The main purpose of the present work is to predict the permeability of a po
rous medium from its three-dimensional (3D) porous structure network. In th
is work, 3D porous structure is reconstructed by the truncated Gaussian met
hod using Fourier transform and starting from a 2D binary image obtained fr
om a thin section of a porous sample. The skeleton of the 3D porous structu
re provides a way of visualizing the graph of the pore network. It is deter
mined using a thinning algorithm, which is conceived to preserve topology.
It gives both visual and quantitative information about the connectivity of
the pore space, the coordination number for every node and local hydraulic
radius. Once the network of the pore structure is obtained, the macroscopi
c transport properties, such as the permeability, can be predicted. The met
hod is applied to a 500 mo Berea sandstone and the predicted permeability i
s in good agreement with the experimental value and empirical correlations.