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An experimental and theoretical stress-strain-damage correlation procedure for constitutive modelling of granite

机译:花岗岩本构型建模的实验与理论应力 - 应变损伤相关步骤

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In this study, new theoretical and experimental stress-strain-damage correlation procedures for hard rock constitutive models are proposed. The damage-plasticity modelling framework is first supplied with the unified yield-failure criterion to describe the failure behaviour of granite under triaxial compression. This unified criterion allows the initial yield surface to evolve to a final failure surface through the utilisation of an appropriate damage evolution law. This evolution automatically captures the quasi-brittle behaviour of rocks under shearing at low confining pressure and ductile response under high confining pressure, as well as the transition from quasi-brittle to ductile reactions. In this theoretical sense, damage and plasticity are tightly coupled to govern the behaviour of rocks under different confining pressures without requiring any separate formulations for softening or hardening. Next, an innovative experimental correlation procedure is proposed to better link the experimental damage measure to stress states throughout triaxial loading. By obtaining full stress, strain and acoustic emission damage results from testing it was possible to construct a series of evolving yield surfaces from experiment. These surfaces, coupled with experimental damage evolution with respect to accumulated plastic strain, provide a comprehensive data set to a constitutive model for calibration. The results of numerical simulation show that this new method to incorporate coupled stress-strain-damage evolution characteristics directly from experiment removes the need for trial and error curve fitting. Also, by maintaining a closer link to detailed experimental results, the model is easier to calibrate and can be relied upon to predict the damage and stress states for compressive stress regimes. Finally, it is shown that the theoretical and experimental procedures can capture the key behaviours of granite under a range of confining pressures.
机译:在这项研究中,提出了硬岩本构模型的新的理论和实验应力 - 应变损伤相关程序。首先提供损坏塑性建模框架,统一的收益率 - 故障标准描述了三轴压缩下花岗岩的故障行为。该统一标准允许初始屈服表面通过利用适当的损伤演化法来发展到最终失败表面。这种进化自动捕获剪切下的岩石的准脆性行为,在高限制压力下在低限制压力下,以及从准脆性转变为韧性反应的过渡。在这种理论上的感觉中,损伤和可塑性紧密地连接,以控制在不同的限制压力下岩石的行为,而不需要任何用于软化或硬化的单独制剂。接下来,提出了一种创新的实验相关程序,以更好地将实验损伤措施与整个三轴加载中的应激状态联系起来。通过获得全应力,应变和声排放损伤是由测试产生的,可以从实验构建一系列演化的屈服表面。这些表面与关于累积塑性应变的实验损伤演化相结合,提供了一个综合数据设置为校准的本构体模型。数值模拟的结果表明,这种新方法直接从实验中掺入耦合应力 - 应变损伤演化特性,除去了对试验和误差曲线的需求。此外,通过维持更接近详细实验结果的链接,该模型更容易校准,并且可以依赖于预测压缩应力制度的损坏和应力状态。最后,显示理论和实验程序可以在一系列限制压力下捕获花岗岩的关键行为。

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