Abstract

This study aims to develop a fundamental understanding of the role of fine particles on the small-strain stiffness of gap-graded granular soils. Stiffness was measured using cyclic triaxial probes, which give a measure of static stiffness, and dynamic wave propagation data, from which the dynamic stiffness can be measured. Assemblies of loosely packed spherical particles were considered. In the laboratory, local deformation transducers were used to measure the static stiffness, while the dynamic stiffness was calculated from stress wave velocities, measured using planar piezoelectric elements. To relate the particle-scale responses to the overall soil stiffness, complementary discrete element method (DEM) simulations were performed in which both static and dynamic stiffnesses were measured. Both the laboratory and the DEM data indicate that at low fines contents (< 30%) the stiffness decreases with increasing fines content. When the fines content increases from 30% to 35% there is a sharp increase in stiffness with increasing fines content; this is understood to mark the transition point at which the fines start to contribute significantly to the overall behaviour. Analyses of the frequency domain response of shear wave signals revealed that the lowpass frequency increases significantly at this transition point. This observation can be used to develop experimental interpretation protocols to assess to what extent fines are contributing to the overall soil stiffness.

Highlights

  • Soil stiffness is a key parameter to predict ground deformation and it is used in earthquake site response analyses

  • Both the laboratory and the Discrete Element Method (DEM) data show that Fc40 gives the largest value of E0sta, while Fc30 exhibits the lowest

  • Discrepancies between the laboratory and DEM data are probably due to differences in e and material segregation; the heterogeneous packing in the laboratory specimens was noted above

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Summary

Introduction

Soil stiffness is a key parameter to predict ground deformation and it is used in earthquake site response analyses. Yang & Liu [5] used mixtures of Toyoura sand and crushed silica fine (χ ≈ 4) and found that G0dyn decreases as Fc increases up to 30%. They prepared the mixtures maintaining an equivalent range of global void ratios (e). Goudarzy et al [10] found a good correlation between eg* and G0dyn for mixtures of large and small spherical glass beads (χ = 10) at Fc ≤ 50% They observed that G0dyn decreases with increasing fines at Fc ≤ 30%; G0dyn increases at 40% ≤ Fc ≤ 50%

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