Wb. Lindquist et al., MEDIAL AXIS ANALYSIS OF VOID STRUCTURE IN 3-DIMENSIONAL TOMOGRAPHIC-IMAGES OF POROUS-MEDIA, J GEO R-SOL, 101(B4), 1996, pp. 8297-8310
We introduce the medial axis as a tool in the analysis of geometric st
ructure of void space in porous media, The medial axis traces the fund
amental geometry of the void pathways. We describe an algorithm for ge
nerating the medial axis of the void structure from digitized three di
mensional images of porous media obtained from X ray CAT scans. The me
dial axis is constructed during an iterative erosion procedure which,
at each step, replaces the image of the void structure with a smaller
version obtained by eroding its surface layer of voxels. The algorithm
is applied to high (5 mu m) resolution microtomographic images of two
rock chips (Berea sandstone and Danish chalk) and a sample pf uniform
(100 mu m) diameter, packed glass beads. We statistically investigate
several geometrical properties of the structure bf the medial axes ob
tained. The first is the distribution of relative volumes in each eros
ion layer of the void space. We find the distributions to be exponenti
al for the two real rock samples and normal for the packed glass beads
. The second property investigated is the distribution of volumes of d
isconnected segments of the medial axis which are in one-to-one corres
pondence with disconnected void segments of the sample. We find indica
tions for a; universal power law behavior governing the distribution o
f volumes of the smallest disconnected pieces. The final behavior stud
ied is a geometric tortuosity as measured by shortest paths through th
e medial axis. This tortuosity distribution appears well described by
a gamma distribution.