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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