Interfacial tension data and models
are of great importance to
the storage of CO2 in deep saline aquifers. In this study,
the pendant-drop method combined with axisymmetric drop shape analysis
was used in the interpretation of the interfacial behavior of CO2 and brine. Extensive experimental measurements of the interfacial
tension between CO2 and an NaCl solution were acquired
for pressures ranging from 3.0 to 12.0 MPa, temperatures from 300
to 353 K, and NaCl molalities from 0 to 1.8 mol·kg–1, for a total of 1,254 valid data points. All experiments were conducted
in a pressure cell fitted with a capillary tube to create pendant
droplets in a CO2-rich atmosphere. The experimental results
indicated that interfacial tension decreased with increasing pressure
and increased with temperature and salinity. As pressure increased
to a certain point, the interfacial tension reached a plateau. At
a given temperature, the CO2–aqueous system reached
a plateau for different salinities under nearly the same pressure.
However, the plateau pressure increased with temperature. The plateau
interfacial tension value slightly increased with temperature and
salinity. We also found a linear relationship between the change in
interfacial tension and the molality concentration of brine. An empirical
model was also proposed based on the Parachor model for the prediction
of interfacial tension. Most results of this model deviated by less
than ±5% from our experimental results, indicating that the model
was a good fit to our experiments.