Skip to main content
U.S. Department of Energy
Office of Scientific and Technical Information

Elimination of numerical dispersion in finite-difference modeling and migration by flux-corrected transport

Technical Report ·
DOI:https://doi.org/10.2172/10108205· OSTI ID:10108205
Finite-difference acoustic-wave modeling and reverse-time depth migration based on the full wave equation are general approaches that can take into account arbitary variations in velocity and density, and can handle turning waves well. However, conventional finite-difference methods for solving the acousticwave equation suffer from numerical dispersion when too few samples per wavelength are used. Here, we present two flux-corrected transport (FCT) algorithms, one based the second-order equation and the other based on first-order wave equations derived from the second-order one. Combining the FCT technique with conventional finite-difference modeling or reverse-time wave extrapolation can ensure finite-difference solutions without numerical dispersion even for shock waves and impulsive sources. Computed two-dimensional migration images show accurate positioning of reflectors with greater than 90-degree dip. Moreover, application to real data shows no indication of numerical dispersion. The FCT correction, which can be applied to finite-difference approximations of any order in space and time, is an efficient alternative to use of approximations of increasing order.
Research Organization:
Colorado School of Mines, Golden, CO (United States). Center for Wave Phenomena
Sponsoring Organization:
USDOE, Washington, DC (United States)
DOE Contract Number:
FG02-89ER14079
OSTI ID:
10108205
Report Number(s):
DOE/ER/14079--30; CWP--142P; ON: DE94004159; BR: KC0403010
Country of Publication:
United States
Language:
English

Similar Records

Elimination of numerical dispersion in finite-difference modeling and migration by flux-corrected transport
Journal Article · Tue Oct 31 23:00:00 EST 1995 · Geophysics · OSTI ID:175961

Seismic modeling and reverse-time depth migration by flux-corrected transport
Technical Report · Thu Dec 31 23:00:00 EST 1992 · OSTI ID:6789377

Seismic modeling and reverse-time depth migration by flux-corrected transport
Technical Report · Thu Dec 31 23:00:00 EST 1992 · OSTI ID:10124847