A predictive framework for flow liquefaction instabilities in sands is presented. A general criterion for liquefaction, based purely on the laws of physics, is presented and adapted to the important case of radial loading (e.g. triaxial, simple shear) using the Cambridge p′–q plane. Three important contributions are made in the paper. First, the instability concept is unified, and it is shown that the liquefaction criterion coincides with other instability criteria proposed previously. Second, the mechanics triggering liquefaction instabilities are highlighted using a simple instability criterion—underscoring the role of the material state and the underlying constitutive response. Third, the proposed framework is compared with experimental data from samples of sand under undrained triaxial compression, and it is shown that the proposed criterion correctly predicts the onset of liquefaction instability as a function of the sand state. Contractive samples encounter the so-called Lade's instability line, whereas dilative samples do not liquefy, but rather undergo a phase transformation. The predictive nature of the proposed procedure may open the door to better understanding, modelling, prediction and capture of catastrophic instabilities in saturated granular materials under general loading conditions.
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1 October 2009
Research Article|
October 01 2009
A predictive framework for liquefaction instability
J.E. ANDRADE
J.E. ANDRADE
*
* Department of Civil and Environmental Engineering, Northwestern University, Evanston, USA.
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* Department of Civil and Environmental Engineering, Northwestern University, Evanston, USA.
Publisher: Emerald Publishing
Received:
May 03 2007
Accepted:
February 10 2009
Online ISSN: 1751-7656
Print ISSN: 0016-8505
© 2009 Thomas Telford Ltd
2009
Geotechnique (2009) 59 (8): 673–682.
Article history
Received:
May 03 2007
Accepted:
February 10 2009
Citation
ANDRADE J (2009), "A predictive framework for liquefaction instability". Geotechnique, Vol. 59 No. 8 pp. 673–682, doi: https://doi.org/10.1680/geot.7.00087
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