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  • 全国中文核心期刊
  • 中国科技核心期刊
  • 美国工程索引(EI)收录期刊
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SONG Yong-jun, ZHANG Lei-tao, REN Jian-xi, CHEN Jia-xing, CHE Yong-xin, YANG Hui-min, BI Ran. Triaxial creep properties and model of red sandstone under freeze-thaw environment[J]. Chinese Journal of Geotechnical Engineering, 2021, 43(5): 841-849. DOI: 10.11779/CJGE202105007
Citation: SONG Yong-jun, ZHANG Lei-tao, REN Jian-xi, CHEN Jia-xing, CHE Yong-xin, YANG Hui-min, BI Ran. Triaxial creep properties and model of red sandstone under freeze-thaw environment[J]. Chinese Journal of Geotechnical Engineering, 2021, 43(5): 841-849. DOI: 10.11779/CJGE202105007

Triaxial creep properties and model of red sandstone under freeze-thaw environment

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  • Received Date: August 09, 2020
  • Available Online: December 04, 2022
  • In order to study the time-effectiveness mechanical properties of rock mass engineering in cold regions under the coupling of freeze-thaw cycles and long-term loads, the triaxial multi-level loading and unloading creep tests are carried out on saturated red sandstone under different freeze-thaw cycles. The results show that the effects of freeze-thaw cycles on the creep deformation of red sandstone are related to the loading stress level. At low stress levels, the viscoelastic strain of rock increases approximately linearly and slowly with the increasing freeze-thaw cycles, and at high stress levels, it increases nonlinearly. The viscoplastic strain increases linearly with increasing freeze-thaw cycles. The fourth-level loading stress level (70%σc) is the boundary point of the creep deformation characteristics of red sandstone. The steady-state creep rate of red sandstone increases exponentially with the increase of the freeze-thaw cycles. Based on the creep test results of the red sandstone, the freeze-thaw-damage creep model considering the effects of freeze-thaw cycles and creep damage is established. The creep equation for rock under three-dimensional stress is obtained. The proposed model is verified and its parameters are identified. The theoretical and experimental data are in good agreement. The influences of freeze-thaw cycles on the model parameters are analyzed. The research results may provide a theoretical basis for the construction of rock mass engineering and long-term stability analysis in cold regions.
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