Efficient Methods to Simulate Planar Free Surface in the 3D 4th-Order Staggered-Grid Finite-Difference Schemes

We numerically tested accuracy of two formulations of Levander's (1988) stress-imaging technique for simulating a planar free surface in the 4th-order staggered-grid finite-difference schemes. We have found that both formulations (one with normal stress-tensor components at the surface, the other with shear stress-tensor components at the surface) require at least 10 grid spacings per minimum wavelength (λmin÷h = 10) if Rayleigh waves are to be propagated without significant grid dispersion in the range of epicentral distances up to 15λdomS.Because interior 4th-order staggered-grid schemes usually do not require more than 6 grid spacings per minimum wavelength, in the considered range of epicentral distances, it was desirable to find alternative techniques to simulate a planar free surface, which would not require denser spatial sampling than λmin÷h = 6. Therefore, we have developed and tested new techniques: 1. Combination of the stress imaging (with the shear stress-tensor components at the surface) with Rodrigues' (1993) vertically refined grid near the free surface. 2. Application of the adjusted finite-difference approximations to the z-derivatives at the grid points at and below the surface that uses no virtual values above the surface and no stress imaging. The normal stress-tensor components are at the surface in one formulation, while the shear stress-tensor components are at the surface in the other formulation.The three developed formulations give for the spatial sampling λmin÷h = 6 results very close to those obtained by the discrete-wavenumber method. Because, however, the technique with the vertically refined grid near the free surface requires 3 times smaller time step (due to the refined grid), the technique with adjusted finite-difference approximations is the most accurate and efficient technique from the examined formulations in the homogeneous halfspace.

[1]  E. Husebye,et al.  3-D versus 2-D finite-difference seismic synthetics including real surface topography , 1999 .

[2]  Stig Hestholm,et al.  Three-dimensional finite difference viscoelastic wave modelling including surface topography , 1999 .

[3]  Bernard A. Chouet,et al.  A free-surface boundary condition for including 3D topography in the finite-difference method , 1997, Bulletin of the Seismological Society of America.

[4]  A. Levander Fourth-order finite-difference P-SV seismograms , 1988 .

[5]  Ellen Gottschämmer,et al.  Accuracy of the Explicit Planar Free-Surface Boundary Condition Implemented in a Fourth-Order Staggered-Grid Velocity-Stress Finite-Difference Scheme , 2001 .

[6]  Jean Virieux,et al.  SH-wave propagation in heterogeneous media: velocity-stress finite-difference method , 1984 .

[7]  S. Hestholm,et al.  2D surface topography boundary conditions in seismic wave modelling , 2001 .

[8]  J. Virieux P-SV wave propagation in heterogeneous media: Velocity‐stress finite‐difference method , 1986 .

[9]  José M. Carcione,et al.  Hybrid modeling of P-SV seismic motion at inhomogeneous viscoelastic topographic structures , 1997, Bulletin of the Seismological Society of America.

[10]  M. Bouchon A simple method to calculate Green's functions for elastic layered media , 1981 .

[11]  Ladislav Halada,et al.  3D Fourth-Order Staggered-Grid Finite-Difference Schemes: Stability and Grid Dispersion , 2000 .

[12]  R. Madariaga Dynamics of an expanding circular fault , 1976, Bulletin of the Seismological Society of America.

[13]  Peter Moczo,et al.  EFFICIENCY AND OPTIMIZATION OF THE 3-D FINITE-DIFFERENCE MODELING OF SEISMIC GROUND MOTION , 2001 .

[14]  Robert W. Graves,et al.  Simulating seismic wave propagation in 3D elastic media using staggered-grid finite differences , 1996, Bulletin of the Seismological Society of America.