›› 2018, Vol. 39 ›› Issue (4): 1203-1210.doi: 10.16285/j.rsm.2016.0901

• Fundamental Theroy and Experimental Research • Previous Articles     Next Articles

Transmission of S-wave across one joint using the continuously yielding model

CUI Zhen1, SHENG Qian1, LENG Xian-lun1, LUO Qing-zi2   

  1. 1. State Key Laboratory of Geomechanics and Geotechnical Engineering, Institute of Rock and Soil Mechanics, Chinese Academy of Sciences, Wuhan, Hubei 430071, China; 2. School of Civil and Transportation Engineering, Guangdong University of Technology, Guangzhou, Guangdong 510006, China
  • Received:2016-04-25 Online:2018-04-11 Published:2018-06-06
  • Supported by:

    This work was supported by the National Program on Key Basic Research Project of China (2015CB057905), the National Key R & D Program of China (2016YFC0401803), the National Natural Science Foundation of China (51779253, 41672319) and the Guangdong Natural Science Foundation (2016A030310345).

Abstract: It is important to consider an aseismic issue, which is that transflective properties of the seismic wave propagating through joints embedded in rock in underground rock engineering. However, there is very limited research on transflective properties by using the continuously yielding nonlinear joints model. In this paper, a continuously yielding (CY) model was developed based on the time-domain recursive method (TDRM) for S wave using a nonlinear Coulomb-slip (MC) model. Verification of TDRM-based results was conducted in comparison with the simulated results via 3DEC code. Meanwhile, the influence parameters were also discussed. Finally, the results from MC model and CY model were compared under an idealised impulse excitation and a real ground motion record, respectively. It can be seen that TDRM-based results show good agreement with the simulated results by 3DEC, which proves that TDRM is reliable to study the subsequent parameters. In addition, CY model is significantly influenced by parameters of normal stress, incident wave amplitude, initial joint stiffness and joint spacing, respectively. Compared with MC model, CY model can better describe complex joint behaviours in the wave propagation, such as tangential stiffness degradation, shear strength deterioration, normal stress dependence and the hysteresis effect. Therefore, research results can provide useful references for the seismic design and analysis of rock underground engineering.

Key words: seismic wave propagation, nonlinear joint, time-domain recursive method, continuously yielding model

CLC Number: 

  • TU 457

[1] CUI Zhen, SHENG Qian, LENG Xian-lun, LUO Qing-zi,. Control effect of large geological discontinuity on seismic response and stability of underground rock caverns [J]. , 2018, 39(5): 1811-1824.
[2] LONG Ping ,WANG Guan-shi ,HU Shi-li,. Fourier series analysis of a elastic longitudinal wave vertically propagating through a nonlinear joint [J]. , 2015, 36(6): 1807-1814.
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