Experimental Study on the Deformation of Anisotropic Loess under Cyclic Spherical StressSource: International Journal of Geomechanics:;2025:;Volume ( 025 ):;issue: 007::page 04025111-1DOI: 10.1061/IJGNAI.GMENG-10903Publisher: American Society of Civil Engineers
Abstract: Cyclic spherical stresses are prevalent in dynamic stress fields and significantly influence the dynamic behavior of loess, a material characterized by high compressibility and anisotropy. Previous research has primarily focused on shear stresses, often overlooking the impact of spherical stresses. This study investigated the deformation induced by cyclic spherical stress under different initial states. Irreversible and reversible components were identified from both volumetric and shear strains, and their variation patterns were analyzed. Shear strain is found to be generated by the material’s anisotropy. The results indicate that the volume of the sample shrinks significantly under cyclic spherical stress, with irreversible volumetric strain increasing nonlinearly as the number of cycles increases. Irreversible shear strains can be categorized into two types based on their formation mechanisms. The first is when significant initial anisotropy leads to radial deformation greater than axial deformation under spherical stress, resulting in shear strain increasing in the negative direction. As consolidation stress increases, the initial anisotropy gradually diminishes. The second is when stress-induced anisotropy results in positive shear strain because consolidation deviatoric stress contributes to an increase in shear strain in the positive direction. As the stress ratio rises, the induced anisotropy is further enhanced. The axial reversible strain of the sample is minor, and the reversible components of volumetric and shear strains primarily arise from radial contraction and expansion. As the spherical stress increases, the sample volume shrinks (positive volumetric strain), whereas the initial anisotropy leads to negative shear strain, resulting in opposite signs. Finally, a method for predicting irreversible strain under cyclic spherical stress is established based on a memoryless geometric distribution.
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| contributor author | Bin Zhang | |
| contributor author | Shuai Shao | |
| contributor author | Shengjun Shao | |
| contributor author | Liguo Yang | |
| contributor author | Jiang Wu | |
| contributor author | Lei Qi | |
| date accessioned | 2025-08-17T22:22:04Z | |
| date available | 2025-08-17T22:22:04Z | |
| date copyright | 7/1/2025 12:00:00 AM | |
| date issued | 2025 | |
| identifier other | IJGNAI.GMENG-10903.pdf | |
| identifier uri | http://yetl.yabesh.ir/yetl1/handle/yetl/4306834 | |
| description abstract | Cyclic spherical stresses are prevalent in dynamic stress fields and significantly influence the dynamic behavior of loess, a material characterized by high compressibility and anisotropy. Previous research has primarily focused on shear stresses, often overlooking the impact of spherical stresses. This study investigated the deformation induced by cyclic spherical stress under different initial states. Irreversible and reversible components were identified from both volumetric and shear strains, and their variation patterns were analyzed. Shear strain is found to be generated by the material’s anisotropy. The results indicate that the volume of the sample shrinks significantly under cyclic spherical stress, with irreversible volumetric strain increasing nonlinearly as the number of cycles increases. Irreversible shear strains can be categorized into two types based on their formation mechanisms. The first is when significant initial anisotropy leads to radial deformation greater than axial deformation under spherical stress, resulting in shear strain increasing in the negative direction. As consolidation stress increases, the initial anisotropy gradually diminishes. The second is when stress-induced anisotropy results in positive shear strain because consolidation deviatoric stress contributes to an increase in shear strain in the positive direction. As the stress ratio rises, the induced anisotropy is further enhanced. The axial reversible strain of the sample is minor, and the reversible components of volumetric and shear strains primarily arise from radial contraction and expansion. As the spherical stress increases, the sample volume shrinks (positive volumetric strain), whereas the initial anisotropy leads to negative shear strain, resulting in opposite signs. Finally, a method for predicting irreversible strain under cyclic spherical stress is established based on a memoryless geometric distribution. | |
| publisher | American Society of Civil Engineers | |
| title | Experimental Study on the Deformation of Anisotropic Loess under Cyclic Spherical Stress | |
| type | Journal Article | |
| journal volume | 25 | |
| journal issue | 7 | |
| journal title | International Journal of Geomechanics | |
| identifier doi | 10.1061/IJGNAI.GMENG-10903 | |
| journal fristpage | 04025111-1 | |
| journal lastpage | 04025111-17 | |
| page | 17 | |
| tree | International Journal of Geomechanics:;2025:;Volume ( 025 ):;issue: 007 | |
| contenttype | Fulltext |