Page 199 - Numerical Analysis and Modelling in Geomechanics
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180 ANNAMARIA CIVIDINI AND GIANCARLO GIODA




























            Figure 6.3 Location of the measurement points.
              This  effect  was  introduced  in  the  elastic  back  analysis  through  the  band
            indicated by a dark zone in Figure 6.5. To take into account the overall loss of
            stiffness of the sand in this zone, the moduli of elasticity were assumed equal to
            those of the mentioned six layers multiplied by a reduction factor α, constant for
            all layers. The elastic moduli of each layer and the reduction factor a represent the
            free variables of a second back analysis problem.
              Two calculations were performed considering as input data the displacements
            measured, respectively, at the end of the first and second stages of excavation.
            Figure 6.6 compares the elastic moduli obtained by the back analyses for the two
            excavation  stages  with  the  loading  and  unloading  moduli  obtained  by  the
            dilatometer tests carried out in situ before the beginning of excavation. This back
            analysis led to a reduction factor within the “weak” zone equal to 0.23 and to 0.
            26 for the top and bottom excavations, respectively. The computed and measured
            vertical displacements at the end of excavation are shown in Figure 6.7.
              It  can  be  observed  that,  apart  from  the  reduction  factor,  the  elastic  moduli
            obtained by the back analysis of the first excavation stage are quite close to those
            calculated at the end of the bottom excavation, but for the soil layers located at
            the  tunnel  depth.  This  depends  on  the  fact  that  the  bottom  excavation
            produces  appreciable  incremental  strains  in  the  soil  close  to  the  tunnel  with
            respect to those obtained at the end of the top excavation. This is interpreted by
            the elastic back analysis as a reduction of the equivalent secant modulus of the
            sand in that zone.
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