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The results also show that the equal permeability point of has moved towards the right.
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The reservoir sand units have high porosities and permeabilities pointing to the fact that they might have been deposited in a progradational shallow marine shelve depositional environment with lesser degree of grain size sorting.
After determination of saturation and relative permeability end point values, relative permeability curvatures in mathematical function can be adjusted until the flow behavior match the laboratory observations.
Thus, the permeability in point bar sediments can be different not only from regional aquifer but also from modern streambed.
Because of the low scCO2 relative permeability end point, post-scCO2-injection chase brine operation is not found to be an effective means of enhancing residual trapping.
High density of tellurite glasses, their low glassy state transition temperature and wide range of IR permeability (melting point lower than 1000 °C) [1] should also be noted.
With the ageing of deposition in a floodplain, the permeability of point bar sediments can likely decrease due to reduced effects of the upward flow and gas ebullition.
The measured scCO2 relative permeability end point is low compared to previous measurements on similar sandstones, which poses a challenge for CO2 flow, formation pressure control, and storage efficiency.
In particular, 20 permeability data points were used to generate the permeability model using geostatistical methods (Table 1).
Notable to mention, the relative permeability end points of water and oil are determined by the experiments.
As discussed above, it is apparent that the majority of the porosity and permeability data points are above 15% and 100 mD, respectively.
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