 
          1402
        
        
          Proceedings of the 18
        
        
          th
        
        
          International Conference on Soil Mechanics and Geotechnical Engineering, Paris 2013
        
        
          0.0
        
        
          0.1
        
        
          0.2
        
        
          0.3
        
        
          0.4
        
        
          0.5
        
        
          1
        
        
          100
        
        
          
            Number of Cycles to reach ru = 1.0
          
        
        
          
            Cyclic Stress Ratio, CSR
          
        
        
          10000
        
        
          
            No rth Co as t Ca lc a re o us S and
          
        
        
          
            S ilic e o us S and ( A ) ( Hus s e in , 200 8 )
          
        
        
          
            S ilic e o us S and ( B ) ( Ev ans & Zho u , 1995 )
          
        
        
          
            σc ' = 100 kP a
          
        
        
          
            Dr = 40 %
          
        
        
          `
        
        
          Figure 10. Liquefaction susceptibility of calcareous and siliceous sands
        
        
          (
        
        
          
            Elmamlouk et al.
          
        
        
          ).
        
        
          Another study on peculiar soils is presented by
        
        
          
            Orense &
          
        
        
          
            Pender
          
        
        
          (New Zealand) on ‘Liquefaction characteristics of
        
        
          crushable pumice sand’ which, like other volcanic soils, is
        
        
          poorly investigated in literature. Undrained CTX tests were
        
        
          performed on reconstituted specimens of uniform sand and
        
        
          undisturbed frozen samples of well-graded sandy silt. The
        
        
          effects of D
        
        
          r
        
        
          and
        
        
          
        
        
          c
        
        
          on the liquefaction resistance were not as
        
        
          significant compared to that of hard-grained sands. Empirical
        
        
          liquefaction procedures derived for hard-grained soils were
        
        
          assessed by comparing the CRR (this time evaluated as CSR
        
        
          corresponding to 15 cycles) from the CTX tests on undisturbed
        
        
          specimens with those from cone penetration (CPT) and seismic
        
        
          dilatometer (sDMT) tests at the sampling sites. Due to particle
        
        
          breakage, the penetration-based methods did not agree well with
        
        
          the laboratory values, while that based on shear wave velocity
        
        
          (Andrus & Stokoe, 2000) showed better correlation (Fig. 11).
        
        
          Figure 11. Comparison between CRR from CTX and those from CPT
        
        
          (a) and V
        
        
          S
        
        
          (b) empirical methods (
        
        
          
            Orense & Pender
          
        
        
          ).
        
        
          
            Åhnberg et al.
          
        
        
          (Sweden) report a comprehensive study on
        
        
          ’Degradation of clay due to cyclic loadings and deformations’
        
        
          including CTX tests on many soft clays with variable frequency,
        
        
          highlighting that the cyclic overstrength was proportional to the
        
        
          logarithm of strain rate. They also mention that the cyclic
        
        
          resistance in terms of cyclic/static strength ratio increased with
        
        
          decreasing sensitivity and increasing organic content, although
        
        
          more specific correlations are not explicitly reported.
        
        
          3.4
        
        
          
            Analytical and physical modelling
          
        
        
          
            Park & Ahn
          
        
        
          (South Korea) propose an interesting ‘Accumulated
        
        
          stress based model for prediction of residual pore pressure’. The
        
        
          model uses a damage parameter, function of the cyclic stress
        
        
          ratio and of the length of the shear stress path, to transform the
        
        
          pore pressure model by Seed et al. (1975), which is instead
        
        
          based on the equivalent number of cycles. The formulation can
        
        
          be therefore incorporated in coupled effective stress analyses of
        
        
          dynamic transient motions in the time domain. The calibration
        
        
          procedure of the parameters, based on the cyclic resistance
        
        
          curves measured in stress-controlled cyclic tests, was
        
        
          successfully validated through comparisons with published and
        
        
          original laboratory test data on clean and silty sands (Fig. 12).
        
        
          Figure 12. Comparison of measured and predicted cyclic resistance and
        
        
          pore pressures (
        
        
          
            Park & Ahn
          
        
        
          ).
        
        
          The paper ‘Liquefaction impact revisited’ by
        
        
          
            Barends et al.
          
        
        
          (Holland) reports laboratory tests on the variation of partial
        
        
          liquefaction with space and time. 1D (soil column) and 3D
        
        
          (cylindrical tub) models were filled with loose sand,
        
        
          respectively overlying and surrounded by a denser one, and
        
        
          instrumented to measure pore pressures and displacements
        
        
          under impact loads. When even partial liquefaction occurred,
        
        
          significant pore pressures arose also in the non-liquefied
        
        
          surroundings and slowly dissipated during the sedimentation of
        
        
          the liquefied mass (Fig. 13). The related porosity decrease was
        
        
          however small enough that the sand remained loose, and re-
        
        
          liquefaction was likely to occur due to subsequent new shaking.
        
        
          Figure 13. Typical pore pressure records after a full liquefying impact
        
        
          load (
        
        
          
            Barends et al.
          
        
        
          ).
        
        
          4 LIQUEFACTION: EMPIRICAL METHODS, FIELD
        
        
          OBSERVATIONS AND COUNTERMEASURES
        
        
          4.1
        
        
          
            Empirical methods
          
        
        
          
            Katzenbach et al.
          
        
        
          (Germany) critically review the ‘Recent
        
        
          developments in procedures for estimation of liquefaction
        
        
          potential of soils’ in relation with Eurocode 8 (2010) as well as
        
        
          the methods described in the NCEER workshops (Youd et al.
        
        
          2001). They discuss the main factors influencing the evaluation
        
        
          of CSR and CRR, claiming for more refinements and univocal
        
        
          approaches in terms of definition of screening criteria, stress
        
        
          reduction factor r
        
        
          d
        
        
          , effects of fines content, magnitude scaling
        
        
          factor. They also suggest to introduce more details in EC8 about
        
        
          the use of penetration resistance and of V
        
        
          S
        
        
          .
        
        
          
            Wang et al.
          
        
        
          (China) discuss the ‘Performance-based
        
        
          evaluation of saturated loess ground liquefaction’ which
        
        
          supports recent updating of the seismic guidelines of Gansu