Influence of intermediate principal stress and major principal stress direction on the drainage-induced deformation of soft clay

被引:0
|
作者
Guo Lin [1 ]
Wang Yu-ke [2 ]
Wang Jun [1 ]
Zheng Min [3 ]
Wu Ting-yu [4 ]
机构
[1] Wenzhou Univ, Architecture & Civil Engn Coll, Wenzhou 325035, Zhejiang, Peoples R China
[2] Hohai Univ, Coll Civil & Transportat Engn, Nanjing 210098, Jiangsu, Peoples R China
[3] Jiangxi Univ Sci & Technol, Sch Architectural & Surveying & Mapping Engn, Ganzhou 341000, Jiangxi, Peoples R China
[4] Zhejiang Univ, Res Ctr Coastal & Urban Geotech Engn, Hangzhou 310058, Zhejiang, Peoples R China
基金
中国国家自然科学基金;
关键词
intermediate principal stress coefficient; major principal stress direction angle; anisotropy; intact soft clay; drained condition;
D O I
10.16285/j.rsm.2016.05.021
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
In order to evaluate the influence of intermediate principal stress and major principal stress direction on the drainage-induced deformation of natural soft clay, a series of drained directional shear tests is carried out on Wenzhou natural soft clay with different intermediate principal stress coefficients and different major principal stress directional angles, using a GDS hollow cylinder torsional shear apparatus. During the tests, the shear stress is increased gradually until the specimens failed, while the major principal stress direction and the intermediate principal stress coefficient remain unchanged. The influences of intermediate principal stress coefficient and major principal stress direction are discussed on the relationship between the deviator stress and major principal strain, and the relationships between the major principal strain and the intermediate principal strain, minor principal strain and volumetric strain. It is found that the anisotropy expressed by the stress-strain relationship is affected by different intermediate principal stress coefficient and major principal stress direction. When the intermediate principal stress coefficient remains as 0.00 and 1.00, the influence of major principal stress direction on stress-strain relationship is insignificant. However, when the intermediate principal stress coefficient reaches 0.50, the secant modulus in stress-strain relationship is significantly influenced by major principal stress direction. When the major principal stress direction angle is 30 degrees, the intermediate principal strain changes from compressive state to tensile state as the intermediate principal stress coefficient increase from 0.00 to 0.50. When the major principal stress direction angle is 45 degrees, the intermediate principal strain changes from compressive state to tensile state when the intermediate principal stress coefficient increases from 0.00 to 1.00.
引用
下载
收藏
页码:1380 / 1387
页数:8
相关论文
共 17 条
  • [1] GEIGER E, 1979, EXPT STUDY BEHAV COH
  • [2] GUAN Lin-bo, 2010, CHINESE J ROCK MECH, V29, P3871
  • [3] LIQUEFACTION AND FLOW FAILURE DURING EARTHQUAKES
    ISHIHARA, K
    [J]. GEOTECHNIQUE, 1993, 43 (03): : 351 - 415
  • [4] Influences of principal stress direction and intermediate principal stress on the stress-strain-strength behaviour of completely decomposed granite
    Kumruzzaman, Md.
    Yin, Jian-Hua
    [J]. CANADIAN GEOTECHNICAL JOURNAL, 2010, 47 (02) : 164 - 179
  • [5] LADE P V, 2013, J GEOTECH GEOENVIRON, V140, P1
  • [6] LADE PV, 2000, SOILS FOUND, V40, P93, DOI DOI 10.3208/SANDF.40.6_93
  • [7] Miura K., 1986, SOILS FOUND, V26, P36, DOI [10.3208/sandf1972.26.36, DOI 10.3208/SANDF1972.26.36]
  • [8] Nakai T., 1986, SOILS FOUND, V26, P67, DOI DOI 10.3208/SANDF1972.26.4_67
  • [9] Shear strength anisotropy of natural London Clay
    Nishimura, S.
    Minh, N. A.
    Jardine, R. J.
    [J]. GEOTECHNIQUE, 2007, 57 (01): : 49 - 62
  • [10] DRAINED PRINCIPAL STRESS ROTATION IN SATURATED SAND
    SYMES, MJ
    GENS, A
    HIGHT, DW
    [J]. GEOTECHNIQUE, 1988, 38 (01): : 59 - 81