›› 2016, Vol. 37 ›› Issue (5): 1380-1387.doi: 10.16285/j.rsm.2016.05.021

• Fundamental Theroy and Experimental Research • Previous Articles     Next Articles

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

GUO Lin1, WANG Yu-ke2, WANG Jun1, ZHENG Min3, WU Ting-yu4   

  1. 1. Architecture and Civil Engineering College, Wenzhou University, Wenzhou, Zhejiang 325035, China; 2. College of Civil & Transportation Engineering, Hohai University, Nanjing, Jiangsu 210098, China; 3. School of Architectural and Surveying & Mapping Engineering, Jiangxi University of Science and Technology, Ganzhou, Jiangxi 341000, China; 4. Research Center of Coastal and Urban Geotechnical Engineering of Zhejiang University, Hangzhou, Zhejiang 310058, China
  • Received:2015-06-03 Online:2016-05-10 Published:2018-06-09
  • Supported by:

    This work was supported by National Natural Science Foundation of China(51408441), Natural Science Foundation of Zhejiang Province(LQ14E080011) and the Program for Innovation Research Team of Zhejiang Province(2011R50020).

Abstract: 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°, 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°, the intermediate principal strain changes from compressive state to tensile state when the intermediate principal stress coefficient increases from 0.00 to 1.00.

Key words: intermediate principal stress coefficient, major principal stress direction angle, anisotropy, intact soft clay, drained condition

CLC Number: 

  • TU 432

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