Abstract
Joints are an important mechanical feature of rock masses. Their effect on wave propagation is significant in characterizing dynamic behaviors of discontinuous rock masses. An experimental study on wave propagation across artificial rock joint was carried out to reveal the relation between the transmission coefficient and the contact situation of the joint surface. The modified split Hopkinson pressure bar apparatus was used in this study while all the bars and specimens were norite cored from the same site. One surface of the specimens with a number of notches was adopted to simulate the artificial rough joint. Two strain gauges were mounted on each pressure bar at a specific spacing. The incident, reflected and transmitted waves across the joints were obtained using a wave separation method. Comparisons of the transmission coefficients were made under two different conditions: with the same joint thickness but different contact area ratios, and with the same contact area ratio but different joint thicknesses. The results show the effects of contact area ratio and thickness of joints on wave transmission.
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Abbreviations
- \(\varepsilon (t)\) :
-
Strain at time t
- \(\varepsilon_{\text{p}} (t)\), \(\varepsilon_{\text{n}} (t)\) :
-
Positive and negative strains
- \(v(t)\) :
-
Particle velocity at time t
- \(c\) :
-
P wave propagation velocity in the rock bar
- \(\varepsilon_{\text{A}} (t)\), \(\varepsilon_{\text{B}} (t)\) :
-
Test records of the strain gauges A and B
- \(\varepsilon_{\text{Ap}} (t)\), \(\varepsilon_{\text{An}} (t)\), \(\varepsilon_{\text{Bp}} (t)\), \(\varepsilon_{\text{Bn}} (t)\) :
-
Positive and negative strains at the positions of the strain gauges A and B
- \(x_{\text{A}}\), \(x_{\text{B}}\) :
-
Distance between the end surface O and the strain gauge A and B, respectively
- \(\Delta t\) :
-
Time interval for positive or negative strain wave propagation between the positions of the strain gauges A and B
- \(\sigma\) :
-
Stress of the joint
- \(E\) :
-
Young’s modulus of the rock bar
- \(\varepsilon_{\text{I}}\), \(\varepsilon_{\text{T}}\) :
-
Strains in the input and output bars
- \(\varepsilon_{\text{Ip}}\), \(\varepsilon_{\text{In}}\), \(\varepsilon_{\text{Tp}}\), \(\varepsilon_{\text{Tn}}\) :
-
Positive and negative strains of the input and output bars, respectively
- \(\dot{\varepsilon }\) :
-
Strain rate of the joint
- \(L\) :
-
Rock joint thickness
- \(\Delta L\) :
-
Normal closure of the joint
- \(T\) :
-
Transmission coefficient of the joint
- \(\varepsilon_{\text{R}} (t)\) :
-
Strain of the reflected wave caused by the joint
- \(\alpha\), \(\beta\), \(\gamma\), \(\varphi\) :
-
Coefficients of the fitting curves
- B–B:
-
Bandis–Barton
- CT:
-
Computerized tomographic
- ISRM:
-
International Society for Rock Mechanics
- SHPB:
-
Split Hopkinson pressure bar
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Acknowledgments
This work was sponsored by the Chinese National Science Research Fund (Grant Nos. 41272348, 51034001) and China Scholarship Council (CSC). The authors also would like to thank Mr. L. Gastaldo and Mr. B. Ferrot of EPFL-LMR for their excellent assistances in specimen preparation, and Professor S. L. Xu of University of Science and Technology of China for his valuable discussions.
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Chen, X., Li, J.C., Cai, M.F. et al. Experimental Study on Wave Propagation Across a Rock Joint with Rough Surface. Rock Mech Rock Eng 48, 2225–2234 (2015). https://doi.org/10.1007/s00603-015-0716-z
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DOI: https://doi.org/10.1007/s00603-015-0716-z