulations suggested strong
interactions between the supercritical CO2 droplet and
the second hydration layer on calcite. The results presented could
be relevant for predicting the longevity of CO2 sequestration
in geological repositories.