Incidence of plane waves upon a fracture

B Gu, R Suárez‐Rivera, KT Nihei… - Journal of Geophysical …, 1996 - Wiley Online Library
B Gu, R Suárez‐Rivera, KT Nihei, LR Myer
Journal of Geophysical Research: Solid Earth, 1996Wiley Online Library
This paper investigates the details of reflection, transmission, and conversion of plane
waves incident upon a fracture at arbitrary angles. The elastic compliance of fractures that is
produced by the presence of a planar collection of void spaces and asperities of contact is
modeled as a displacement‐discontinuity boundary condition between two elastic half‐
spaces. Closed‐form expressions for the transmission and reflection coefficients on a
fracture are derived by replacing the boundary conditions for a welded interface by those for …
This paper investigates the details of reflection, transmission, and conversion of plane waves incident upon a fracture at arbitrary angles. The elastic compliance of fractures that is produced by the presence of a planar collection of void spaces and asperities of contact is modeled as a displacement‐discontinuity boundary condition between two elastic half‐spaces. Closed‐form expressions for the transmission and reflection coefficients on a fracture are derived by replacing the boundary conditions for a welded interface by those for a fracture into the standard procedure for plane wave analysis. The closed‐form expressions reveal that a single fracture can produce a variety of potentially diagnostic waves such as transmitted waves, reflected waves, converted waves, head waves, and P interface waves and introduce a finite group time delay to all these waves with respect to the incident wave. The amplitude and group time delay of the fracture‐induced waves are controlled by the fracture stiffness, wave frequency, and the Poisson's ratio of the medium. The head wave and inhomogeneous P interface waves are generated when an SV wave is incident upon a fracture, at and beyond a critical angle, respectively, which is determined by Snell's law. For some combinations of the fracture stiffness and the Poisson's ratio of the half‐spaces, no reflection or transmission of a P wave or an SV wave occurs.
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