Despite the multiple
length and time scales over which fluid-mineral
interactions occur, interfacial phenomena control the exchange of
matter and impact the nature of multiphase flow, as well as the reactivity
of C–O–H fluids in geologic systems. In general, the
properties of confined fluids, and their influence on porous geologic
phenomena are much less well understood compared to those of bulk
fluids. We used equilibrium molecular dynamics simulations to study
fluid systems composed of propane and water, at different compositions,
confined within cylindrical pores of diameter ∼16 Å carved
out of amorphous silica. The simulations are conducted within a single
cylindrical pore. In the simulated system all the dangling silicon
and oxygen atoms were saturated with hydroxyl groups and hydrogen
atoms, respectively, yielding a total surface density of 3.8 −OH/nm2. Simulations were performed at 300 K, at different bulk propane
pressures, and varying the composition of the system. The structure
of the confined fluids was quantified in terms of the molecular distribution
of the various molecules within the pore as well as their orientation.
This allowed us to quantify the hydrogen bond network and to observe
the segregation of propane near the pore center. Transport properties
were quantified in terms of the mean square displacement in the direction
parallel to the pore axis, which allows us to extract self-diffusion
coefficients. The diffusivity of propane in the cylindrical pore was
found to depend on pressure, as well as on the amount of water present.
It was found that the propane self-diffusion coefficient decreases
with increasing water loading because of the formation of water bridges
across the silica pores, at sufficiently high water content, which
hinder propane transport. The rotational diffusion, the lifespan of
hydrogen bonds, and the residence time of water molecules at contact
with the silica substrate were quantified from the simulated trajectories
using the appropriate autocorrelation functions. The simulations contribute
to a better understanding of the molecular phenomena relevant to the
behavior of fluids in the subsurface.