“…Moreover, in recent years several fractal models have been proposed, for example, in order: to study spontaneous imbibition process in different rock types, fibrous materials, and silica glass [47]; to stream current in porous media [48]; to demonstrate that the heterogeneity of the Geysers rocks can be determined quantitatively using fractal dimension [49]; to evaluate and predict thermal conductivity, permeability, diffusion and sorptivity coefficient taking into account pore size distribution influence [42,[50][51][52][53][54].…”