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Three‐dimensional elasto‐plastic model for unsaturated compacted soils with different initial densities
Author(s) -
Sun D.A.,
Matsuoka H.,
Cui H.B.,
Xu Y.F.
Publication year - 2003
Publication title -
international journal for numerical and analytical methods in geomechanics
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.419
H-Index - 91
eISSN - 1096-9853
pISSN - 0363-9061
DOI - 10.1002/nag.313
Subject(s) - geotechnical engineering , isotropy , suction , materials science , compression (physics) , yield surface , stress (linguistics) , plane stress , soil water , mechanics , yield (engineering) , plasticity , triaxial shear test , geology , constitutive equation , structural engineering , engineering , composite material , thermodynamics , finite element method , physics , soil science , linguistics , philosophy , quantum mechanics , shear (geology)
This paper presents an elasto‐plastic model for unsaturated compacted soils and experimental results obtained from a series of suction‐controlled triaxial tests on unsaturated compacted clay with different initial densities. The initial density dependency of the compacted soil behaviour is modelled by establishing experimental relationships between the initial density and the corresponding yield stress and thereby between the initial density and the location and slope of normal compression line. The model is generalized to three‐dimensional stress states by assuming that the shapes of the failure surface and the yield surface in the deviatoric plane are given by the extended SMP criterion. A considerable number of the isotropic compression, triaxial compression and extension tests on unsaturated compacted clay with different initial densities were performed using a suction‐controllable triaxial apparatus, to measure the stress–strain–volume change in different stress paths and wetting paths. The model has well‐predicting capabilities to reproduce the mechanical behaviour of specimens compacted under different conditions not only in isotropic compression but also in triaxial compression and triaxial extension. Copyright © 2003 John Wiley & Sons, Ltd.