Dp. Bentz et Ns. Martys, HYDRAULIC RADIUS AND TRANSPORT IN RECONSTRUCTED MODEL 3-DIMENSIONAL POROUS-MEDIA, Transport in porous media, 17(3), 1994, pp. 221-238
Methods for reconstructing three-dimensional porous media from two-dim
ensional cross sections are evaluated in terms of the transport proper
ties of the reconstructed systems. Two-dimensional slices are selected
at random from model three-dimensional microstructures, based on pene
trable spheres, and processed to create a reconstructed representation
of the original system. Permeability, conductivity, and a critial por
e diameter are computed for the original and reconstructed microstruct
ures to assess the validity of the reconstruction technique. A surface
curvature algorithm is utilized to further modify the reconstructed s
ystems by matching the hydraulic radius of the reconstructed three-dim
ensional system to that of the two-dimensional slice. While having onl
y minor effects on conductivity, this modification significantly impro
ves the agreement between permeabilities and critical diameters of the
original and reconstructed systems for porosities in the range of 25-
40%. For lower porosities, critical pore diameter is unaffected by the
curvature modification so that little improvement between original an
d reconstructed permeabilities is obtained by matching hydraulic radii
.