Interpretation of micromorphic constitutive relations for porous materials at the microscale via harmonic decomposition

TL;DR

This paper uses harmonic decomposition and microscale homogenization to interpret the 18 constitutive parameters of micromorphic theory for porous materials, linking them to size effects and validating predictions with experiments.

Contribution

It provides a clear interpretation of micromorphic constitutive parameters through harmonic analysis and microscale modeling, enhancing understanding of size effects in porous materials.

Findings

Closed-form expressions for all 18 parameters derived

Predicted size effects match experimental results

Harmonic decomposition clarifies parameter roles

Abstract

Micromorphic theories became an established tool to model size effects in materials like dispersion, localization phenomena or (apparently) size dependent properties. However, the formulation of adequate constitutive relations with its large number of constitutive relations and respective parameters hinders the usage of the full micromorphic theory, which has 18 constitutive parameters already in the isotropic linear elastic case. Although it is clear that these parameters are related to predicted size effects, the individual meaning of single parameters has been rather unclear. The present work tries to elucidate the interpretation of the constitutive relations and their parameters. For this purpose, a harmonic decomposition is applied to the governing equations of micromorphic theory. The harmonic modes are interpreted at the microscale using a homogenization method for a simple volume element with spherical pore. The resulting boundary-value problem at the microscale is solved analytically for the linear-elastic case using spherical harmonics resulting in closed-form expressions for all of the elastic 18 parameters. These values are used to predict the size effect in torsion of slender foam specimens. The predictions are compared with respective experimental results from literature.