A significant uncertainty which remains for CO2 sequestration, is the effect of natural geological heterogeneities
and hysteresis on capillary trapping over different length scales. This paper uses laboratory data measured in
cores from the Goldeneye formation of the Captain D Sandstone, North Sea in 1D numerical simulations to
evaluate the potential capillary trapping from natural rock heterogeneities across a range of scales, from cm to
65m. The impact of different geological realisations, as well as uncertainty in petrophysical properties, on the
amount of capillary heterogeneity trapping is estimated. In addition, the validity of upscaling trapping characteristics in terms of the Land trapping parameter is assessed. The numerical models show that the capillary
heterogeneity trapped CO2 saturation may vary between 0 and 14% of the total trapped saturation, depending
upon the geological realisation and petrophysical uncertainty. When upscaling the Land model from core-scale
experimental data, using the maximum experimental Land trapping parameter could increase the expected
heterogeneity trapping by a factor of 3. Conversely, depending on the form of the imbibition capillary pressure
curve used in the numerical model, including capillary pressure hysteresis may reduce the heterogeneity trapping by up to 70%.