Molecular
diffusion has been proved to be the main factor affecting
the solubility and miscibility of carbon dioxide (CO2).
On the basis of previous work, X-ray computed tomography (CT) technology
is developed in this paper to investigate the CO2 diffusion
process in brine with varying pressures and a constant temperature,
simulating CO2 storage in a saline aquifer. Interface migration
and volume expansion in response to CO2 diffusion processes
are imaged by use of an X-ray tomographic scanner and quantitatively
analyzed. Volume expansion and pressure decline occur simultaneously.
Interfacial area and migration velocity were calculated to describe
interface migration related to the diffusion process. Combined with
Fick’s second law, the CO2 diffusion coefficients,
which vary with pressure, are calculated in consideration of the mixture
volume V
mix and interfacial area A. The CO2 diffusion process is divided into
two stages, early and late. Two effective diffusion coefficients,
corresponding to these two stages, were calculated. The results representing
the early stages are in the range (1.0–2.2) × 10–7 m2·s–1, which is 2 orders of magnitude
larger than those for late stages of the experiments, in the range
(1.9–2.1) × 10–9 m2·s–1. The first coefficient increases linearly as the
pressure increases from 2 to 8 MPa, showing strong sensitivity to
pressure. In contrast, diffusion coefficients during the late stage
can be assumed to be constant for a wide range of pressures. The maximum
velocity of the interface migration tested here can reach 1.5 ×
10–5 m·h–1. Equilibrium solubility
is in the range of 0.20–1.24 mol·L–1. This is of great significance for understanding the mass-transfer
process in CO2 storage.