Stearic acid is an example of a carboxylic compound naturally
present
in geological formations (deep saline aquifers and depleted hydrocarbon
reservoirs), which renders the rock hydrophobic (CO2-wet)
over a geological time scale. Such hydrophobic surfaces are detrimental
to residual CO2 trapping. There is, however, a lack of
comprehensive dataset about how traces of these organic molecules
affect the rock′s CO2 wettability and residual CO2 trapping. We, thus, used in situ NMR T
1–T
2 2D images to visualize
fluid configurations in the pore network and used T
1/T
2 ratios to assess the
microscopic wettability of the rock to pore space fluids subsequent
to each process step. The T
2 relaxation
time was measured to demonstrate displacement processes and evaluate
the trapping behavior at the pore scale, which is closely correlated
to reservoir-scale flow functions. The trapping in the CO2-wet sample (14%) was significantly lower than that of the analogous
water-wet sample (18%). This reduction in CO2 trapping
is due to surface macroscopic flow layers acting as conduits allowing
slow desaturation of CO2. Importantly, in the CO2-wet sample, trapping predominately occurred in meso- and micropores,
whereas trapping in the analogous water-wet rock primarily occurred
in macropores. This work thus provides a comprehensive dataset on
the impact of organic acids on residual trapping at the pore scale,
which ultimately helps to advance industrial-scale implementation
of CGS and EOR project schemes in carbonate reservoirs.