TECHNICAL PAPERS
Jun 14, 2002

Influence of Permeability on Liquefaction-Induced Shear Deformation

Publication: Journal of Engineering Mechanics
Volume 128, Issue 7

Abstract

Permeability of a liquefiable soil profile may affect the rate of pore-pressure buildup and subsequent dissipation during and after earthquake excitation. Consequently, effective soil confinement and available resistance to shear deformations may be significantly dependent on permeability in many practical situations. If present, spatial variation in permeability may even have a more profound impact on available overall shear resistance. Indeed, case histories and experimental evidence (shake table and centrifuge tests) suggest that spatial permeability variation in stratified liquefiable deposits can highly influence the nature and extent of associated lateral deformation. In such situations, the onset of liquefaction-induced densification may result in water or water-rich thin interlayers trapped below overlying low-permeability strata. The presence of these low-shear-strength interlayers may trigger excessive (or even unbounded) localized shear deformations (flow failure mechanism). In this paper, numerical modeling is employed in order to investigate the influence of permeability and the spatial variation thereof on liquefaction-induced shear deformations. The involved response characteristics are numerically simulated using a fully coupled two-phase (solid–fluid) Finite Element program.

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Go to Journal of Engineering Mechanics
Journal of Engineering Mechanics
Volume 128Issue 7July 2002
Pages: 720 - 729

History

Received: Oct 18, 2000
Accepted: Oct 15, 2001
Published online: Jun 14, 2002
Published in print: Jul 2002

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Zhaohui Yang, A.M.ASCE
Research Fellow, Dept. of Structural Engineering, Univ. of California, San Diego, La Jolla, CA 92093.
Ahmed Elgamal, M.ASCE
Professor, Dept. of Structural Engineering, Univ. of California, San Diego, La Jolla, CA 92093 (corresponding author).

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