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contributor authorTomáš Janda
contributor authorPavel Kuklik
contributor authorMichal Šejnoha
date accessioned2017-05-08T21:31:48Z
date available2017-05-08T21:31:48Z
date copyrightSeptember 2004
date issued2004
identifier other%28asce%291532-3641%282004%294%3A3%28199%29.pdf
identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/54975
description abstractThe present contribution reports on a mixed numerical experimental study of the time dependent processes in saturated soils with reference to isotropic consolidation. Owing to its relative simplicity, isotropic consolidation is often viewed as a basic tool for inferring the material parameters of various constitutive models. Within this modeling framework, the paper advocates the use of critical state models for an accurate description of the time dependent deformation of clayey soils. Material models, in which the critical state model applies only to the subcritical region, have been also addressed. Examples include models where the supercritical region is cut off, e.g., by a Mohr–Coulomb surface. Starting with the modified Cam clay model, as a classical representative, the paper revisits a simple isotropic consolidation test. It is suggested that such a conventional laboratory experiment, when combined with a suitable optimization procedure, is sufficient in deriving the desired material parameters, including the initial void ratio, deformation dependent variation of the coefficient of permeability and the preconsolidation pressure representing here an important measure of the structural strength of soils. Several numerical and experimental results are presented to support the theoretical grounds.
publisherAmerican Society of Civil Engineers
titleMixed Experimental and Numerical Approach to Evaluation of Material Parameters of Clayey Soils
typeJournal Paper
journal volume4
journal issue3
journal titleInternational Journal of Geomechanics
identifier doi10.1061/(ASCE)1532-3641(2004)4:3(199)
treeInternational Journal of Geomechanics:;2004:;Volume ( 004 ):;issue: 003
contenttypeFulltext


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