Viscous behaviour of unbound granular materials in direct shear

被引:42
作者
Duttine, Antoine [1 ]
Tatsuoka, Fumio [1 ]
Kongkitkul, Warat [1 ]
Hirakawa, Dalki [1 ]
机构
[1] Tokyo Univ Sci, Dept Civil Engn, Tokyo 162, Japan
基金
日本学术振兴会;
关键词
direct shear; particle shape; Positive & Negative; rate sensitivity coefficient; stick/slip behaviour; strain/displacement rate; TESRA; unstable behaviour; viscosity; viscous properties (IGC : D6/D7);
D O I
10.3208/sandf.48.297
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
The viscous properties of a variety of poorly graded unbound granular materials were investigated by direct shear tests on 12 cm-cubic specimens. A number of natural sands having different particle shapes and sizes as well as uniform glass beads having different particle sizes were used. The viscous properties were evaluated by changing the shear displacement rate many times during otherwise monotonic loading (ML) at constant shear displacement rate and normal pressure. Creep loadings were performed in two tests. Different types of viscous properties, which are affected by the particle shape but essentially independent of the particle size, are reported. The viscosity type varies as the shear displacement increases from the pre-peak regime towards the residual state. A new viscosity type, called "Positive & Negative", was found with relatively round granular materials in the pre-peak regime and with relatively angular granular materials in the post-peak softening regime and at the residual state. Peculiar "rate-independent unstable behaviour" is observed with round natural sands and glass beads in the post-peak regime, which is more significant and frequent with glass beads. Controlled by the particle size, this behaviour is caused by the so-called stick/slip phenomenon. The viscous properties observed in the DS tests are quantified by the rate-sensitivity coefficient defined in terms of the shear and normal stresses, which are then converted to those defined in terms of the major and minor principal stresses, beta(13). These beta(13) values are consistent with those directly obtained by the triaxial and plane strain compression tests. The effects of particle size on the beta(13) value are negligible and the beta(13) value tends to decrease as the particle shape becomes more round.
引用
收藏
页码:297 / 318
页数:22
相关论文
共 41 条
[1]   Laboratory gouge friction: Seismic-like slip weakening and secondary rate- and state-effects [J].
Chambon, G ;
Schmittbuhl, J ;
Corfdir, A .
GEOPHYSICAL RESEARCH LETTERS, 2002, 29 (10)
[2]  
Cole E.R.L., 1967, Ph. D Thesis
[3]   Exploring the macro- and micro-scale response of an idealised granular material in the direct shear apparatus [J].
Cui, L. ;
O'Sullivan, C. .
GEOTECHNIQUE, 2006, 56 (07) :455-468
[4]  
Davis E.H., 1968, SOIL MECH SELECTED T
[5]  
de Magistris FS, 1999, GEOTECH TEST J, V22, P44
[6]  
Di Benedetto H, 2002, SOILS FOUND, V42, P1
[7]  
DIBENEDETTO H, 2001, P 2 INT S PREF DEF C, V2, P1357
[8]  
DIBENEDETTO H, 2005, P 3 INT S DEF CHAR G, V2, P59
[9]   Anisotropic small strain elastic properties of sands and mixture of sand-clay measured by dynamic and static methods [J].
Duttine, A. ;
Di Benedetto, H. ;
Van Bang, D. Pham ;
Ezaoui, A. .
SOILS AND FOUNDATIONS, 2007, 47 (03) :457-472
[10]  
DUTTINE A, 2006, P 41 JAP S GEOT ENG, P391