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  • Incorporation of void ratio as a state variable into constitutive models allows, in principle, to use a single set of material parameters for soils with different degrees of overconsolidation. p constant experiments by Hattab and Hicher (2004) on soils with overconsolidation ratios (OCR) ranging from I to 50 are used for evaluation of three constitutive models of different complexity. It is demonstrated by means of a scalar error measure and stress-strain diagrams that at least two sets of parameters for different OCR intervals should be used. Further, advanced models perform significantly better than the Modified Cam clay model and a hypoplastic model for clays leads to better predictions than elasto-plastic three surface kinematic hardening model.
  • Incorporation of void ratio as a state variable into constitutive models allows, in principle, to use a single set of material parameters for soils with different degrees of overconsolidation. p constant experiments by Hattab and Hicher (2004) on soils with overconsolidation ratios (OCR) ranging from I to 50 are used for evaluation of three constitutive models of different complexity. It is demonstrated by means of a scalar error measure and stress-strain diagrams that at least two sets of parameters for different OCR intervals should be used. Further, advanced models perform significantly better than the Modified Cam clay model and a hypoplastic model for clays leads to better predictions than elasto-plastic three surface kinematic hardening model. (en)
Title
  • An evaluation of constitutive models to predict the behaviour of fine-grained soils with different degrees of overconsolidation
  • An evaluation of constitutive models to predict the behaviour of fine-grained soils with different degrees of overconsolidation (en)
skos:prefLabel
  • An evaluation of constitutive models to predict the behaviour of fine-grained soils with different degrees of overconsolidation
  • An evaluation of constitutive models to predict the behaviour of fine-grained soils with different degrees of overconsolidation (en)
skos:notation
  • RIV/00216208:11310/06:9792!RIV11-AV0-11310___
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • P(IAA200710605), Z(AV0Z20710524)
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
http://linked.open.../riv/druhVysledku
http://linked.open...iv/duvernostUdaju
http://linked.open...titaPredkladatele
http://linked.open...dnocenehoVysledku
  • 464793
http://linked.open...ai/riv/idVysledku
  • RIV/00216208:11310/06:9792
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • overconsolidation ratio; constitutive models; clays (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...ontrolniKodProRIV
  • [0221530EA003]
http://linked.open...v/mistoKonaniAkce
  • Graz, Austria
http://linked.open...i/riv/mistoVydani
  • Leiden, The Netherlands
http://linked.open...i/riv/nazevZdroje
  • Numerical methods in geotechnical engineering
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...vavai/riv/projekt
http://linked.open...UplatneniVysledku
http://linked.open...iv/tvurceVysledku
  • Mašín, David
  • Hájek, Václav
http://linked.open...vavai/riv/typAkce
http://linked.open.../riv/zahajeniAkce
http://linked.open...n/vavai/riv/zamer
number of pages
http://purl.org/ne...btex#hasPublisher
  • Taylor & Francis Group plc
https://schema.org/isbn
  • 0-415-40822-9
http://localhost/t...ganizacniJednotka
  • 11310
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