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Three new boundary conditions for the seismic response analysis of geomechanics problems using the numerical manifold method

机译:数值歧管方法对地质力学问题的地震反应分析的三个新边界条件

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摘要

The numerical manifold method (NMM) provides a unified approach to address continuum-discontinuum problems in geotechnical engineering. Owing to the dynamic nature of its governing equations, the NMM should be suitable for modelling dynamic problems such as those associated to earthquakes. However, due to the current limitations in far-field boundary conditions implemented in the original NMM formulation, NMM has not been used to carry out seismic response analysis. In the present study, three new boundary conditions have been developed to extend the capability of the NMM to conduct seismic response analysis: (1) the classical viscous boundary condition, which allows for the absorption of the seismic wave energy at the boundaries, based on the viscous boundaries, and the seismic motion input method is also proposed; (2) the free field boundary condition, which captures the free field motion and absorption of the reflected waves at the sides of the model. The algorithms to generate free field mesh and its coupling calculations with the main mesh are also presented; (3) the static-dynamic unified boundary, which models the transition from fixed boundary condition in static state to free field boundary condition in seismic state, thus ensuring the accuracy and consistency of the numerical simulation. Finally, five numerical examples are shown to validate the proposed methods. The numerical results indicate that the improved NMM can be successfully adopted for seismic response analysis.
机译:数值歧管方法(NMM)提供了一种统一的方法来解决岩土工程中的连续不连续性问题。由于其控制方程的动态性质,NMM应该适用于建模动态问题,例如与地震相关的动态问题。然而,由于原始NMM制剂中实施的远场边界条件的电流限制,NMM尚未用于进行地震响应分析。在本研究中,已经开发了三种新的边界条件来延长NMM进行地震反应分析的能力:(1)经典粘性边界条件,其允许基于界限的地震波能量吸收还提出了粘性边界和地震运动输入法; (2)自由场边界条件,其捕获模型侧面的自由场运动和反射波的吸收。还提出了生成自由场网的算法及其与主网格的耦合计算; (3)静态动态统一边界,其模拟从静态状态的固定边界条件转换到地震状态下的自由场边界条件,从而确保了数值模拟的准确性和一致性。最后,显示了五个数值例子来验证所提出的方法。数值结果表明可以成功采用改进的NMM用于地震响应分析。

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