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Theory and laboratory experiments of elastic wave scattering by dry planar fractures
Author(s) -
Blum Thomas E.,
Snieder Roel,
van Wijk Kasper,
Willis Mark E.
Publication year - 2011
Publication title -
journal of geophysical research: solid earth
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2011jb008295
Subject(s) - scattering , wavelength , amplitude , planar , slip (aerodynamics) , scattering amplitude , fracture (geology) , attenuation , born approximation , s wave , geology , mechanics , geophysics , physics , optics , acoustics , geotechnical engineering , computer science , computer graphics (images) , thermodynamics
Remote sensing of fractures with elastic waves is important in fields ranging from seismology to nondestructive testing. In many geophysical applications, fractures control the flow of fluids such as water, hydrocarbons or magma. While previous analytic descriptions of scattering mostly deal with very large or very small fractures (compared to the dominant wavelength), we present an analytic solution for the scattering of elastic waves from a fracture of arbitrary size. Based on the linear slip model for a dry fracture, we derive the scattering amplitude in the frequency domain under the Born approximation for all combinations of incident and scattered wave modes. Our analytic results match laser‐based ultrasonic laboratory measurements of a single fracture in clear plastic, allowing us to quantify the compliance of a fracture.

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