2019
DOI: 10.1680/jgeot.17.p.023
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Grading evolution and critical state in a discrete numerical model of Fontainebleau sand

Abstract: Granular materials reach critical states upon shearing. The position and shape of a critical state line (CSL) in the compression plane are important for constitutive models, interpretation of in situ tests and liquefaction analyses. It is not fully clear how grain crushing may affect the identification and uniqueness of the CSL in granular soils. Discrete-element simulations are used here to establish the relation between breakage-induced grading evolution and the CSL position in the compression plane. An effi… Show more

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Cited by 91 publications
(37 citation statements)
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“…The grain size distribution is also close to that of Fontainebleau sand [66]. More recently, Ciantia et al [17] refined this calibration, using new data to obtain better experimental agreement at very high pressures. The work presented here is not aimed to match laboratory experiments and, for coherence with previous work on response envelopes, the model parameters applied ( Table 1) are those of Ciantia et al [16].…”
Section: Dem Particle Crushing Modelmentioning
confidence: 63%
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“…The grain size distribution is also close to that of Fontainebleau sand [66]. More recently, Ciantia et al [17] refined this calibration, using new data to obtain better experimental agreement at very high pressures. The work presented here is not aimed to match laboratory experiments and, for coherence with previous work on response envelopes, the model parameters applied ( Table 1) are those of Ciantia et al [16].…”
Section: Dem Particle Crushing Modelmentioning
confidence: 63%
“…1). As explained in detail by Ciantia et al [17], this CSL is that relevant to normally consolidated states such as those considered here. The p 0 -constant stress path accelerates the crushing-induced evolution with respect to that observed along the isotropic path ( Fig.…”
Section: Initial Statesmentioning
confidence: 93%
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“…The discrete-element method (DEM), first proposed by Cundall and Strack (1979), is a numerical approach widely used to study fundamental aspects of soil response (Calvetti et al, 2003;Huang et al, 2014b;Ciantia et al, 2016bCiantia et al, , 2018. Typically, small cubic or cylindrical samples are generated to obtain a 'representative elementary volume' (REV), which is later tested to explore different links between micromechanical features and the mesomechanical response of soil.…”
Section: Introductionmentioning
confidence: 99%