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  ON THE SHAFT FRICTION MODELLING OF NON-DISPLACEMENT 
 PILES IN SANDTIME-DEPENDENT SHEAR DEFORMATION CHARACTERISTICS OF 
 GEOMATERIALS AND THEIR SIMULATION  
 
 Tatsuoka Fumio, Ishihara Masanori, Di Benedetto Herve 
  and Kuwano Reiko   
 ABSTRACT: The viscous aspects of the stress-strain behaviour 
 of saturated and air-dried clean sands in drained plane strain 
 compression (PSC) and saturated clean sand and soft clays in undrained 
 triaxial compression (TC) are presented. Common as well as different 
 viscous features among the different geomaterials are addressed. The 
 general three-component model is used as the framework for constitutive 
 modelling, in which the total strain ratee  
 is decomposed into elastic and irreversible components ee 
 andeir while the stresss 
 is decomposed into inviscid (non-viscous) and viscous components sfandsv 
 . In the simplest model (called the new isotach model) among those 
 described in the papersf, is a 
 non-linear function ofeir , whilesv 
 is a non-linear function of eirand 
 sfalways proportional tosf 
 for primary loading. This model is relevant to kaolin for the full 
 pre-peak range and a reconstituted low-plasticity clay (Fujinomori clay) 
 at small strains, both in undrained TC. The model is modified to 
 simulate the viscous effect that decays witheir 
 , as observed with clean sands and a natural soft clay. It is shown that 
 the second type of model (called the viscous evanescent model and the 
 TESRA model) simulates well the above-mentioned behaviour, not only 
 during primary loading, but also at unloaded conditions. The model is 
 further modified to simulate the behaviour of Fujinomori clay whereby 
 the rate at which the viscous effect decays gradually increases witheir 
 (the general TESRA model). The viscous componentssv 
 of the three models can be represented by a pair of common equations, 
 and the other models are specifically simplified versions of the general 
 TESRA model.  
 Keywords: Constitutive modelling, Deformation, Plane strain 
 compression tests, Geomaterials, Three-component model, Triaxial 
 compression tests, Viscous effect (IGC: D6/D7)  
 
 
 
 
 
 
 
 
 
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