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Damage constitutive model for strain-softening rock based on normal distribution and its parameter determination

机译:基于正态分布的应变软化岩石损伤本构模型及其参数确定

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摘要

Firstly, using the damage model for rock based on Lemaitre hypothesis about strain equivalence, a new technique for measuring strength of rock micro-cells by adopting the Mohr-Coulomb criterion was developed, and a statistical damage evolution equation was established based on the property that strength of micro-cells is consistent with normal distribution function, through discussing the characteristics of random distributions for strength of micro-cells, then a statistical damage constitutive model that can simulate the full process of rock strain softening under specific confining pressure was set up. Secondly, a new method to determine the model parameters which can be applied to the situations under different confining pressures was proposed, by deeply studying the relations between the model parameters and characteristic parameters of the full stress-strain curve under different confining pressures. Therefore, a unified statistical damage constitutive model for rock softening which can reflect the effect of different confining pressures was set up. This model makes the physical property of model parameters explicit, contains only conventional mechanical parameters, and leads its application more convenient. Finally, the rationality of this model and its parameters-determining method were identified via comparative analyses between theoretical and experimental curves.
机译:首先,利用基于Lemaitre应变当量假设的岩石损伤模型,开发了一种采用Mohr-Coulomb准则测量岩石微孔强度的新技术,并基于该性质建立了统计损伤演化方程。通过讨论微孔强度的随机分布特征,建立了微孔强度与正态分布函数相一致的模型,建立了可以模拟岩石在特定围压下软化全过程的统计损伤本构模型。其次,通过深入研究模型参数与不同约束压力下全应力-应变曲线特征参数之间的关系,提出了一种适用于不同约束压力条件的模型参数确定方法。因此,建立了能够反映不同围压作用的统一的岩石软化统计损伤本构模型。该模型使模型参数的物理特性更加明确,仅包含常规的机械参数,从而使其应用更加方便。最后,通过理论和实验曲线的对比分析,确定了该模型的合理性及其参数确定方法。

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