Phsw. Kulatilake et al., DISCONTINUITY GEOMETRY CHARACTERIZATION IN A TUNNEL CLOSE TO THE PROPOSED PERMANENT SHIPLOCK AREA OF THE 3 GORGES DAM SITE IN CHINA, International journal of rock mechanics and mining sciences & geomechanics abstracts, 33(3), 1996, pp. 255-277
Citations number
19
Categorie Soggetti
Geochemitry & Geophysics","Mining & Mineral Processing
Discontinuity data from a 400 m tunnel located close to the proposed s
hiplock area were investigated to characterize the discontinuity geome
try of the rock mass around the tunnel. Traces of 39 major discontinui
ties (faults and dykes) were found on the tunnel exposures. Over 2000
minor discontinuity (joint) trace data available showed that the rock
mass can be separated into about five statistically homogeneous region
s. Three to four joint sets were found to exist in each of these regio
ns, Available theoretical probability, distributions, were found to be
insufficient to represent the statistical distribution of orientation
of joint clusters. For about 94% of the joint sets, the gamma distrib
ution was found to be the best probability distribution for representi
ng a joint size distribution. Exponential and gamma distributions were
the best probability distributions for representing joint spacing dis
tributions for the joint data studied here, Censored joint trace data
showed a significant effect of the trace length biases on the estimate
d mean trace length. This indicated that the 2 m wide exposures which
were used for collecting the joint trace data may not be sufficient to
produce reliable estimates for joint size parameters for the shiplock
area. Different estimates were obtained based on, wall data and roof
data for the joint size and 3-D intensity parameters. The following ma
y have contributed to this result: (a) the effect of different finite
sample sizes used; (b) the effect of sampling biases; and (c) the effe
ct of modelling uncertainties on the estimated parameters. To obtain b
etter estimates, it is suggested to collect joint data for several exp
osures which are at least 4-5 m wide and have different orientations.
When such data become available for the Three Gorges region, it is sug
gested;to perform validation studies to check the applicability of the
models, in addition to performing the joint geometry, modelling.