Postcore flood analysis was conducted
on a tertiary-mode CO2 flooding test under reservoir conditions.
A composite carbonate
core was retrieved to extract remaining hydrocarbons via Dean-stark
distillation, and asphaltenes were measured in the extracted oil from
each plug core using the IP-143 method. The analysis revealed uneven
variation of asphaltene mass along plug cores: more asphaltenes were
collected from the inlet-side core. To understand the mechanism of
uneven in situ asphaltene-deposition, two numerical models were adopted
that were based on thermodynamic and three-dimensional geological
porous transport. The outcomes of thermodynamic modeling, using a
cubic-plus-association model to estimate asphaltene precipitation
as a function of CO2 concentration, proposed a scenario
causing the uneven asphaltene distribution by incorporating vaporizing-gas-drive
(VGD) into an asphaltene-destabilizing mechanism. This means more
asphaltene deposition was predominantly caused when purer CO2 was in contact with fresh reservoir oil. The vaporized intermediate
hydrocarbons in front, extracted through VGD, might dilute the injected
CO2 concentration in the gas phase. This briefly caused
the CO2 concentration to be higher in the inlet-side cores
and lower in the outlet-side cores. Using a micro-CT scanned core,
a 3D geological transport model was generated to estimate in-depth
penetration of asphaltene particles in porous media. Three particle
sizes (0.59–17.6 μm) were modeled as per visual inspection
of destabilized asphaltene particles/aggregates that grew as oil was
mixed with higher CO2 concentration (average particle diameters
of 2.5, 3.6, and 17.6 μm for 0, 20, and 40 mol % CO2 addition). The setting of model particle sizes also considered the
pore throat size distribution of the 3D geological transport model.
The 3D transport model results propose a subsequent scenario in which
smaller asphaltene spheres penetrate more deeply in porous media.