A unified constitutive model for pressure sensitive shear flow transitions in moderate dense granular materials

Abstract Granular shear flows exhibit complex transitional regimes that are dramatically affected by the pressure level and shear stress state. New advances in granular shear tests at low pressure have enlightened the understanding of the two granular shear flow transitions: between quasi-static and...

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Main Authors: Xiaohui Cheng, Shize Xiao, Alex Sixie Cao, Meiying Hou
Format: Article
Language:English
Published: Nature Publishing Group 2021-10-01
Series:Scientific Reports
Online Access:https://doi.org/10.1038/s41598-021-99006-4
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spelling doaj-ae546a05e10c4ece8136428fe81f96902021-10-10T11:32:07ZengNature Publishing GroupScientific Reports2045-23222021-10-0111111110.1038/s41598-021-99006-4A unified constitutive model for pressure sensitive shear flow transitions in moderate dense granular materialsXiaohui Cheng0Shize Xiao1Alex Sixie Cao2Meiying Hou3Department of Civil Engineering, Tsinghua UniversityDepartment of Civil Engineering, Tsinghua UniversityDepartment of Civil Engineering, Tsinghua UniversityInstitute of Physics, Chinese Academy of ScienceAbstract Granular shear flows exhibit complex transitional regimes that are dramatically affected by the pressure level and shear stress state. New advances in granular shear tests at low pressure have enlightened the understanding of the two granular shear flow transitions: between quasi-static and moderate shear flows, and between steady-state and transient shear flows. However, a unified constitutive model to describe these two transitions is yet to develop. In this work, a simplified and unified model is proposed based on innovative triaxial shear flow tests, using two dimensionless physical variables. Model results validated against experimental data suggest that the shear flow transition between a quasi-static to a moderate Isotach type flow state is highly pressure-dependent. At extremely low pressure, the granular viscosity becomes the primary mechanism, suppressing the quasi-static mechanism even under “quasi-static” shear rates. In transient to steady state granular flow transitions, a mobilized shear stress ratio or mobilized friction coefficient between zero and the critical state ratio for consolidated granular packings is taken into consideration. This is coupled with the mechanism of granular viscosity. These findings have not been discussed before and are of great relevance to granular mechanics as well as space and earthquake engineering.https://doi.org/10.1038/s41598-021-99006-4
collection DOAJ
language English
format Article
sources DOAJ
author Xiaohui Cheng
Shize Xiao
Alex Sixie Cao
Meiying Hou
spellingShingle Xiaohui Cheng
Shize Xiao
Alex Sixie Cao
Meiying Hou
A unified constitutive model for pressure sensitive shear flow transitions in moderate dense granular materials
Scientific Reports
author_facet Xiaohui Cheng
Shize Xiao
Alex Sixie Cao
Meiying Hou
author_sort Xiaohui Cheng
title A unified constitutive model for pressure sensitive shear flow transitions in moderate dense granular materials
title_short A unified constitutive model for pressure sensitive shear flow transitions in moderate dense granular materials
title_full A unified constitutive model for pressure sensitive shear flow transitions in moderate dense granular materials
title_fullStr A unified constitutive model for pressure sensitive shear flow transitions in moderate dense granular materials
title_full_unstemmed A unified constitutive model for pressure sensitive shear flow transitions in moderate dense granular materials
title_sort unified constitutive model for pressure sensitive shear flow transitions in moderate dense granular materials
publisher Nature Publishing Group
series Scientific Reports
issn 2045-2322
publishDate 2021-10-01
description Abstract Granular shear flows exhibit complex transitional regimes that are dramatically affected by the pressure level and shear stress state. New advances in granular shear tests at low pressure have enlightened the understanding of the two granular shear flow transitions: between quasi-static and moderate shear flows, and between steady-state and transient shear flows. However, a unified constitutive model to describe these two transitions is yet to develop. In this work, a simplified and unified model is proposed based on innovative triaxial shear flow tests, using two dimensionless physical variables. Model results validated against experimental data suggest that the shear flow transition between a quasi-static to a moderate Isotach type flow state is highly pressure-dependent. At extremely low pressure, the granular viscosity becomes the primary mechanism, suppressing the quasi-static mechanism even under “quasi-static” shear rates. In transient to steady state granular flow transitions, a mobilized shear stress ratio or mobilized friction coefficient between zero and the critical state ratio for consolidated granular packings is taken into consideration. This is coupled with the mechanism of granular viscosity. These findings have not been discussed before and are of great relevance to granular mechanics as well as space and earthquake engineering.
url https://doi.org/10.1038/s41598-021-99006-4
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