Volume 39 Issue 6
Dec.  2025
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Xu Chao, Wang Longquan, Chen Feng, Xiao Dandan, Huang Zikai, Tang Xiaodong, Zhang Junhan. Pore pressure development of freeze-thaw soft soil under cyclic loading[J]. GEOTECHNICAL ENGINEERING TECHNIQUE, 2025, 39(6): 898-906. doi: 10.20265/j.cnki.issn.1007-2993.2024-0334
Citation: Xu Chao, Wang Longquan, Chen Feng, Xiao Dandan, Huang Zikai, Tang Xiaodong, Zhang Junhan. Pore pressure development of freeze-thaw soft soil under cyclic loading[J]. GEOTECHNICAL ENGINEERING TECHNIQUE, 2025, 39(6): 898-906. doi: 10.20265/j.cnki.issn.1007-2993.2024-0334

Pore pressure development of freeze-thaw soft soil under cyclic loading

doi: 10.20265/j.cnki.issn.1007-2993.2024-0334
  • Received Date: 2024-07-20
  • Accepted Date: 2025-03-10
  • Rev Recd Date: 2025-02-27
  • Available Online: 2025-12-08
  • Publish Date: 2025-12-08
  • Artificial freezing method is widely used in subway tunnel engineering because of its low cost and high safety. The mechanical properties of soft soil will change after freezing and thawing. The development of axial cumulative strain, stiffness and pore water pressure of frozen and thawed soft soil under different freezing temperatures and freezing and thawing confining pressure PF-T was studied through dynamic triaxial tests, and the dynamic pore water pressure prediction model of frozen and thawed soft soil under cyclic loading was established on the basis of quadratic logarithmic model. Based on the nuclear magnetic resonance test, the influence tf PF-T on the pore distribution of frozen-thawed soil samples was studied. The research results show that: the internal structure of the soil sample was balanced under the action of PF-T, and the restraining effect of PF-T on the deformation of the soil sample gradually decreases with the increase of PF-T; the lower the freezing temperature, the more obvious the frost heave effect of soil; with the increase of freezing and thawing confining pressure, the stiffness softening degree of soil samples gradually weakens; during the freezing and thawing process of soil samples, the increase of PF-T promotes the compaction of damaged skeleton in soil. After the first freeze-thaw, the mechanical properties of soil have the greatest attenuation, and after the second and third freeze-thaw, the existing structural damage area will be aggravated and new structural damage will be brought. In the process of freezing and thawing, the larger PF-T was applied, the more unfrozen water is, the less frost heaving is, and the more compact the skeleton structure is. The research results can provide theoretical basis for predicting the development of pore pressure of frozen-thawed soft soil under cyclic loading.

     

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