MISC

2003年10月

Three-dimensional elasto-plastic model for unsaturated compacted soils with different initial densities

INTERNATIONAL JOURNAL FOR NUMERICAL AND ANALYTICAL METHODS IN GEOMECHANICS
  • DA Sun
  • ,
  • H Matsuoka
  • ,
  • HB Cui
  • ,
  • YF Xu

27
12
開始ページ
1079
終了ページ
1098
記述言語
英語
掲載種別
DOI
10.1002/nag.313
出版者・発行元
JOHN WILEY & SONS LTD

This paper presents an elasto-plastic model for unsaturated compacted soils and experimental results obtained from a series of suction-controlled triaxial tests on unsaturated compacted clay with different initial densities. The initial density dependency of the compacted soil behaviour is modelled by establishing experimental relationships between the initial density and the corresponding yield stress and thereby between the initial density and the location and slope of normal compression line. The model is generalized to three-dimensional stress states by assuming that the shapes of the failure surface and the yield surface in the deviatoric plane are given by the extended SMP criterion. A considerable number of the isotropic compression, triaxial compression and extension tests on unsaturated compacted clay with different initial densities were performed using a suction-controllable triaxial apparatus, to measure the stress-strain-volume change in different stress paths and wetting paths. The model has well-predicting capabilities to reproduce the mechanical behaviour of specimens compacted under different conditions not only in isotropic compression but also in triaxial compression and triaxial extension. Copyright (C) 2003 John Wiley Sons, Ltd.

リンク情報
DOI
https://doi.org/10.1002/nag.313
CiNii Articles
http://ci.nii.ac.jp/naid/80016271124
Web of Science
https://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcAuth=JSTA_CEL&SrcApp=J_Gate_JST&DestLinkType=FullRecord&KeyUT=WOS:000185659200006&DestApp=WOS_CPL
ID情報
  • DOI : 10.1002/nag.313
  • ISSN : 0363-9061
  • CiNii Articles ID : 80016271124
  • Web of Science ID : WOS:000185659200006

エクスポート
BibTeX RIS