1887
Volume 24, Issue 3-4
  • ISSN: 0812-3985
  • E-ISSN: 1834-7533

Abstract

Conventional methods of treating boundaries in finite difference () migration, namely padding in both space and time, have the disadvantage of increasing the data volume. This increase, whilst acceptable for 2-D processing, becomes uneconomical in the 3-D arena. Dipping events move up-dip during the migration process. Dips close to the sides of the data that move outside the data range can be reflected back if the boundary conditions are poorly set. This results in misleading events appearing in the migrated data. The addition of extra zero trace padding allows these events to move out of the data and so avoids these artefacts.

The alternative to padding with zero traces is to use absorbing side boundary conditions. Absorbing sides have been proposed by several authors. A method developed by Clayton and Engquist is reviewed in detail, and implementation issues are discussed. Although this method is exact for only one propagation angle, it is found to attenuate significantly the reflections of other dipping events.

Time padding is used to avoid the wraparound that causes shallow data to reappear as noise at later times in the migrated result. Wraparound is inherent in () finite difference migration, because of the cyclic nature of the fast Fourier transform. The time padding increases the run time of both the fast Fourier transform and the migration.

Clearly, it is desirable to find a technique to remove the wraparound and so avoid the need for costly time padding. Kjartansson showed a method for wraparound removal for the case when the sampling interval is equal to the migration time step or depth interval. In practice, however, a coarser time step is usually employed. A new generalised method has been developed for wraparound removal under these conditions of coarse time step. The technique is applied at each time step extrapolation. Although this obviously involves more computation, the method is more efficient than using extra time padding.

Both these techniques, the absorbing side boundaries and the wraparound removal, can be used in 2-D and one-pass 3-D implementations. Without the need for extra padding, migration run times and hence costs are reduced. The methods are demonstrated on synthetic data. The results compare well with those obtained using conventional padding, with a considerable reduction in run time.

Loading

Article metrics loading...

/content/journals/10.1071/EG993521
1993-09-01
2026-01-16
Loading full text...

Full text loading...

References

  1. Bracewell, R.N. (1985), The Fourier Transform and its Applications, McGraw-Hill p.104.
  2. Cerjan, C., Kosloff, D., Kosloff, R. and Reshef, M. (1985), ‘A nonreflecting boundary condition for discrete acoustic and elastic wave equations’, Geophysics50, 705–708.
  3. Claerbout, J.F. (1985), Imaging the Earth’s interior, Blackwell Scientific Publications.
  4. Clayton, R.W. and Engquist, B. (1977), ‘Absorbing boundary conditions for acoustic and elastic wave equations’, SSABulletin67, 1529–1540.
  5. Clayton, R.W. and Engquist, B. (1980), ‘Absorbing boundary conditions for wave-equation migration’, Geophysics45, 895–904.
  6. Kjartansson, E. (1978), ‘Modeling and migration with the monochromatic wave equation — variable velocity and attenuation’, Stanford Exploration Project15, 1–19.
  7. Reynolds, A.C. (1978), ‘Boundary conditions for the numerical solution of wave propagation problems’, Geophysics43, 1099–1110.
/content/journals/10.1071/EG993521
Loading
  • Article Type: Research Article
Keyword(s): boundary conditions; finite difference migration; wraparound.

Most Cited This Month Most Cited RSS feed

This is a required field
Please enter a valid email address
Approval was a Success
Invalid data
An Error Occurred
Approval was partially successful, following selected items could not be processed due to error