Abstract
Seismic waves might be unavoidably triggered during underground energy and resource exploitation. Surface irregularities and subsurface cavities have significant effects on seismic wave propagation and cause amplification or reduction of ground motion. Hence, it is significant to address the scattering problem of SH waves induced by topography features and subsurface cavities in earthquake engineering. In this paper, based on the wave function expansion method coupling with the conjunction concept and the Graf’s addition formula, a series solution to this scattering problem of SH waves induced by a semi-cylindrical hill and a nearby cylindrical cavity in a homogeneous, isotropic, linear elastic half-space is derived. The displacement amplitudes on the hill surface and its environs are calculated, and compared with the results in the existing works to verify the validity of the deriving process. Then, parametric studies are performed to analyze the effects of the cavity (its location and size), and the characteristics of incident waves (the frequency and incident angle) on the seismic response of the semi-cylindrical hill. Finally, the seismic behavior of the cylindrical cavity near or away from the hill for different frequencies and incident angles is examined.
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Abbreviations
- \(a_{1}\) :
-
Semi-cylindrical hill radius
- \(d\) :
-
Burial depth of the cavity
- \(\theta\), \(\theta_{ 1}\), \(\theta_{ 2}\) :
-
Polar angles measured from the vertical y-, y1-, y2-axes, respectively
- \(\alpha\) :
-
Incident angle
- u f :
-
Steady-state out-of-plane motion corresponding to free field
- i :
-
\(\sqrt { - 1}\)
- c :
-
Shear wave velocity
- k :
-
Shear wavenumber
- \(J_{n} \left( \cdot \right)\) :
-
nth order Bessel function of the first kind
- \(\varepsilon_{n}\) :
-
Neumann factor
- \(\left| u \right|\) :
-
Displacement amplitude
- \(\lambda\) :
-
Wavelength of incident SH wave
- Im():
-
Imaginary part of a complex expression
- \(a_{2}\) :
-
Subterranean cylindrical cavity radius
- \(l\) :
-
Horizontal distance between the centers of the hill and the cavity
- \(\omega\) :
-
Circular frequency of incident SH wave
- \(u^{\left( j \right)}\) :
-
Steady-state out-of-plane motion in the region j
- u s :
-
Steady-state out-of-plane motion corresponding to scattered field
- t :
-
Time
- \(\mu\) :
-
Shear modulus
- \(\tau\) :
-
Shear stress
- \(H_{n}^{\left( 1 \right)} \left( \cdot \right)\) :
-
nth order Hankel function of the first kind
- \(x\) :
-
Abscissa corresponding to the rectangular coordinate system x–o–y
- \(\eta\) :
-
Dimensionless frequency
- Re():
-
Real part of a complex expression
- n, q, s, m :
-
Summation indexes
- N, QQ, SS, M :
-
Values corresponding to n, q, s, m, respectively, when the infinite series is truncated to a finite number
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Acknowledgements
This work is supported by National Natural Sciences Foundation of China (41525009, 41831281).
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Li, Z.L., Li, J.C. & Li, X. Seismic interaction between a semi-cylindrical hill and a nearby underground cavity under plane SH waves. Geomech. Geophys. Geo-energ. Geo-resour. 5, 405–423 (2019). https://doi.org/10.1007/s40948-019-00120-5
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DOI: https://doi.org/10.1007/s40948-019-00120-5