An approach is developed to scale up the two-dimensional conductivity tenso
r for highly heterogenous fracture networks, based on a numerical modelling
approach that was proposed previously by Zhang et al., J. Rock Mech. Min.
Sci. 33, 17-37 (1996). In that approach, it was assumed that the fractured
rock mass was statistically uniform and only a unit square of sample rock w
as needed to work out the conductivity tensor. Hence, its application was l
imited where the heterogenous characteristics of a fracture network was not
negligible. In the present paper, the local conductivity tensors, both mag
nitude and direction, either calculated based on small fracture networks or
samples measured on separate exposures are scaled up to estimate the overa
ll nature of conductivity for a relatively large region.
The approach developed is used to estimate the two-dimensional conductivity
tensor of naturally fractured rock masses for two types of fracture networ
ks, constant aperture and variable aperture under stress. The effects of sa
mple number and sample size of local sub-areas were examined against the to
tally sampled area. Finally, field data were used to predict the overall co
nductivity tensor of a large region, based on four fracture networks sample
d on separate exposures within the region. (C) 1999 Elsevier Science B.V. A
ll rights reserved.