Abstract
This paper describes patterns of nonlinear shear stiffness degradation with respect to the stress history of clay. An experimental study using undrained triaxial compression tests was conducted on specimens cut from reconstituted clay samples of kaolinite. The nonlinear pattern of stiffness degradation was analyzed within the frameworks of both the conventional overconsolidation ratio (OCR) and the stress path rotation angle. The experimental data were subsequently interpreted based on the concept of the kinematic sub-yield surface. The pattern of stiffness degradation is more relevant to the rotation angle of the current stress path than the OCR value. The sizes of the sub-yield surfaces are variable. Results show that the kinematic movements of sub-yield surfaces within the overall bounding surface may provide an insufficient tool to fully describe the pattern of stiffness degradation.
| Original language | English |
|---|---|
| Pages (from-to) | 309-331 |
| Number of pages | 23 |
| Journal | Marine Georesources and Geotechnology |
| Volume | 31 |
| Issue number | 4 |
| DOIs | |
| Publication status | Published - Oct 2013 |
Bibliographical note
Funding Information:Received 9 November 2011; accepted 12 March 2012. This work was supported by the Integrated Research Institute of Construction and Environmental Engineering at Seoul National University, and the Basic Science Research Program through the National Research Foundation of Korea (NRF) funded by the Ministry of Science (2012-0003341). This support is gratefully acknowledged. Address correspondence to Jinhyun Choo, Department of Civil and Environmental Engineering, Stanford University, Stanford, CA 94305, USA. E-mail: [email protected]
Keywords
- seafloor
- sediments
- surveys
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