Contact-scale insights into the shear stiffness of non-spherical granular materials

Small-strain shear stiffness (G0) is an essential parameter to predict deformation characteristics and dynamic properties of granular materials. It is empirically known that G0 increases with decreasing a void ratio (e0) and increasing isotropic stress level (p0′). Recently, the effect of particle shape on G0 has been studied; however, the mechanism underlying the evolution of G0 is not fully understood. Using the discrete-element method, this contribution quantifies the G0 of granular materials by performing small-strain probing where multi-sphere clumped particles are used to vary particle shape and surface topology systematically. The Hertzian contact theory is applied for each sphere-element contact to capture the stress-dependent contact stiffness. The results reveal that G0 is well correlated with e0 or mean coordination number for a given particle shape; however, G0 is measurably reduced when finer sphere-elements dominate inter-particle contact responses. The present study proposes two contact-scale expressions of G0 for non-spherical particles based on contact area and micromechanical effective medium theory (EMT) by extending the EMT expression for spherical particles; both can capture the effects of particle shape and p0′ on G0 under given conditions where particle breakage does not occur.

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Publication Details

Journal
Géotechnique
Published
2025-02-04
DOI
https://doi.org/10.1680/jgeot.23.00042
Citations
5
Primary Topic
Granular flow and fluidized beds
Type
article
Field-Weighted Citation Impact
6.67
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article

Contact-scale insights into the shear stiffness of non-spherical granular materials

Sadegh Nadimi, Reiko Kuwano, Vasileios Angelidakis, Yang Li et al.
5 citations
Géotechnique
Granular flow and fluidized beds
6.67
article

Contact-scale insights into the shear stiffness of non-spherical granular materials

Sadegh Nadimi, Reiko Kuwano, Vasileios Angelidakis, Yang Li, M. Otsubo
article en
5 citations

Abstract

Small-strain shear stiffness (G0) is an essential parameter to predict deformation characteristics and dynamic properties of granular materials. It is empirically known that G0 increases with decreasing a void ratio (e0) and increasing isotropic stress level (p0′). Recently, the effect of particle shape on G0 has been studied; however, the mechanism underlying the evolution of G0 is not fully understood. Using the discrete-element method, this contribution quantifies the G0 of granular materials by performing small-strain probing where multi-sphere clumped particles are used to vary particle shape and surface topology systematically. The Hertzian contact theory is applied for each sphere-element contact to capture the stress-dependent contact stiffness. The results reveal that G0 is well correlated with e0 or mean coordination number for a given particle shape; however, G0 is measurably reduced when finer sphere-elements dominate inter-particle contact responses. The present study proposes two contact-scale expressions of G0 for non-spherical particles based on contact area and micromechanical effective medium theory (EMT) by extending the EMT expression for spherical particles; both can capture the effects of particle shape and p0′ on G0 under given conditions where particle breakage does not occur.

GéotechniqueVol. 75(11)
Northwestern University (US), Queen's University Belfast (GB), Port and Airport Research Institute (JP), The University of Tokyo (JP), Newcastle University (GB)
Openalex Percentile: Top 4%
Granular flow and fluidized beds
6.67
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