Rock and Soil Mechanics ›› 2019, Vol. 40 ›› Issue (10): 4101-4110.doi: 10.16285/j.rsm.2018.1964

• Numerical Analysis • Previous Articles     Next Articles

3D seismic response broadband-simulation of the alluvial basin in urban region based on the FMM-IBEM

LIU Zhong-xian1, ZHANG Zheng1, WANG Shao-jie1, 2, LIANG Jian-wen3, WANG Hai-liang1   

  1. 1. Tianjin Key Laboratory of Civil Structure Protection and Reinforcement, Tianjin Chengjian University, Tianjin 300384, China; 2. Hebei Building Research Technical Co., Ltd., Shijiazhuang, Hebei 050021, China; 3. Department of Civil Engineering, Tianjin University, Tianjin 300072, China
  • Received:2018-10-25 Online:2019-10-11 Published:2019-10-20
  • Supported by:
    This work was supported by the National Natural Science Foundation of China (51678390), the Key Program for Natural Foundation of Tianjin (18JCZDJC39200) and the Key Projects of Science and Technology Pillar Program of Tianjin (17YFZCSF01140).

Abstract: Aiming at the three-dimensional ground motion simulation of alluvial basins in urban areas, the unique advantages of boundary element method (BEM) in dealing with wave motion in infinite domain and the high efficiency and large capacity of fast multipole algorithm (FMM) are brought into play. A simulation method suitable for broadband multi-degree-of-freedom model, fast multipole indirect boundary element method (FMM-IBEM) is developed. Through precision comparison and efficiency verification, it is found that FMM-IBEM can accurately and efficiently realize broadband simulation of ground motions in three-dimensional complex sites, and greatly reduce the storage and calculation. Then, the method is used to analyze a three-dimensional alluvial basin with complex shape and undulating bedrock surface in frequency domain and time domain. The results show that: incidence frequency, basin shape and location of the basin have different effects on the magnification of surface displacement of alluvial basins, and generally, the amplification effect in low frequency domain is higher than that in high frequency domain. Spectrum curves show multiple resonance bands, and the magnification effect of surface displacement in the middle and margin of alluvial basin is significantly different. Site selection of important projects should avoid seismic energy accumulation areas in alluvial basins.

Key words: 3D alluvial basin seismic response, FMM-IBEM, seismic wave

CLC Number: 

  • TU 435
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