TECHNICAL PAPERS
Sep 1, 1990

Double‐Yield‐Surface Model. II: Implementation and Verification

Publication: Journal of Geotechnical Engineering
Volume 116, Issue 9

Abstract

A double‐yield‐surface constitutive model for the stress‐strain‐time behavior of cohesive soils is implemented into a nonlinear finite element program based on Biot's three‐dimensional consolidation theory. The coupled soil deformation‐fluid flow model allows creep effects to be modeled concurrently. The soil's hydraulic conductivity is considered a state variable, which varies with the void ratio so that it decreases as the soil compacts. Parametric, laboratory, and field‐case studies are performed on various cohesive soils such as Weald clay, undisturbed bay mud, and Boston blue clay to validate the model. Numerical simulations include drained, undrained, consolidation, creep, stress‐relaxation, and combined stress‐relaxation and creep tests under triaxial and plane‐strain stress conditions. The constitutive model is shown to predict the stress‐strain‐time behavior of “wet” clays more accurately than did an earlier version based on a single‐yield‐surface criterion.

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Go to Journal of Geotechnical Engineering
Journal of Geotechnical Engineering
Volume 116Issue 9September 1990
Pages: 1402 - 1421

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Published online: Sep 1, 1990
Published in print: Sep 1990

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Authors

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R. I. Borja
Asst. Prof., Dept. of Civ. Engrg., Stanford Univ., Stanford, CA 94305
H. S. Hsieh
Sr. Geotech. Engr., Moh and Assoc., 8th floor, 131, Nanking East Rd., Sec. 3, Taipei, Taiwan
E. Kavazanjian, Jr., Associate Members, ASCE
Assoc., The Earth Tech. Corp., 100 West Broadway, Suite 5000, Long Beach, CA 90802

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