Percolation parameter and percolation-threshold estimates for three-dimensional random ellipses with widely scattered distributions of eccentricity and size
Jr. De Dreuzy et al., Percolation parameter and percolation-threshold estimates for three-dimensional random ellipses with widely scattered distributions of eccentricity and size, PHYS REV E, 62(5), 2000, pp. 5948-5952
In fractured materials of very low matrix permeability, fracture connectivi
ty is the first-order determinant of the occurrence of flow. For systems ha
ving a narrow distribution of object sizes (short-range percolation), a fir
st-order percolation criterion is given by the total excluded Volume which
is almost constant at threshold. In the case of fractured media, recent obs
ervations have demonstrated that the fracture-length distribution is extrem
ely large. Because of this widely scattered fracture-length distribution, t
he classical expression of the total excluded volume is no longer scale inv
ariant at the percolation threshold and has no finite limit for infinitely
large systems. Thus, the classical estimation method of the percolation thr
eshold established in short-range percolation becomes useless for the conne
ctivity determination of fractured media. In this study, we derive an expre
ssion for the total excluded volume that remains scale invariant at the per
colation threshold and that can thus be used as the proper control paramete
r, called the parameter of percolation in percolation theory. We show that
the scale-invariant expression of the total excluded volume is the geometri
cal union normalized by the system volume rather than the summation of the
mutual excluded volumes normalized by the system volume. The summation of t
he mutual excluded volume (classical expression) remains linked to the numb
er of intersections between fractures, whereas the normalized geometrical u
nion of the mutual excluded volume (our expression) can be essentially iden
tified with the percolation parameter. Moreover, fluctuations of this perco
lation parameter at threshold with length and eccentricity distributions re
main limited within a range of less than one order of magnitude, giving in
rum a rough percolation criterion. We finally show that the scale dependenc
e of the percolation parameter causes the connectivity of fractured media t
o increase with scale, meaning especially that the hydraulic properties of
fractured media fan dramatically change with scale.