Effects of periodic fluctuations of micro-polar boundary conditions on shear localizations in granular soil-structure interaction
| Autor: | Mustafa I. Alsaleh, Asadollah Noorzad, Babak Ebrahimian |
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| Rok vydání: | 2011 |
| Předmět: |
Materials science
Computational Mechanics Mechanics Granular layer Geotechnical Engineering and Engineering Geology Rigid body Finite element method Void ratio Classical mechanics Shear (geology) Mechanics of Materials Soil structure interaction General Materials Science Boundary value problem Shear band |
| Zdroj: | International Journal for Numerical and Analytical Methods in Geomechanics. 36:855-880 |
| ISSN: | 0363-9061 |
| Popis: | SUMMARY In this work, the interface behavior between an infinite extended narrow granular layer and a rough surface of rigid body is investigated numerically, using finite element method in the updated Lagrangian (UL) frame. In this regard, the elasto-plastic micro-polar (Cosserat) continuum approach is employed to remove the limitations caused by strain-softening of materials in the classical continuum. The mechanical properties of cohesionless granular soil are described with Lade's model enhanced by polar terms, including Cosserat rotations, curvatures, and couple stresses. Furthermore, the mean grain diameter as the internal length is incorporated into the constitutive relations accordingly. Here, the evolution and location of shear band, within the granular layer in contact with the rigid body, are mainly focused. In this regard, particular attention is paid to the effects of homogeneous distribution and periodic fluctuation of micro-polar boundary conditions, prescribed along the interface. Correspondingly, the effects of pressure level, mean grain diameter, and stratified soil are also considered. The finite element results demonstrate that the location and evolution of shear band in the granular soil layer are strongly affected by the non-uniform micro-polar boundary conditions, prescribed along the interface. It is found that the shear band is located closer to the boundary with less restriction of grain rotations. Furthermore, the predicted thickness of shear band is larger for higher rotation resistance of soil grains along the interface, larger mean grain diameter, and higher vertical pressure. Regarding the stratified soil, comprising a thin layer with slightly different initial void ratio, the shear band moves towards the layer with initially higher void ratio. Copyright © 2011 John Wiley & Sons, Ltd. |
| Databáze: | OpenAIRE |
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