Stick-slip behaviour of model granular materials in drained triaxial compression

Drained triaxial axisymmetric compression tests are performed on water-saturated short cylindrical samples of nearly monodisperse glass beads, initially assembled in a loose state by a moist tamping technique. Both deviator stress and volumetric strain , measured as functions of axial strain , for d...

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Bibliographic Details
Published inGranular matter Vol. 15; no. 1; pp. 1 - 23
Main Authors Doanh, T., Hoang, M. T., Roux, J.-N., Dequeker, C.
Format Journal Article
LanguageEnglish
Published Berlin/Heidelberg Springer-Verlag 01.02.2013
Springer Nature B.V
Springer Verlag
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Summary:Drained triaxial axisymmetric compression tests are performed on water-saturated short cylindrical samples of nearly monodisperse glass beads, initially assembled in a loose state by a moist tamping technique. Both deviator stress and volumetric strain , measured as functions of axial strain , for different strain rates, are affected by stick-slip events of very large amplitude, while the classical behavior of loose, contractant granular assemblies, approaching the critical state for large , corresponds to the upper envelop of the stress-strain behaviour. Those events consist in a very fast ( slip ) part in which a drop of coincides with a jump of (contraction), while loss of control of and generation of pore pressure signal a dynamic collapse of the material structure triggered by an instability; and then a quasi-static ( stick ) part in which the sample regains its strength and, over a short strain interval, behaves similarly to a denser system that dilates before reaching its critical state. A unique stress-dilatancy relation applies to all stick-slip events. Apparent internal friction angles and effects of strain rate and confining pressure are discussed, and it is argued that stick-slip instabilities originate in physico-chemical aging phenomena coupled to contact mechanics.
Bibliography:ObjectType-Article-2
SourceType-Scholarly Journals-1
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ISSN:1434-5021
1434-7636
DOI:10.1007/s10035-012-0384-6