A discrete element analysis of the micromechanical interaction of non-spherical particles in cohesionless granular solids under K$_0$ condition

In: Geomechanics from Micro to Macro - Proceedings of the TC105 ISSMGE International Symposium on Geomechanics from Micro to Macro, IS-Cambridge 2014
Cambridge, UK.


The coefficient of earth pressure at rest K0 is often used to determine the stress state of a soil in the design of retaining walls, excavations and foundations. The most commonly used equation was proposed originally by Jaky (1944) which expresses the ratio of horizontal to vertical stress in a normally consolidated soil as K0 = 1 - sin $\phi$, where $\phi$ is the effective angle of internal friction of the soil. This raises the question as to why the at rest stress state in a soil, which is not at failure, should be governed by the failure friction angle of the soil. The expression is often reported as empirical in nature however, Jaky arrived at the expression from an analytical approach.

This paper explores the micromechanics of cohesionless soils by investigating the effect of soil fabric and the evolution of the lateral pressure under confined compression using the Discrete Element Method (DEM). Many DEM models use spherical particles due to their greater efficiency. However, particle sphericity leads to the over-prediction of the lateral pressure ratio for a typical granular soil during a confined K0 compression test. The lack of particle interlocking that is associated with spherical particles leads to a greater transmission of forces laterally in an assembly under confined compression, resulting in a higher K0 value.

Click the Cite button above to get publication metadata for your reference management software in .bib format.
John P. Morrissey
John P. Morrissey
Research Scientist in Granular Mechanics

My research interests include particulate mechanics, the Discrete Element Method (DEM) and other numerical simulation tools. I’m also interested in all things data and how to extract meaningful information from it.