Rock and Soil Mechanics ›› 2025, Vol. 46 ›› Issue (7): 2071-2084.doi: 10.16285/j.rsm.2024.1265

• Fundamental Theory and Experimental Research • Previous Articles     Next Articles

Mechanical response and constitutive modeling of frozen calcareous clay under complex multi-axial stress paths

CAO Yi1, 2, 3, RONG Chuan-xin2, 3, WANG Yan-sen1, CHANG Lei2, 3, WANG Bin2, 3   

  1. 1. State Key Laboratory of Intelligent Construction and Healthy Operation & Maintenance of Deep Underground Engineering, China University of Mining & Technology, Xuzhou, Jiangsu 221116, China; 2. Engineering Research Center of Underground Mine Construction, Ministry of Education, Anhui University of Science and Technology, Huainan, Anhui 221116, China; 3. School of Civil Engineering and Architecture, Anhui University of Science and Technology, Huainan, Anhui 232001, China
  • Received:2024-10-14 Accepted:2025-03-03 Online:2025-07-10 Published:2025-07-08
  • Supported by:
    This work was supported by the National Natural Science Foundation of China (51878005, 52074264), the Open Fund for Engineering Research Center of Underground Mine Construction, Ministry of Education (JYBGCZX2024103), the Postgraduate Research Practice Innovation Program of Jiangsu Province (KYCX24_2818), the Graduate Innovation Program of China University of Mining and Technology (2024WLKXJ197) and Anhui Provincial Natural Science Foundation (2408085ME147).

Abstract: Calcium clay layers are widely distributed in the Huainan-Huaibei mining area, with the characteristics of low freezing point, strong frost heave, easy disintegration upon contact with water, and low strength, posing a severe challenge to construction using freezing methods. To investigate the mechanical response of frozen calcareous clay under complex stress paths, true triaxial compression tests were performed on the ZSZ-2000 frozen soil true triaxial test platform, varying confining pressures, temperatures, moisture contents, and intermediate principal stress ratios. The strength and deformation characteristics of frozen calcareous clay under these varying conditions were analyzed. The test results indicate that the strength of frozen calcareous clay has a good quadratic relationship with the intermediate principal stress coefficient b and confining pressure, is negatively correlated with temperature, and positively correlated with moisture content. Furthermore, the rate of increase in the failure strength of frozen calcareous clay decreases as the moisture content rises. The failure strength is significantly influenced by the intermediate principal stress and confining pressure, showing both strengthening and weakening effects. A critical intermediate principal stress coefficient of bc =0.75 and a critical confining pressure of σ3c=3 MPa were identified. As the confining pressure rises, the volumetric strain gradually shifts from initial shear contraction followed by shear dilation to pure shear contraction. Moreover, as the b value increases, the peak volumetric strain of the samples also increases. Based on the experimental results, an improved Duncan-Chang model was developed, taking into account the effects of temperature, moisture content, and intermediate principal stress coefficient, and its reliability was verified. The research findings provide a theoretical foundation for optimizing frozen wall design and deep shaft excavation using freezing methods.

Key words: frozen clay, intermediate principal stress coefficient, strength evolution law, true triaxial stress path, Duncan-Chang model

CLC Number: 

  • TU 411
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