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BACK ANALYSIS OF GEOTECHNICAL PROBLEMS 189












            Figure 6.14 Rheological model.
            elastic modulus of the rock mass, and laboratory shear tests, for determining the
            peak and residual values of the friction angle along the schistosities.
              The elastic modulus for the rock mass ranged between 6000 and 14,700 MN/
             2
            m . The shear tests provided average values of peak and residual friction angles
            of about 60° and 34°, respectively. The relatively large value of the peak friction
            angle depends on the appreciable influence of its “geometrical” portion.
              In addition to the above investigation, the following measurements were also
            carried out during excavation to monitor the overall stability of the opening:

             1) Size  of  the  relaxed  zone  around  the  tunnel  using  multiple  point
               extensometers to a depth of 6 to 10m.
             2) Convergence of the opening contour.
             3) Axial force in the rock bolts.
             4) Seismic wave velocity by geophysical survey.


                                   Model for the analysis
            The  mentioned  in  situ  measurements  showed  an  appreciable  time-dependent
            deformation  of  the  opening.  This  suggested  to  base  the  back  analyses  on  the
            rheological material model depicted in Figure 6.14. It consists of a linear spring
            (governing the instantaneous response of the rock mass), a friction block (with
            limit resistance governed by the Mohr-Coulomb criterion) and a linear dashpot
            (that accounts for the observed time-dependent behaviour).
              The rock mass surrounding the tunnel did not exhibit an appreciable volume
            increase (or swelling) during time. This allows the disregarding of the volumetric
            part of the viscous behaviour, i.e. the one related to the spherical component of
            the state of stress, and to consider only one deviatoric viscosity coefficient η for
            the rheological model.
              The shear strength c, φ and viscosity η parameters of the rock mass represent
            the free variables of the back analysis. The values of the elastic constants were
            chosen on the basis of in situ investigations. As suggested in [24], the average
                                                                       2
            value  of  the  elastic  modulus  from  the  plate  load  tests  (E=10,000  MN/m )  was
            adopted, and Poisson’s ratio was estimated equal to 0.3.
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