Materials with a granular microstructure frequently fail in narrow zones due to strain localisation. Examplarily, one may look at the shear-zone development in dry sand during bi-and triaxial loading, where grains in the shear-zone exhibit large displacements and rotations. Furthermore, localisation is also observed in materials, where the microstructure consists of grains and a binding material, such as for example metal-casting moulds. Here, sand grains are bound together via a polyurethanbased material and macroscopic material failure originates from the deformation and breakage of the binder material. Within a continuum-based modelling approach, these microstructural effects can be accounted for by the consideration of an additional microcontinuum at each material point of the macroscopic body. These extended continuum theories, such as the micromorphic continua and its micropolar and microstrain sub-formulations, assume a characteristic microcontinuum deformation on a lower scale and have been successfully applied in the field of granular media. Exemplarily, in the framework of a micropolar continua, it is possible to contact forces to stresses and couple stresses via an appropriate homogenisation technique. This method includes the introduction of a Representative Elementary Volume (REV) on the mesoscale situated between the particle and the continuum scale. In this contribution, a homogenisation strategy based on a particle-centre-based REV definition is presented that is generally valid for micromorphic and micropolar continua. Therefore, a grain-binder microstructure is investigated, where particle rotations contribute to the micropolar part, while binder deformations yield the additional macromorphic character. Numerical examples are given, where results from discrete-element simulations are locally averaged and show the individual activation of the microcontinuum characteristics in the localised zones.
Homogenisation strategyA Representative Elementary Volume R is introduced on the mesoscale located between the macroscale of the overall body and the microscale of the particles. Thereby, an ensemble of particles forms the REV and its boundary is defined by the connection of the centres of mass of the boundary particles. Evaluating the balances of momentum and moment of momentum of a REV in an equilibrium state reveals its micropolar character, as surface couplesm arise due to the shifting of the surface stress vector t towards the particle's centre of mass at the REV-boundary, compare [1] for details. The stress state is hence described by non-symmetric stresses T and couple stressesM. This is the case for unbonded and bonded granular materials, as there is no formal difference whether contact stresses arise from direct collision of particles at contact points or from binder-material bridges that cover a larger surface area of the particles. The microstress that is associated with binder deformations in the REV is therefore identified through evaluation of the principle of virtual work [2], where the ...