2008
DOI: 10.1680/geot.2008.58.4.237
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Quantifying and modelling fabric anisotropy of granular soils

Abstract: entes combinaisons de charges et de préparation des échantillons. On démontre que le modèle est en mesure de simuler, de façon harmonisée, les résultats expérimentaux reflétant les effets conjugués des méthodes de préparation des échantillons, des chemins de charge, de la densité du sol, et des pressions de confinement.

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Cited by 252 publications
(107 citation statements)
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“…Because we are interested in dense aggregates of frictional particles, we require that the solid volume fraction φ is close to the random close packing value φ RCP 0.64. It is well known that different packing structures are obtained experimentally according to the preparation protocol [17,18]. Our approach is to generate numerical packings with different final structure.…”
Section: Numerical Simulationmentioning
confidence: 99%
See 1 more Smart Citation
“…Because we are interested in dense aggregates of frictional particles, we require that the solid volume fraction φ is close to the random close packing value φ RCP 0.64. It is well known that different packing structures are obtained experimentally according to the preparation protocol [17,18]. Our approach is to generate numerical packings with different final structure.…”
Section: Numerical Simulationmentioning
confidence: 99%
“…Conventional approaches in the framework of solid-state elasticity consider the response to be dependent on the solid volume fraction and the stress state. On the other hand, micromechanics has supported the idea that along with macroscopic properties, the response of an aggregate is characterized by the fabric tensors and the coordination number [13,14,8,18]. The former refers to the geometric arrangement of the contacts, the latter is the (scalar) average number of contacts per particle.…”
Section: Introductionmentioning
confidence: 99%
“…Fabric anisotropic effects were studied on sandy soil responses by a series of experimental studies (Yu et al, 2013;Guo and Zhao, 2013;Louis et al, 2009 between microscopic and macroscopic structures Yang et al, 2008;Yang et al, 2013;Hicher and Chang, 2007;Kruyt and Rothenburg, 2016;Khalili and Mahboubi, 2014;Voiadjis et al, 1995;Kruyt and Rothenburg, 2014;Guo, 2014;Li and Yu, 2014;Yan, 2009;Chang and Hicher, 2005). Other studies have been conducted to predict the fabric anisotropic behaviour using different parameters and placing them in equations of constitutive model of soil (Yu et al, 2013;Yang et al, 2008;Gao et al, 2014;Dafalias and Manzari, 2004;Lashkari, 2009;Zhao and Guo, 2013;.…”
Section: Introductionmentioning
confidence: 99%
“…Other studies have been conducted to predict the fabric anisotropic behaviour using different parameters and placing them in equations of constitutive model of soil (Yu et al, 2013;Yang et al, 2008;Gao et al, 2014;Dafalias and Manzari, 2004;Lashkari, 2009;Zhao and Guo, 2013;. In addition, a few studies have been conducted to consider the effect of induced anisotropy by using constitutive models (Hareb and Doanh, 2012;Tang Tron Tran et al, 2014;Ye et al, 2012).…”
Section: Introductionmentioning
confidence: 99%
“…Quartzitic sands recovered from river beds and coastal areas, for example, tend to be poorly graded (Ham River sand (Coop, 2003), Toyoura sand (Yang et al, 2008), Hostun sand (De Gennaro et al, 2004)), while some granular soils which result from in-situ erosion, for example decomposed granite (Lee and Coop, 1995), or some residual soils (Ferreira and Bica, 2006), are more likely to have well-distributed (poorly-sorted) particles sizes. Subglacial sediments, which also tend to be well graded, were transported and deposited by ice, and unlike any other sediment they were subjected to incessant shearing while depositing (Benn and Evans, 1998), with crushing and grinding at interparticle and particle-bed level (Boulton et al, 1974).…”
Section: Introductionmentioning
confidence: 99%