Abstract
The paper presents a simple constitutive model for normally consolidated clay. A mathematical formulation, using a single tensor-valued function to define the incrementally nonlinear stress–strain relation, is proposed based on the basic concept of hypoplasticity. The structure of the tensor-valued function is determined in the light of the response envelope. Particular attention is paid towards incorporating the critical state and to the capability for capturing undrained behaviour of clayey soils. With five material parameters that can be determined easily from isotropic consolidation and triaxial compression tests, the model is shown to provide good predictions for the response of normally consolidated clay along various stress paths, including drained true triaxial tests and undrained shear tests.
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The financial support of Australian Research Council (grant DP0453056) is gratefully acknowledged by the first author.
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Appendix
Appendix
Here we present a brief description of the hypoplastic model proposed by Mašín [12]. The constitutive equation is
Here the fourth order tensor L takes the form
and the second order tensor N is given as
with m being defined by
In these equations, the parameters a and F are related to the critical friction angle φc and the Lode angle θ through the relation [21]
with \(\tan \psi = {\sqrt 3 }|\hat{\varvec{\sigma} }_{\rm d} \,|.\) The parameter Y in expression for N, known as the degree of nonlinearity [16], has the following form:
where I 1, I 2 and I 3 are the first, second and third stress invariants, respectively:
The factors f s and f d in Eq. 29 are defined by
where the scalar parameter α can be determined from
The factors c 1 and c 2 in above equation are related to other parameters via
The model contains five parameters: φc, λ*, κ*, r and N *, where φc is the critical state friction angle, λ* and κ* has the same meaning as in Eq.10a, b, r is the ratio of the bulk modulus over the shear modulus at an isotropic stress state, r=K + i /G i , and N * represents the logarithmic specific volume at a mean pressure of 1 kPa so that N *=ln (1+e) |p=1 kPa.
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Huang, WX., Wu, W., Sun, DA. et al. A simple hypoplastic model for normally consolidated clay. Acta Geotech. 1, 15–27 (2006). https://doi.org/10.1007/s11440-005-0003-3
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DOI: https://doi.org/10.1007/s11440-005-0003-3