Giang Nguyen
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CY Cergy Paris Université
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Papers by Giang Nguyen
The multiple failure mechanisms captured by the proposed model enable the behavior of cemented granular rocks to be well reproduced for a wide range of confining pressures. Furthermore, through comparison of the model predictions and experimental data, the micromechanical basis of the model provides improved understanding of failure mechanisms of cemented granular materials. In particular, we show that grain crushing is the predominant inelastic deformation mechanism under high pressures while cement failure is the relevant mechanism at low pressures. Over an intermediate pressure regime a mixed mode of failure mechanisms is observed. Furthermore, the micromechanical roots of the model allow the effects on localized deformation modes of various initial microstructures to be studied. The results obtained from both the constitutive responses and BVP solutions indicate that the proposed approach and model provide a promising basis for future theoretical studies on cemented granular materials.
accompanied by intensive deformation and irreversible
micro-structural changes of the material in a small but
finite size region. Shear, compaction, and dilation bands
observed in soils and porous rocks are typical examples
of phenomena that lead to localised failure. The width h
of the localisation band has been experimentally shown
to be a physical quantity related to the microstructure
of the material. On the other hand, numerical methods
for the solution of boundary value problems usually
introduce another length scale H, as a result of the
spatial discretisation of the considered domain into
smaller ones over which the constitutive response of
the material is defined in terms of incremental stressstrain
relationships. While h, as a physical quantity,
is fixed, H varies with the resolution of the numerical
discretisation. Since h scales with the material
microstructure and therefore is usually much smaller
than the resolution of the numerical discretisation,
the case H > h is considered in this study, e.g. failure
behaviour governed by a localisation band of width
h embedded in an elastic bulk of nominal side H. We
present a general constitutive modelling framework to
connect these two scales, and corresponding responses
of the materials inside and outside the localisation zone.
We demonstrate how this approach can help obtain
physically meaningful solutions that are independent
of the spatial discretisation in numerical analysis.
Numerical analyses of localised failure in quasi-brittle
materials are used to further highlight the features and
applicability of the proposed approach.
The multiple failure mechanisms captured by the proposed model enable the behavior of cemented granular rocks to be well reproduced for a wide range of confining pressures. Furthermore, through comparison of the model predictions and experimental data, the micromechanical basis of the model provides improved understanding of failure mechanisms of cemented granular materials. In particular, we show that grain crushing is the predominant inelastic deformation mechanism under high pressures while cement failure is the relevant mechanism at low pressures. Over an intermediate pressure regime a mixed mode of failure mechanisms is observed. Furthermore, the micromechanical roots of the model allow the effects on localized deformation modes of various initial microstructures to be studied. The results obtained from both the constitutive responses and BVP solutions indicate that the proposed approach and model provide a promising basis for future theoretical studies on cemented granular materials.
accompanied by intensive deformation and irreversible
micro-structural changes of the material in a small but
finite size region. Shear, compaction, and dilation bands
observed in soils and porous rocks are typical examples
of phenomena that lead to localised failure. The width h
of the localisation band has been experimentally shown
to be a physical quantity related to the microstructure
of the material. On the other hand, numerical methods
for the solution of boundary value problems usually
introduce another length scale H, as a result of the
spatial discretisation of the considered domain into
smaller ones over which the constitutive response of
the material is defined in terms of incremental stressstrain
relationships. While h, as a physical quantity,
is fixed, H varies with the resolution of the numerical
discretisation. Since h scales with the material
microstructure and therefore is usually much smaller
than the resolution of the numerical discretisation,
the case H > h is considered in this study, e.g. failure
behaviour governed by a localisation band of width
h embedded in an elastic bulk of nominal side H. We
present a general constitutive modelling framework to
connect these two scales, and corresponding responses
of the materials inside and outside the localisation zone.
We demonstrate how this approach can help obtain
physically meaningful solutions that are independent
of the spatial discretisation in numerical analysis.
Numerical analyses of localised failure in quasi-brittle
materials are used to further highlight the features and
applicability of the proposed approach.