A non-local constitutive model for slow granular flow that incorporates dilatancy
Over the past two decades several attempts have been made to formulate constitutive models for slow granular flow to remedy the deficiencies of classical plasticity. All the proposed models assume the medium to be incompressible, though it is well known that density change accompanies deformation in...
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Published in | Journal of fluid mechanics Vol. 888 |
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Main Authors | , |
Format | Journal Article |
Language | English |
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Cambridge University Press
10.04.2020
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Abstract | Over the past two decades several attempts have been made to formulate constitutive models for slow granular flow to remedy the deficiencies of classical plasticity. All the proposed models assume the medium to be incompressible, though it is well known that density change accompanies deformation in granular materials. A particularly important aspect of density change that is distinctive of granular materials is dilatancy, or volume deformation caused by shear deformation. No constitutive model for sustained flow has thus far captured dilatancy. Here we present a non-local constitutive model wherein the deformation rate and density at a point depend on the state of stress in a mesoscopic region around it. Apart from incorporating dilatancy, our model has a physical origin that is distinct from that of the previously proposed non-local models. We test our model on simple shear flow in the absence and presence of gravity, and find its predictions to be in good agreement with particle dynamics simulations. |
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AbstractList | Over the past two decades several attempts have been made to formulate constitutive models for slow granular flow to remedy the deficiencies of classical plasticity. All the proposed models assume the medium to be incompressible, though it is well known that density change accompanies deformation in granular materials. A particularly important aspect of density change that is distinctive of granular materials is dilatancy, or volume deformation caused by shear deformation. No constitutive model for sustained flow has thus far captured dilatancy. Here we present a non-local constitutive model wherein the deformation rate and density at a point depend on the state of stress in a mesoscopic region around it. Apart from incorporating dilatancy, our model has a physical origin that is distinct from that of the previously proposed non-local models. We test our model on simple shear flow in the absence and presence of gravity, and find its predictions to be in good agreement with particle dynamics simulations. Over the past two decades several attempts have been made to formulate constitutive models for slow granular flow to remedy the deficiencies of classical plasticity. All the proposed models assume the medium to be incompressible, though it is well known that density change accompanies deformation in granular materials. A particularly important aspect of density change that is distinctive of granular materials is dilatancy, or volume deformation caused by shear deformation. No constitutive model for sustained flow has thus far captured dilatancy. Here we present a non-local constitutive model wherein the deformation rate and density at a point depend on the state of stress in a mesoscopic region around it. Apart from incorporating dilatancy, our model has a physical origin that is distinct from that of the previously proposed non-local models. We test our model on simple shear flow in the absence and presence of gravity, and find its predictions to be in good agreement with particle dynamics simulations. |
ArticleNumber | R3 |
Author | Dsouza, Peter Varun Nott, Prabhu R. |
Author_xml | – sequence: 1 givenname: Peter Varun surname: Dsouza fullname: Dsouza, Peter Varun – sequence: 2 givenname: Prabhu R. orcidid: 0000-0003-0656-2648 surname: Nott fullname: Nott, Prabhu R. |
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Cites_doi | 10.1103/PhysRevLett.106.108301 10.1017/S0022112002007796 10.1103/PhysRevLett.95.068003 10.1098/rspa.2016.0846 10.1016/B978-0-12-493120-6.50018-0 10.1017/S0022112008002358 10.1017/S0022112095004320 10.1007/s00707-009-0166-3 10.1103/PhysRevLett.109.128002 10.1038/35019032 10.1017/jfm.2011.251 10.1016/0020-7225(83)90058-7 10.1038/nature03805 10.1063/1.4812800 10.1103/PhysRevLett.111.238301 10.1016/0009-2509(88)87009-X 10.1103/PhysRevLett.85.1428 10.1017/S0022112092001976 10.1017/jfm.2017.651 10.1016/S0032-5910(02)00132-8 10.1080/14786448508627791 10.1038/ncomms10630 10.1103/PhysRevLett.102.228301 10.1073/pnas.1219153110 10.1016/0032-5910(80)87014-8 10.1007/BF01179543 10.1017/jfm.2017.612 10.1038/nature04801 10.1017/jfm.2015.412 10.1017/CBO9780511611513 10.1103/PhysRevLett.113.178001 10.1103/PhysRevLett.103.036001 10.1680/geot.1996.46.3.529 |
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SubjectTerms | Computational fluid dynamics Computer simulation Constitutive models Deformation Deformation mechanisms Density Dilatancy Granular materials Gravity Mathematical models Model testing Shear deformation Shear flow |
Title | A non-local constitutive model for slow granular flow that incorporates dilatancy |
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