Inclusion of specific water volume within an elasto-plastic model for unsaturated soil

被引:114
作者
Wheeler, SJ
机构
[1] Department of Civil Engineering, University of Glasgow, Rankine Building, Glasgow
关键词
compacted clays; constitutive model; critical state; elasto-plasticity; triaxial tests; unsaturated;
D O I
10.1139/t96-023
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
Existing elasto-plastic critical state constitutive models for unsaturated soil provide no information on the variation of water content or degree of saturation. These models cannot therefore, for example, be used to predict unsaturated soil behaviour during undrained loading, when the variation of suction is determined by the requirement that water content remains constant. This problem has been tackled by extending an existing elastoplastic model to include relationships describing the variation of specific water volume (the volume of water and solids in an element of soil containing unit volume of solids). The proposed form of the variation of specific water volume was based on consideration of the soil fabric, resulting in a coupled form of elasto-plastic behaviour. Predictions from the elasto-plastic model showed good agreement with experimental results from suction-controlled triaxial tests on unsaturated samples of compacted speswhite kaolin. Normal compression lines for specific water volume at different values of suction were well predicted, as was the variation of specific water volume during wetting. Critical state values of specific water volume were slightly underestimated, but test paths for both drained and undrained shearing were predicted with reasonable success.
引用
收藏
页码:42 / 57
页数:16
相关论文
共 24 条
[1]   A CONSTITUTIVE MODEL FOR PARTIALLY SATURATED SOILS [J].
ALONSO, EE ;
GENS, A ;
JOSA, A .
GEOTECHNIQUE, 1990, 40 (03) :405-430
[2]  
ALONSO EE, 1987, 9TH P EUR C SOIL MEC, V3, P1087
[3]  
Bishop A.W., 1963, GEOTECHNIQUE, V13, P177, DOI DOI 10.1680/GEOT.1963.13.3.177
[4]  
CRONEY D, 1952, GEOTECHNIQUE, V3, P1, DOI DOI 10.1680/GEOT.1952.3.1.1
[5]  
CUI YJ, 1995, P 1 INT C UNS SOILS, V2, P703
[6]   THE SHEAR-STRENGTH OF PARTLY SATURATED SOILS [J].
ESCARIO, V ;
SAEZ, J .
GEOTECHNIQUE, 1986, 36 (03) :453-456
[7]   CONSTITUTIVE RELATIONS FOR VOLUME CHANGE IN UNSATURATED SOILS [J].
FREDLUND, DG ;
MORGENSTERN, NR .
CANADIAN GEOTECHNICAL JOURNAL, 1976, 13 (03) :261-276
[8]   DIFFUSED AIR VOLUME INDICATOR FOR UNSATURATED SOILS [J].
FREDLUND, DG .
CANADIAN GEOTECHNICAL JOURNAL, 1975, 12 (04) :533-539
[9]   SHEAR-STRENGTH OF UNSATURATED SOILS [J].
FREDLUND, DG ;
MORGENSTERN, NR ;
WIDGER, RA .
CANADIAN GEOTECHNICAL JOURNAL, 1978, 15 (03) :313-321
[10]  
FREDLUND DG, 1977, ASCE J GEOTECHNICAL, V103, P447