Proceedings of GeoShanghai 2018 International Conference: Fundamentals of Soil Behaviours 2018
DOI: 10.1007/978-981-13-0125-4_92
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Exploring Grading-Dependency of Deformation Modulus of Loose Aggregates of Spherical Particles Using DEM

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Cited by 2 publications
(8 citation statements)
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“…Unlike the typical nonlinear e‐p curves obtained from laboratory, the void ratio obtained from the simulations linearly decreases with the increase of the mean stress for all samples. The linear e ‐ p relation was also consistently revealed in three‐dimensional DEM simulations of isotropic compression tests 9,62 and confined compression tests 13,33 . This phenomenon could be attributed to the lack of particle breakage in the simulations.…”
Section: Resultssupporting
confidence: 62%
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“…Unlike the typical nonlinear e‐p curves obtained from laboratory, the void ratio obtained from the simulations linearly decreases with the increase of the mean stress for all samples. The linear e ‐ p relation was also consistently revealed in three‐dimensional DEM simulations of isotropic compression tests 9,62 and confined compression tests 13,33 . This phenomenon could be attributed to the lack of particle breakage in the simulations.…”
Section: Resultssupporting
confidence: 62%
“…[26] for quantifying the fabric of granular materials at a particular stress level, it is computed as: VWCN=1Vp=1NVpCpwhere V is the total volume of a sample composed of N particles with more than one contacts; and V p and C p are the volume and contact number of the p th particle, respectively. Our previous study 9 suggested that VWCN strongly connects to the space filling properties of granular materials. The strong I G ‐VWCN correlation could explain the good performance of I G in describing the variation of the reference void ratio (see Figure 9A).…”
Section: Resultsmentioning
confidence: 96%
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“…These contradictory findings led to different empirical prediction models for the small-strain shear modulus, suggesting that the D50 and Cu, derived respectively from only one and two points on a GSD curve, is too crude to characterize size polydispersity. Moreover, in some cases where the GSD is highly truncated [9,10], d10 or even d60 can often not be determined and Cu cannot be calculated. Although some other descriptors are developed to better characterize size polydispersity, such as the moments of GSD [11,12], and the breakage potential defined from the area under a GSD curve [13,14], their validity in the gradationdependent correlations requires further investigations.…”
Section: Introductionmentioning
confidence: 99%