考虑历史加卸载影响的盐岩蠕变本构模型研究

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

  • 摘要: 加卸载历史对蠕变变形的显著影响表明地下工程中反复变化的应力环境(如开挖、回填和卸载)会改变盐岩的长期稳定性。基于此,开展了相同应力水平下分级加载和分级卸载的盐岩蠕变试验,研究了不同加卸载历史对盐岩蠕变行为的影响。通过引入表征岩石硬化程度的状态变量,构建了一种能够考虑加卸载历史影响的盐岩蠕变本构模型,从而实现对盐岩变形行为更为准确的表征和预测。结果表明:升梯度和降梯度的蠕变速率因加卸载历史的影响存在显著差异。基于状态变量的新型蠕变本构模型对不同加载路径的蠕变变形拟合曲线和试验曲线契合度均较高,能够较好地预测盐岩蠕变行为的历史效应。此外,加载引起的塑性变形只与加载前后的应力状态有关,与加载路径、加卸载速率和加卸载时间无关。模型参数分析显示,参数k、m和c通过影响状态变量影响模型。参数a通过影响等速蠕变变形影响模型。参数b通过影响变速蠕变应变影响模型。参数n表征蠕变变形与应力的敏感性,同时影响变速蠕变和等速蠕变变形。

     

    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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