To improve the efficiency
of CO
2
geological sequestration,
it is of great significance to in-depth study the physical mechanism
of the immiscible CO
2
–water displacement process,
where the influential factors can be divided into fluid–fluid
and fluid–solid interactions and porous media characteristics.
Based on the previous studies of the interfacial tension (capillary
number) and viscosity ratio factors, we conduct a thorough study about
the effects of fluid–solid interaction (i.e., wettability)
and porous media characteristics (i.e., porosity and non-uniformity
of granule size) on the two-phase displacement process by constructing
porous media with various structural parameters and using a multiphase
lattice Boltzmann method. The displacement efficiency of CO
2
is evaluated by the breakthrough time characterizing the displacement
speed and the quasi-steady state saturation representing the displacement
amount. It is shown that the breakthrough time of CO
2
becomes
longer, but the quasi-steady state saturation increases markedly with
the increase in CO
2
wettability with the surface, demonstrating
an overall improvement of the displacement efficiency. Furthermore,
the breakthrough time of CO
2
shortens and the saturation
increases significantly with increasing porosity, granule size, and
non-uniformity, showing the improvement of the displacement efficiency.
Therefore, enhancing the wettability of CO
2
with the surface
and selecting reservoirs with greater porosity, larger granule size,
and non-uniformity can all contribute to the efficiency improvement
of CO
2
geological sequestration.