Abstract

This paper results from an ongoing investigation of the effect of cohesion on the compaction of sheared soft wet granular materials. We compare dry non-cohesive and wet moderately-to-strongly cohesive soft almost frictionless granular materials and report the effect of cohesion between the grains on the local volume fraction. We study this in a three dimensional, unconfined, slowly sheared split-bottom ring shear cell, where materials while sheared are subject to compression under the confining weight of the material above. Our results show that inter-particle cohesion has a considerable impact on the compaction of soft materials. Cohesion causes additional stresses, due to capillary forces between particles, leading to an increase in volume fraction due to higher compaction. This effect is not visible in a system of infinitely stiff particles. In addition, acting oppositely, we observe a general decrease in volume fraction due to increased cohesion for frictional particle, which we attribute to the role of contact friction that enhances dilation.

Highlights

  • We study here the packing fraction in the critical state for non-cohesive to strongly cohesive systems by varying the surface tension of the liquid

  • Note that compression is prevailing for soft particles but is negligible when p∗ > 0 in the limit of infinite stiffness, when the local volume fraction is expected to increase with Bo

  • We studied the local packing fraction of dry and wet granular materials as a function of dimensionless numbers, namely, the inertial number I, the softness p∗ and the Bond number Bo

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Summary

Introduction

We study here the packing fraction in the critical state for non-cohesive to strongly cohesive systems by varying the surface tension of the liquid. Wet granular materials are cohesive and particles can stick together and form local agglomerates or granules, due to formation of clusters of particles for very cohesive systems, as shown in figure 1 and 4(c). It is observed from the figure that some particles form clumps near the surface while the particles near the base are seen through the hollow region. The system is highly inhomogeneous in its spatial distribution

Geometry
Dimensionless numbers
Rheological model
Contact model and parameters
Non-cohesive granular materials
Cohesive granular materials
Effect of cohesion on soft particles
Generalized effect of cohesion
Findings
Discussion
Conclusion
Full Text
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