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Gradient dependent dilatancy and its implications in shear banding and liquefaction

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dc.contributor.author Vardoulakis, I en
dc.contributor.author Aifantis, E en
dc.date.accessioned 2014-03-01T01:07:29Z
dc.date.available 2014-03-01T01:07:29Z
dc.date.issued 1989 en
dc.identifier.uri https://dspace.lib.ntua.gr/xmlui/handle/123456789/10018
dc.subject Deformation Theory en
dc.subject Length Scale en
dc.subject Shear Bands en
dc.title Gradient dependent dilatancy and its implications in shear banding and liquefaction en
heal.type journalArticle en
heal.identifier.primary 10.1007/BF00532250 en
heal.identifier.secondary http://dx.doi.org/10.1007/BF00532250 en
heal.publicationDate 1989 en
heal.abstract A gradient dependent dilatancy condition is assumed in order to capture the heterogeneous character of deformation in granular soils. This assumption is incorporated into the structure of classical deformation and flow theories of plasticity and its implications in two interesting examples of patterning instability, that is shear banding and liquefaction, are examined. Shear banding is considered within a modified gradient en
heal.journalName Archive of Applied Mechanics en
dc.identifier.doi 10.1007/BF00532250 en


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