A Detailed Analysis of Body Waves Simulated in Homogenized Media
Non-periodic homogenization has proved to be an accurate asymptotic method for computing long-wavelength equivalent media for the seismic wave equation, turning small-scale heterogeneities and geometric complexity into smooth elastic properties. Using homogenized media allows i) decreasing the computation cost of wave propagation simulation and ii) studying the apparent, small-scale-induced anisotropy. After illustrating these two aspects briefly, we propose to analyze in great detail the accuracy of body waves simulated in homogenized 3D models of the subsurface. First, the behaviour of head-, reflected and refracted waves with respect to source-receiver offset, maximum frequency and velocity contrast across a planar interface, is investigated. Then, we consider the SEG-EAGE overthrust model to exemplify how the accuracy of simulated body waves anti-correlates with the distance to seismic source and the amount of apparent anisotropy. In high apparent anisotropy regions, we show that the first-order correction provided by the homogenization theory significantly improves the computed wavefield. The overall results of this analysis better frame the use of homogenized media in seismic wave simulation.
Session: Numerical Modeling in Seismology: Developments and Applications - II
Type: Oral
Room: Tubughnenq’ 4
Date: 5/1/2024
Presentation Time: 10:45 AM (local time)
Presenting Author: Paul Cupillard
Student Presenter: No
Additional Authors
Paul Cupillard Presenting Author Corresponding Author paul.cupillard@univ-lorraine.fr Université de Lorraine |
Wim Mulder W.A.Mulder@tudelft.nl TU Delft & Shell Global Solutions |
Pierre Anquez pierre.anquez@geode-solutions.com Geode-solutions |
Antoine Mazuyer antoine.mazuyer@totalenergies.com TotalEnergies |
Mustapha Zakari mustapha.zakari@univ-lorraine.fr CNRS |
Jean-François Barthélémy jean-francois.barthelemy@cerema.fr CEREMA |
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A Detailed Analysis of Body Waves Simulated in Homogenized Media
Category
Numerical Modeling in Seismology: Developments and Applications
Description