Abstract

SUMMARYThe correct implementation of the continuity conditions between different media is fundamental for the accuracy of any wave equation solver used in applications from seismic exploration to global seismology. Ideally, we would like to benchmark a code against an analytical Green’s function. The latter, however, is rarely available for more complex media. Here, we provide a general framework through which wave equation solvers can be benchmarked by comparing plane wave simulations to transmission/reflection (R/T) coefficients from plane-wave analysis with exact boundary conditions (BCs). We show that this works well for a large range of incidence angles, but requires a lot of computational resources to simulate the plane waves. We further show that the accuracy of a numerical Green’s function resulting from a point-source spherical-wave simulation can also be used for benchmarking. The data processing in that case is more involved than for the plane wave simulations and appears to be sufficiently accurate only below critical angles. Our approach applies to any wave equation solver, but we chose the poroelastic wave equation for illustration, mainly due to the difficulty of benchmarking poroelastic solvers, but also due to the growing interest in imaging in poroelastic media. Although we only use 2-D examples, our exact R/T approach can be extended to 3-D and various cases with different interface configurations in arbitrarily complex media, incorporating, for example, anisotropy, viscoelasticity, double porosities, partial saturation, two-phase fluids, the Biot/squirt flow and so on.

Highlights

  • As seismic waves travel through a medium, information about the internal properties of the medium is collected along their paths

  • To address the issue of lacking analytical Green’s functions, we propose a simple and flexible framework based on reflection and transmission (R/T) coefficients using the exact boundary conditions (BC) of the problem

  • We provide numerical examples from SPECFEM2D in the case of coupled interfaces in porous media

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Summary

INTRODUCTION

As seismic waves travel through a medium, information about the internal properties of the medium is collected along their paths. The accuracy of a wave equation solver is checked by relying on an analytical Green’s function for special cases (e.g. homogeneous or two-layer models) for benchmarking This approach cannot be applied to more complex media where a closedform solution to the wave equation is not available. A more recent discussion on the theoretical derivation of interface conditions involving porous media is presented by Quiroga-Goode (2005) When it comes to numerically modelling of waves in poroelastic media, various methods have been proposed based on finite difference methods For porous media, plane-wave analysis has been used to study the seismic reflection and transmission of an acoustic/poroelastic interface The numerical similations can be benchmarked against analytical Greens’s functions if they are available

Poroelastic wave equations
Different interface conditions in porous media
Plane-wave analysis for interface conditions in coupled porous media
Q compensation for waves propagating in the poroelastic medium
Plane-wave simulation
Model setup
Spherical-wave simulation
Reflected P
Reflected P Reflected S Transmitted fast P Transmitted slow P
CONCLUSION
Findings
Transmitted slow P
Full Text
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