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On the role of microstructure in the behavior of soils: Effects of higher order gradients and internal inertia

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dc.contributor.author Vardoulakis, I en
dc.contributor.author Aifantis, EC en
dc.date.accessioned 2014-03-01T01:10:00Z
dc.date.available 2014-03-01T01:10:00Z
dc.date.issued 1994 en
dc.identifier.issn 0167-6636 en
dc.identifier.uri https://dspace.lib.ntua.gr/xmlui/handle/123456789/11294
dc.subject Microstructures en
dc.subject Higher Order en
dc.subject.classification Materials Science, Multidisciplinary en
dc.subject.classification Mechanics en
dc.subject.other Crystals en
dc.subject.other Dislocations (crystals) en
dc.subject.other Flow of fluids en
dc.subject.other Plasticity en
dc.subject.other Soil mechanics en
dc.subject.other Soils en
dc.subject.other Solids en
dc.subject.other Strain en
dc.subject.other Stresses en
dc.subject.other Back stress en
dc.subject.other Complete balance laws en
dc.subject.other Crystal plasticity en
dc.subject.other Darcy's law en
dc.subject.other Internal momentum balance equation en
dc.subject.other Shear banding en
dc.subject.other Soil plasticity en
dc.subject.other Strain gradient en
dc.subject.other Microstructure en
dc.title On the role of microstructure in the behavior of soils: Effects of higher order gradients and internal inertia en
heal.type journalArticle en
heal.identifier.primary 10.1016/0167-6636(94)00002-6 en
heal.identifier.secondary http://dx.doi.org/10.1016/0167-6636(94)00002-6 en
heal.language English en
heal.publicationDate 1994 en
heal.abstract The role of microstructure in the behavior of soils is outlined by considering two typical examples: fluid flow and shear banding. In particular, the modifications resulting on Darcy's law and flow rule of soil plasticity due to the development of high strain gradients and internal inertia are discussed. This is done by resorting to ""complete balance laws"" for the internal variables. In the case of Darcy's law, the ""internal"" variable is an interaction stress between the porous solid and the interpenetrating fluid phase, which is required to obey an internal momentum balance equation. In the case of flow rule, the ""internal"" variable is the so-called back stress which is also required to obey a complete balance law containing both a rate and flux term. © 1994. en
heal.publisher ELSEVIER SCIENCE BV en
heal.journalName Mechanics of Materials en
dc.identifier.doi 10.1016/0167-6636(94)00002-6 en
dc.identifier.isi ISI:A1994NY71900007 en
dc.identifier.volume 18 en
dc.identifier.issue 2 en
dc.identifier.spage 151 en
dc.identifier.epage 158 en


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