Assessment of the risks and environmental impacts of
carbon geosequestration
requires knowledge about the wetting behavior of mineral surfaces
in the presence of CO2 and the pore fluids. In this context,
the interfacial tension (IFT) between CO2 and the aqueous
fluid and the contact angle, θ, with the pore mineral surfaces
are the two key parameters that control the capillary pressure in
the pores of the candidate host rock. Knowledge of these two parameters
and their dependence on the local conditions of pressure, temperature,
and salinity is essential for the correct prediction of structural
and residual trapping. We have performed classical molecular dynamics
simulations to predict the CO2–water IFT and the
CO2–water–calcite contact angle. The IFT
results are consistent with previous simulations, where simple point
charge water models have been shown to underestimate the water surface
tension, thus affecting the simulated IFT values. When combined with
the EPM2 CO2 model, the SPC/Fw water model indeed underestimates
the IFT in the low-pressure region at all temperatures studied. On
the other hand, at high pressure and low temperature, the IFT is overestimated
by ∼5 mN/m. Literature data regarding the CO2/water/calcite
contact angle on calcite are contradictory. Using our new set of force
field parameters, we performed NVT simulations at 323 K and 20 MPa
to calculate the contact angle of a water droplet on the calcite {10.4}
surface in a CO2 atmosphere. We performed simulations for
both spherical and cylindrical droplet configurations for different
initial radii to study the size dependence of the water contact angle
on calcite in the presence of CO2. Our results suggest
that the contact angle of a cylindrical droplet, is independent of
droplet size, for droplets with a radius of 50 Å or more. On
the contrary, spherical droplets make a contact angle that is strongly
influenced by their size. At the largest size explored in this study,
both spherical and cylindrical droplets converge to the same contact
angle, 38°, indicating that calcite is strongly wetted by water.