Two-phase flow of CO2/brine in porous media
is critical
to the capacity and safety of carbon sequestration into the brine
aquifer. In order to provide valuable information and important theoretical
basis for site selection and CO2 injection, the microscopic
visualization technology was employed in this study to conduct displacement
experiments of CO2/brine at the pore scale. Four micromodels
with different sizes and structures, five injection rates of CO2, and six salinities of brine were used to study the effects
of micromodel’s structure and displacement pattern on two-phase
flow. Several parameters including the differential pressure, contact
angle, permeability, velocity field, and force field were obtained
by experimental measurement, image post-processing, and theoretical
analysis, and then, these parameters’ variation was investigated.
Phenomena such as thin film, corner flow, and Haines jump were also
found during the displacement. Although brine could be completely
displaced by CO2 in the capillary duct, the backflow of
the wetting phase would occur at a low injection rate. Phenomena different
from the theoretical analysis also occurred in pore doublet models:
some brine was residual in the homogeneous pore doublet model at a
low injection rate, while the heterogeneous pore doublet model was
fully occupied by CO2 at a high injection rate. These phenomena
are very useful for two-phase flow, and multiple factors need to be
comprehensively considered to determine the operating conditions of
CO2 storage into the brine aquifer.