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| The fabric-stress relationship and the equivalent stress method of granular materials |
| DONG Tong1,2,KONG Liang2,ZHENG Yingren1,WANG Xing2,LIU Yun3 |
(1. Chongqing Key Laboratory of Geomechanics and Geoenvironmental Protection,Army Logistics University of PLA,
Chongqing 401311,China;2. School of Sciences,Qingdao Technological University,Qingdao,Shandong 266033,China;
3. Chongqing Industry Polytechnic College,Chongqing 401120,China) |
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Abstract The methods in establishing the existing anisotropic constitutive models are reviewed systematically. It is pointed out that the description of the fabric direction should be attributed to the coordinate transformation of fabric and stress. For anisotropic materials,the total stress needs to be allocated according to the actual bearing area of each component,because the effective bearing areas of soil skeleton in different directions are different. Therefore,by introducing the transformation matrix,the equivalent stress tensor is proposed to describe the anisotropy of granular materials,the true stress inside the material and the relationship between the fabric direction and the stress direction. Therefore,the material anisotropy in macro-scale can be regarded as the result of the application of anisotropic stress on an equivalent isotropic material in micro-scale. The equivalent stress tensor is used to describe the anisotropic stress and the existing isotropic model is used to describe the mechanical property of the equivalent isotropic material. A general method of transforming the existing isotropic failure criterion and constitutive model into anisotropic ones,named“Equivalent Stress Method”,is put forward from the perspective of stress. Finally,the SMP criterion is transformed into anisotropic one as an example. The comparison with the existing experimental results proves the rationality and validity of the anisotropic transformation.
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