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

被引:32
|
作者
Wei, Wei [1 ,2 ]
Zhao, Qi [2 ]
Jiang, Qinghui [1 ,3 ]
Grasselli, Giovanni [2 ]
机构
[1] Wuhan Univ, Sch Civil Engn, Wuhan 430072, Hubei, Peoples R China
[2] Univ Toronto, Dept Civil Engn, 35 St George St, Toronto, ON M5S 1A4, Canada
[3] Nanchang Univ, Sch Civil Engn & Architecture, Nanchang 330031, Jiangxi, Peoples R China
基金
中国国家自然科学基金;
关键词
Numerical manifold method; Viscous boundary; Free field boundary; Seismic response analysis; WAVE-PROPAGATION PROBLEMS; UNITY-BASED METHODS; HETEROGENEOUS MEDIA; WENCHUAN EARTHQUAKE; STABILITY ANALYSIS; TRANSIENT ANALYSIS; ELEMENT-METHOD; ROCK SLOPE; SIMULATION; DDA;
D O I
10.1016/j.ijrmms.2018.03.009
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
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.
引用
收藏
页码:110 / 122
页数:13
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