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A discontinuous sub-block meso-damage evolution model for rock mass

机译:岩体不连续亚块细观破坏演化模型

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As an effective numerical simulation method, DDA is used in the stability evaluation of rook mass widely although it has some limitations. The failure of rock mass is due to crack propagation between rock maases and the failure within the rock. In the existing DDA methods, the first factor is taken into account usually. Some researchers consider the second factor using fracture mechanics. But remeshing makes the computation complex, and sometimes even difficult. In this paper, a discontinuous sub-block meso-damage evolution model is proposed. In the new model, each block is divided into smaller sub-blocks. There are two kinds of contacts between sub-blocks. One is continuous and the other is discontinuous. The continuity condition can change along the sub-block contacts and the continuous contacts can convert into discontinuous ones using Mohr-Coulomb criterion. The two kinds of contacts are modeled using the Augmented Lagrangian Method. The failure of rock mass is a progressive process. There is damage in rock mass before it loses stability. So the meso-damage mechanics is introduced into the new model. The tensile damage and shearing damage in the sub-block are considered.
机译:DDA作为一种有效的数值模拟方法,虽然有一定的局限性,但却广泛用于车厢质量的稳定性评估。岩体的破坏是由于岩石之间的裂纹扩展以及岩石内部的破坏。在现有的DDA方法中,通常会考虑第一个因素。一些研究人员考虑使用断裂力学的第二个因素。但是重新整理会使计算变得复杂,有时甚至很困难。本文提出了一种不连续的亚块细观破坏演化模型。在新模型中,每个块都分为较小的子块。子块之间有两种接触。一个是连续的,另一个是不连续的。连续性条件可以沿着子块触点变化,并且连续触点可以使用Mohr-Coulomb准则转换为不连续触点。两种接触都是使用增强拉格朗日方法建模的。岩体的破坏是一个渐进的过程。岩体在失去稳定性之前会受到破坏。因此,介观损伤力学被引入到新模型中。考虑了子块中的拉伸损伤和剪切损伤。

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