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考慮歷史加卸載影響的鹽巖蠕變本構模型研究

Study on creep constitutive model of salt rock considering the effects of historical loading and unloading

  • 摘要: 加卸載歷史對蠕變變形的顯著影響表明地下工程中反復變化的應力環境(如開挖、回填和卸載)會改變鹽巖的長期穩定性。基于此,開展了相同應力水平下分級加載和分級卸載的鹽巖蠕變試驗,研究了不同加卸載歷史對鹽巖蠕變行為的影響。通過引入表征巖石硬化程度的狀態變量,構建了一種能夠考慮加卸載歷史影響的鹽巖蠕變本構模型,從而實現對鹽巖變形行為更為準確的表征和預測。結果表明:升梯度和降梯度的蠕變速率因加卸載歷史的影響存在顯著差異。基于狀態變量的新型蠕變本構模型對不同加載路徑的蠕變變形擬合曲線和試驗曲線契合度均較高,能夠較好地預測鹽巖蠕變行為的歷史效應。此外,加載引起的塑性變形只與加載前后的應力狀態有關,與加載路徑、加卸載速率和加卸載時間無關。模型參數分析顯示,參數k、m和c通過影響狀態變量影響模型。參數a通過影響等速蠕變變形影響模型。參數b通過影響變速蠕變應變影響模型。參數n表征蠕變變形與應力的敏感性,同時影響變速蠕變和等速蠕變變形。

     

    Abstract: The significant influence of loading and unloading history on creep deformation indicates that the cyclic stress environment in underground engineering (such as excavation, backfilling, and unloading) can alter the long-term stability of salt rock. Based on this, creep tests of salt rock under stepped loading and unloading at the same stress level were conducted to investigate the effects of different loading and unloading histories on the creep behaviour of salt rock. By introducing a state variable that characterizes the degree of rock hardening, a creep constitutive model for salt rock was established to account for the influence of loading and unloading history, enabling more accurate characterization and prediction of salt rock deformation behaviour. The creep rates under ascending and descending stress gradients exhibit significant differences due to the influence of loading and unloading history. The new creep constitutive model based on state variables shows a high degree of agreement between the fitted creep deformation curves under different loading paths and the test curves, providing a good prediction of the historical effects on the creep behaviour of salt rock. In addition, the plastic deformation during loading is only related to the stress state before and after loading, and is independent of the loading path, loading and unloading rate, and loading and unloading time. Parameters k, m, and c influence the model by affecting the state variable. Parameter a affects the model by influencing steady-state creep deformation, while parameter b affects the model by influencing variable creep strain. Parameter n characterizes the sensitivity of creep deformation to stress, while also affecting both decay-rate and steady-state creep deformation.

     

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