Geological heterogeneities essentially affect the dynamics of a CO2 plume in
subsurface environments. Previously we showed how the dynamics of a CO2 plume
is influenced by the multi-scale stratal architecture in deep saline
reservoirs. The results strongly suggest that representing small-scale features
is critical to understanding capillary trapping processes. Here we present the
result of simulation of CO2 trapping using two different conventional
approaches, i.e. Brooks-Corey and van Genuchten, for the capillary pressure
curves. We showed that capillary trapping and dissolution rates are very
different for the Brooks-Corey and van Genuchten approaches when heterogeneity
and hysteresis are both represented.Comment: 10 pages 6 figure