I am trying to understand the difference in the spreading rate of supercritical-CO2 plume for a stacked reservoir. The hypothetical reservoir has two permeable horizons, separated by a non-permeable horizon. I am trying to account for which of the petrophysical properties (porosity, permeability, entry pressure, relative permeability) is controlling the radial plume spreading rate the most and for that I am trying to calculate the dissimilar behaviour of the plume spreading rate curves (which is a time-distance plot). Can anyone suggest which statistical measure should I follow to account for the dissimilarity between the two curves?

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