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Modeling transient excavation-induced dynamic responses in rock mass using an elasto-plastic cellular automaton

机译:使用弹塑性细胞自动机对岩体中瞬态开挖引起的动力响应进行建模

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摘要

The problem of transient excavation-induced dynamic response in rock mass is discretized on both spatial and temporal scales and is solved by using the cellular automaton (CA) technique and the Newmark scheme, respectively. Using this approach, a dynamic analysis version of 3D elasto-plastic cellular automaton (EPCA(3D)) is developed. The advantage of this method is it avoids the solution of large-scale linear equations since only the local CA rule is used for dynamic state updating. The Den Iseger algorithm is introduced to validate the numerical method. The evolution of stress and velocity for the transient excavation in rock mass under different conditions obtained by the EPCA(3D) and Den Iseger methods are in good agreement. The abilities of EPCA(3D) in the modeling of elasto-plastic dynamics of transient excavation in rock mass are well demonstrated. By considering different in situ stresses, excavation radiuses, unloading durations and unloading paths, the factors affecting nonlinear dynamic responses are investigated. It is found that the failure extent increases with the decrease of unloading time. When lateral pressure coefficient (sigma(x)/sigma(y)) equals to 1, the failure zone is evenly distributed around the tunnel. However, with the decrease of lateral pressure coefficient, the extent of failure localization increases. The fault around the tunnel makes the dynamic failure zone asymmetric distribution. The modeling helps to understand the major mechanism of rock mass damage for the transient excavation.
机译:岩体中瞬态开挖引起的动力响应问题在空间和时间尺度上都是离散的,并分别通过使用元胞自动机(CA)技术和Newmark方案得以解决。使用这种方法,开发了3D弹塑性细胞自动机(EPCA(3D))的动态分析版本。这种方法的优点是它避免了大规模线性方程的求解,因为只有局部CA规则用于动态状态更新。引入了Den Iseger算法来验证数值方法。通过EPCA(3D)和Den Iseger方法获得的在不同条件下岩体中瞬态开挖的应力和速度的变化是一致的。充分证明了EPCA(3D)在岩体中瞬态开挖的弹塑性动力学建模中的能力。通过考虑不同的原地应力,开挖半径,卸载持续时间和卸载路径,研究了影响非线性动力响应的因素。可以发现,随着卸载时间的减少,失效程度增加。当侧向压力系数(sigma(x)/ sigma(y))等于1时,破坏区域在隧道周围均匀分布。但是,随着侧向压力系数的减小,失效局部化的程度增加。隧道周围的断层使动态破坏带不对称分布。该模型有助于了解瞬时开挖过程中岩体破坏的主要机理。

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