Density-driven convection, which
can accelerate the dissolution
rate of carbon dioxide (CO
2
) in resident brine, is critical
for the long-term fate of the injected CO
2
permanence and
security of CO
2
geological storage. Visualization experiments
and pressure–volume–temperature (PVT) testing were conducted
to investigate the influence from gravitational convection. For investigate
gravitational instabilities and convective diffusion, we designed
a Hele-Shaw cell rated to 70 MPa and Rayleigh number of 346 to conduct
visualization experiments with the micro-schlieren technique. The
average diffusion coefficient and time-dependent values were measured
in the PVT experiments. We also calculated the convection parameters,
including Rayleigh number and critical onset time, with a series of
PVT testing at the temperature ranging 293.15–423.15 K and
pressure ranging 14–24 MPa by using the constant-pressure method.
Through visualization experiments, we observed convective currents
triggered by the density gradient in the gas–liquid interface,
which noticeably enhanced the CO
2
dissolution rate. The
PVT testing confirmed that the diffusion coefficient increased sharply
under the influence of the gravitational convection at the early stage
and then decreased toward the average diffusion coefficient with time.
The PVT testing also demonstrated the Rayleigh number increasing with
temperature or pressure increasing under the reservoir conditions.
The gravitational convection will be more likely to occur and more
rapid with a greater pressure or higher temperature.