2019
DOI: 10.1007/s10035-019-0915-5
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On the role of pore pressure in dynamic instabilities of saturated model granular materials

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Cited by 7 publications
(8 citation statements)
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“…2. Moreover, we obtained identical results 50 (not presented here) for all the tested confining pressures ranging from 50 to 500 kPa. From all the collected high-resolution measurements (cf.…”
Section: Stick-slip Motions Under Triaxial Compressionsupporting
confidence: 80%
“…2. Moreover, we obtained identical results 50 (not presented here) for all the tested confining pressures ranging from 50 to 500 kPa. From all the collected high-resolution measurements (cf.…”
Section: Stick-slip Motions Under Triaxial Compressionsupporting
confidence: 80%
“…The stick-slip phenomenon, manifested as strong fluctuations of stress and volumetric strain, was not detected in DEM calculations despite several additional runs with an increase/decrease of the spheres number and a reduction of both the grain size and the wall stiffness. To our knowledge, the phenomenon was not detected in any DEM simulations for spherical particles yet [63,64]. There is a suggestion that the stick-slip appears in reality due to physicochemical reactions at grain contacts [63].…”
Section: Calibration Of the Dem Modelmentioning
confidence: 68%
“…Instead of having a usual continuous increase of solid fraction with increasing internal effective stress 18 of real granular media such as natural sands 14 , the isotropic drained compression creates irregular stick-slip-like events termed as isotropic local collapses , 16 , 19 in a sawtooth behaviour in Fig. 1 , beginning from 20 kPa up to an unexpected full destruction of the granular structure at 212 kPa.…”
Section: Resultsmentioning
confidence: 99%
“…The internal stress of the saturated granular structure is greatly reduced by U , according to the Terzaghi effective stress principle, = - U 18 . The last event has a vanishing internal stress accompanied by an exceptionally large incremental axial strain of 19.2% and a jump in solid fraction of 0.018 in one single step in less than 1 s, moving I toward a higher value of about 10 ; hence the dynamic isotropic liquefaction for the slip phase 16 , crossing the jamming transition 21 and the dynamic consolidation for the stick phase 19 . Note the consistent positive delay of pore pressure outburst for all instability events, indicating a surprising counter-intuitive coupled response with systematic constant time delay 22 between the solid and liquid phases for a fully saturated two-phase mixture (Fig.…”
Section: Resultsmentioning
confidence: 99%
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