It has been previously demonstrated that no reflection is generated when elastic (or electromagnetic) waves enter a region with Perfectly Matching Layer (PML) absorbing conditions in a continuous medium. The practical application of PMLs, however, is in numerical modeling, where the medium is discretized by either a finite-element or a finite-difference scheme thus introducing a reduced amount of reflection. In such a case what is the practical and quantitative efficiency of PML absorbing boundaries? Assuming a regular spatial mesh, we start by evaluating analytically the reflection of body waves introduced by the discrete transition toward PML properties, under variable angle of incidence and wavelength. We then extend our evaluation with numerical tests for both body and Rayleigh waves. Surprisingly enough, the absorption remains equally efficient at wavelengths far larger than the PML thickness itself. As a consequence, the PML thickness can be kept minimal even for studies involving relatively low frequencies, and no rescaling with model size is required. Another pleasant feature is that it is all the more efficient at shallow angles of incidence. Finally, we show through numerical examples that a major advantage of using PMLs is their efficiency in absorbing Rayleigh waves at the free surface, a point where more classical methods perform rather poorly. Although previous authors essentially limited the description of their discrete implementation to 2D, we develop to some level of detail a 3D finite-difference scheme for PMLs and provide numerical examples.
[1]
Qing Huo Liu,et al.
PERFECTLY MATCHED LAYERS FOR ELASTODYNAMICS: A NEW ABSORBING BOUNDARY CONDITION
,
1996
.
[2]
Patrick Joly,et al.
Stability of perfectly matched layers, group velocities and anisotropic waves
,
2003
.
[3]
C. Tsogka,et al.
Application of the perfectly matched absorbing layer model to the linear elastodynamic problem in anisotropic heterogeneous media
,
2001
.
[4]
J. Sochacki.
Absorbing boundary conditions for the elastic wave equations
,
1988
.
[5]
K. Yee.
Numerical solution of initial boundary value problems involving maxwell's equations in isotropic media
,
1966
.
[6]
Marcus J. Grote,et al.
Exact Nonreflecting Boundary Condition For Elastic Waves
,
2000,
SIAM J. Appl. Math..
[7]
Qing Huo Liu,et al.
The application of the perfectly matched layer in numerical modeling of wave propagation in poroelastic media
,
2001
.
[8]
J. Bérenger.
Three-Dimensional Perfectly Matched Layer for the Absorption of Electromagnetic Waves
,
1996
.
[9]
R. Higdon.
Absorbing boundary conditions for elastic waves
,
1991
.
[10]
R. Madariaga.
Dynamics of an expanding circular fault
,
1976,
Bulletin of the Seismological Society of America.
[11]
Ladislav Halada,et al.
3D Fourth-Order Staggered-Grid Finite-Difference Schemes: Stability and Grid Dispersion
,
2000
.
[12]
J. Virieux.
P-SV wave propagation in heterogeneous media: Velocity‐stress finite‐difference method
,
1986
.