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首页> 外文期刊>KSCE journal of civil engineering >Energy Evolution of Rock under Different Stress Paths and Establishment of a Statistical Damage Model
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Energy Evolution of Rock under Different Stress Paths and Establishment of a Statistical Damage Model

机译:不同应力路径下岩石的能量演化及统计损伤模型的建立

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摘要

In consideration of the influence of energy dissipation on the rock compression process, the traditional elastic stress-strain relationship was improved by adding the energy release rate. The microintensity of the rock was assumed to satisfy the Weibull distribution. The improved stress-strain relationship was transformed into a triaxial stress-strain model in consideration of the loading damage combined with mesodamage mechanics. The characteristic points of the stress-strain curve and the experimental data were utilized to calculate the distribution parameters of the rock under different conditions. The model curve was compared with the experimental data. Results showed that the stress-strain curve of the rock has peak points in the conventional triaxial compression test, but the radial peak of the rock was not evident in the unloading test. The energy of the rock under the loading path was smaller than that under the unloading path. The model curve exhibited a high degree of fitting with the experimental data, and its correlation coefficient was relatively large (> 0.90), which indicated that the model can clearly represent the actual damage and evolution law of the surrounding rock. Furthermore, the established model can also reflect the rock's stress-strain relationship, which can serve as a practical guide for relevant applications. Finally, the distribution parameters also reflected the evolution law of rock energy and provided a method for the assessment of rock energy and damage trend.
机译:考虑到能量耗散对岩石压缩过程的影响,通过增加能量释放率来改善传统的弹性应力-应变关系。假定岩石的微强度满足威布尔分布。考虑到载荷损伤并结合介观损伤力学,将改进的应力-应变关系转换为三轴应力-应变模型。利用应力-应变曲线的特征点和实验数据来计算不同条件下岩石的分布参数。将模型曲线与实验数据进行比较。结果表明,在常规的三轴压缩试验中,岩石的应力-应变曲线具有峰值,但在卸载试验中,岩石的径向峰值并不明显。装载路径下的岩石能量小于卸载路径下的岩石能量。模型曲线与实验数据高度吻合,相关系数较大(> 0.90),表明模型可以清晰地反映出围岩的实际破坏和演化规律。此外,建立的模型还可以反映岩石的应力-应变关系,可以为相关应用提供实用指南。最后,分布参数还反映了岩石能量的演化规律,为评估岩石能量和破坏趋势提供了一种方法。

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