To
gain a better understanding of the effect of surface coverage
of water (H2O) on methane (CH4) adsorption on
shale, we performed molecular dynamics simulations. The interactions
of H2O with minerals play a key role in the surface coverage
of H2O; hence, two representative minerals were investigated:
muscovite, which has a high layer charge, and pyrophyllite, which
has a net zero layer charge. On the muscovite surface, the amount
of CH4 adsorption decreases due to the formation of a structured
adsorption layer of H2O, which increases the free energy
barrier of CH4 adsorption. On the pyrophyllite surface,
the amount of CH4 adsorption decreases due to the spread
of a H2O droplet on the surface, which reduces accessible
adsorption sites for the CH4 molecules. These insights
from an atomic-scale viewpoint are expected to improve our interpretation
of the results from the core analysis and modeling of the adsorption
amount on shale reservoirs.