 
          1454
        
        
          Proceedings of the 18
        
        
          th
        
        
          International Conference on Soil Mechanics and Geotechnical Engineering, Paris 2013
        
        
          On the other hand the PR’s model clearly shows an
        
        
          accumulation of vertical displacement at each cycle. Moreover
        
        
          during the first phase, transient and stationary behaviours can be
        
        
          distinctly observed. The change in amplitude of loading implies
        
        
          a change in the tendency of accumulation.
        
        
          Figure 6. Comparison between mean effective and deviatoric stresses at
        
        
          0.5m depth under the top of the suction caisson for PR and DP models.
        
        
          Corresponding evolutions of mean effective and deviatoric
        
        
          stresses are shown in Figure 6 while pore pressure accumulation
        
        
          is given in Figure 8. During the first part of the loading, the
        
        
          difference between both models is limited. For the Prevost’s
        
        
          model, the transient phase is short and a drop in mean effective
        
        
          stress is coupled with an increase of pore water pressure. Then a
        
        
          stationary phase takes place, corresponding to an
        
        
          accommodation phase (see in Figure 7) and the mean effective
        
        
          pressure gets back to its first value when pore water pressure
        
        
          dissipates. The difference is quantitatively greater for the
        
        
          deviatoric stress but qualitatively the behaviour is identical.
        
        
          Figure 7. Stress paths in the p’-q plane at 0.5m depth (PR model). The
        
        
          first step of loading ends after 1000s when the second begins.
        
        
          During the second part of loading, the soil characterized by
        
        
          PR model shows a continuous decrease of mean effective stress
        
        
          without reaching a stationary state. Greater amplitude of loading
        
        
          entails greater plasticity effects and then contractancy. After
        
        
          about 1600s, the stress path reaches the phase transformation
        
        
          line and the mean effective stress increases for a while before
        
        
          going down again. This continuous contractancy appears
        
        
          because the model involves plasticity in loading and unloading
        
        
          as well as a transition between contractive and dilative zones.
        
        
          On the other hand, the soil described by DP model behaves
        
        
          elastically most of the time because once the greatest deviatoric
        
        
          stress is reached, the stress path lies within the plasticity surface
        
        
          when unloaded and reloaded.
        
        
          4 CONCLUSIONS
        
        
          The Prevost’s model is simple, elegant and able to qualitatively
        
        
          take into account the main features of cyclic loading. Basic
        
        
          parameters are easy to obtain from classical laboratory tests.
        
        
          Nevertheless an accurate modelling of cyclic tests requires
        
        
          additional parameters and a new form of plastic potential.
        
        
          A suction caisson was modelled as a practical case study.
        
        
          Capabilities of the Prevost’s model compared with a classical
        
        
          Drucker-Prager model appear clearly. The transient modelling
        
        
          depicts pore pressure and plastic deformation accumulation
        
        
          which the Drucker-Prager model is unable to represent.
        
        
          Figure 8. Comparison between pore pressure evolutions at 0.5m depth
        
        
          under the top of the suction caisson for PR and DP models.
        
        
          5 ACKNOWLEDGEMENTS
        
        
          I would warmly acknowledge all people that help me daily to
        
        
          achieve this PhD and my colleagues that suffer my little
        
        
          idiosyncrasies. I would also thank the FNRS for its financial
        
        
          support.
        
        
          6 REFERENCES
        
        
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            Verification of Liquefaction Analyses by
          
        
        
          
            Centrigue Studies, Laboratory Testing Program, Soil Data Report. .
          
        
        
          Elgamal, Ahmed, et al. 2003. Modeling of cyclic mobility in saturated
        
        
          cohesionless soils.
        
        
          
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          Houlsby, G. T., Ibsen, L. B. et Byrne, B. W. 2005.
        
        
          
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          Popescu, R. et Prevost, J.-H. 1993. Centrifuge validation of a numerical
        
        
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          Prevost, J.H. 1985. A simple plasticity theory for frictional cohesionless
        
        
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          Vertseele, H. 2012.
        
        
          
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            offshore wind turbines.
          
        
        
          University of Liège. 2012. Master Thesis.
        
        
          Yang, Zhaohui et Elgamal, Ahmed. 2008. Multi-surface Cyclic
        
        
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