Technical Papers
Jan 2, 2020

Analysis of Seismic Waves Propagating through an In Situ Stressed Rock Mass Using a Nonlinear Model

Publication: International Journal of Geomechanics
Volume 20, Issue 3

Abstract

In situ stress is a significant characteristic of underground rock masses. This work extended the time-domain recursive method (TDRM) to study oblique wave attenuation across an in situ stressed joint wherein the normal and shear deformation behaviors were both treated nonlinearly. Employing the Barton–Bandis (B-B) and hyperbolic nonlinear (HN) slip models, equations were established for wave propagation across a rock mass under a combination of gravitational and tectonic stress. Then, the stress and displacement in the normal and shear directions were calculated under different in situ stresses for P- and S-wave incidence. The waveforms of the HN slip model and the Coulomb slip model were compared to investigate the differences therein and verify the wave propagation equation. Parametric studies were conducted to elucidate the influences of in situ stress, lateral pressure coefficient, angle of incidence, and amplitude of the incident wave. The results showed that the HN model depends on the stress history and shear stiffness degradation. The effect of the in situ stress on wave propagation depends not only on the gravitational and tectonic stresses but also on the direction of the particle vibration of the incident wave.

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Data Availability Statement

Some or all data, models, or code generated or used during the study are available from the corresponding author by request, including the original data for Figs. 311.

Acknowledgments

The research was financially supported by the National Natural Science Foundation of China (Grant Nos. 51609183 and 51774222); the Natural Science Foundation of Hubei Province, China (Grant No. 2017CFB508); the Open Research Fund of the State Key Laboratory of Geomechanics and Geotechnical Engineering, Institute of Rock and Soil Mechanics, Chinese Academy of Sciences (Nos. Z015005 and Z018009); and the project supported by the Hubei Key Laboratory of Roadway Bridge and Structure Engineering (Wuhan University of Technology) (DQJJ201710).

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Go to International Journal of Geomechanics
International Journal of Geomechanics
Volume 20Issue 3March 2020

History

Received: Apr 4, 2019
Accepted: Sep 3, 2019
Published online: Jan 2, 2020
Published in print: Mar 1, 2020
Discussion open until: Jun 2, 2020

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Tingting Liu [email protected]
Associate Professor, Key Laboratory of Roadway Bridge and Structure Engineering, Wuhan Univ. of Technology, Wuhan, Hubei 430070, PR China; Assistant Professor, State Key Laboratory of Geomechanics and Geotechnical Engineering, Institute of Rock and Soil Mechanics, Chinese Academy of Sciences, Wuhan, Hubei 430071, PR China. Email: [email protected]
Professor, Key Laboratory of Roadway Bridge and Structure Engineering, Wuhan Univ. of Technology, Wuhan, Hubei 430070, PR China. Email: [email protected]
Assistant Professor, State Key Laboratory of Geomechanics and Geotechnical Engineering, Institute of Rock and Soil Mechanics, Chinese Academy of Sciences, Wuhan, Hubei 430071, PR China (corresponding author). Email: [email protected]
Assistant Professor, State Key Laboratory of Geomechanics and Geotechnical Engineering, Institute of Rock and Soil Mechanics, Chinese Academy of Sciences, Wuhan, Hubei 430071, PR China; Assistant Professor, Faculty of Science, Engineering and Technology, Swinburne Univ. of Technology, Hawthorn, VIC 3122, Australia. Email: [email protected]
Dongri Song [email protected]
Associate Professor, Key Laboratory of Mountain Hazards and Earth Surface Process, Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu 610041, China. Email: [email protected]

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