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| Experimental and theoretical study on elastoplastic behavior of saturated saline clay |
| ZHOU Fengxi1,WANG Liye1,2,WAN Xusheng3,LIANG Yuwang1,YE Weilin2 |
| (1. School of Civil Engineering,Lanzhou University of Technology,Lanzhou,Gansu 730050,China;3. Institute of Geology of Natural Disaster Prevention,Gansu Academy of Sciences,Lanzhou,Gansu 730000,China;3. School of Civil Engineering and Architecture,Southwest Petroleum University,Chengdu,Sichuan 610500,China) |
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Abstract A series of triaxial compression tests involving saline condition and degree of overconsolidation are carried out to investigate the influence of type and concentration of pore solution and overconsolidation ratio(OCR) on the stress-strain curve,dilatancy behavior and other mechanical properties of saturated clay. The test results indicate that the change of the type and concentration of pore solution can change the degree of overconsolidation,deformation capacity,dilatancy ratio and slope of critical state line of clay,but it has little effect on the elastic modulus. Therefore,a new chemo-elastoplastic model is established based on UH model to simulate mechanical behavior of saturated saline clay. This model considers the impact of osmotic suction on clay?s mechanical properties and can describe its stress-strain behavior under different saline conditions. The new model introduces equivalent stress to define osmotic suction?s contribution and presents a chemical elasticity theory for saturated saline clay. Additionally,the yield surface,hardening modulus,stress-dilatancy equation and constitutive relation of saturated saline clay are derived by considering osmotic suction effects. It is observed that increasing osmotic suction leads to a“shorter and fatter”yield surface in three-dimensional stress space for saturated saline clay while reducing overconsolidation degree but increasing dilatancy ratio gradually. The universality and prediction ability of this model are verified by simulation and comparative analysis of test results of saturated saline clay under different osmotic suction.
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