The
wettability behaviors of nanoscale pores in shales from Longmaxi
Formation in the Sichuan Basin of South China, which contain quartz
pores, illite pores, and organic matter pores, were investigated using
the molecular dynamics simulation and experimental methods, and the
organic matter surface was approximated by grafting oxygenated functional
groups onto a graphite surface. The distribution characteristics of
a water–methane system in organic matter pores were studied.
The results indicate that the organic matter pore network and the
inorganic pore network in shales show cross-distribution characteristics.
The speed of spontaneous imbibition of oil is less than that of water,
and the spontaneous imbibition mass of oil increases with increasing
the total organic carbon (TOC) contents. The surfaces of illite and
quartz mineral are hydrophilic. With the increase in oxygen-containing
functional groups, the interaction energy between the organic matter
surface and water molecules decreases, resulting in an increase in
the wetting contact angle of the organic matter surface. With increasing
temperature, the interaction energy between the organic matter surface
and water molecules increases, resulting in a decrease in the wetting
contact angle. In symmetrical graphite pore models with different
C/O ratios, water molecules are symmetrically spread near the oxygen-functionalized
graphite wall, and with a decrease in the C/O ratio, the relative
concentration of water molecules increases and the diffusion coefficient
decreases. In contrast, methane molecules are gathered and distributed
in the center of the pore. In an asymmetric graphite pore model with
different C/O ratios, water molecules are asymmetrically spread near
the oxygen-functionalized graphite wall, whereas methane molecules
are concentrated and spread in the pore center. The side with a lower
C/O ratio has stronger hydrophilicity and a higher relative concentration
of water molecules, whereas the side with a higher C/O ratio has stronger
hydrophobicity and a lower relative concentration of water molecules.