Abstract

Numerous triaxial tests on sand and sand-like materials have been performed worldwide during the past several decades. Their results provided a development of the advanced soil constitutive models and laboratory testing devices, as well as the establishment of a worldwide database of different types of uniform sandy materials. From such research, the critical state and steady state theory has emerged as one of the most useful tool for the modelling of a soil behaviour. This paper presents the results of static drained tests performed on the uniform Drava River sand from the Osijek region in Croatia. The main aim was to determine the shear behaviour and critical state, given that these characteristics are mostly unknown for the tested sand material. A series of detail triaxial tests were performed in drained conditions for three different initial relative densities, DR, and two different loading directions; e.g., axial compression and axial extension. In total, 18 drained tests were performed. The study indicated that the value of 33.75∘ is the critical friction angle for the tested sand. The relative density of 57% is determined as the critical relative density. Additionally, the study confirmed the difference in critical state for compression and extension loading. In addition, the results indicate that the sample preparation procedure has an important impact on the critical state of loosely prepared sandy samples. These results give the first insights into the behaviour of the Drava River sand, which can generally contribute to the worldwide sand behaviour knowledge base.

Highlights

  • One of the most useful tools and theories for the modelling of soil behaviour is the critical state and steady state theory [1,2,3,4,5,6,7]

  • Stress-strain behaviour for both compression and extension types of tests are presented in Figures 5b, 6b and 7b

  • A series of detail triaxial tests were performed on sand in drained conditions under three different initial relative densities, DR

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Summary

Introduction

One of the most useful tools and theories for the modelling of soil behaviour is the critical state and steady state theory [1,2,3,4,5,6,7]. A soil, by definition, has reached its critical state when the shear strains (γ) or deviatoric strains (eq ) are developing without changes in mean effective stress (p0 ), deviatoric stress (q) and specific volume (v). The critical state of a soil is such a state at which the plastic yielding can constantly develop without the change in deviatoric stress and specific volume at constant mean normal stress (p0 ) [5,6,9]. Such yielding changes an initial soil fabric and structure, by destroying the initial contacts between the grains and rearranging them. Over the several past decades, there have been numerous research of triaxial tests on sand and sand-like materials

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