In this study we performed three categories of steady-and unsteady-state 8 core-flooding experiments to investigate capillary trapping, relative perme-9 ability, and capillary pressure, in a scCO 2 +SO 2 /brine/limestone system at 10 elevated temperature and pressure conditions, i.e., 60 • C and 19.16 MPa. We 11 used a Madison limestone core sample acquired from the Rock Springs Uplift 12 in southwest Wyoming. We carried out two sets of steady-state drainage-13 imbibition relative permeability experiments with different initial brine sat-14 urations to study hysteresis. We found that the final scCO 2 +SO 2 drainage 15 relative permeability was very low, i.e., 0.04. We also observed a rapid re-16 duction in the scCO 2-rich phase imbibition relative permeability curve, which 17 resulted in a high residual trapping. The results showed that between 62.8% 18 to more than 76% of the initial scCO 2 +SO 2 at the end of drainage was 19 trapped by capillary trapping mechanism (trapping efficiency). We found 20 that at higher initial brine saturations, the trapping efficiency was higher. 21 The maximum initial and residual scCO 2-rich phase saturations at the end 22 of primary drainage and imbibition were 0.525 and 0.329, respectively. Each