1887

Abstract

Summary

Conventional two-point ray tracing in a general 3D heterogeneous medium is normally performed by a shooting method. The location and the slowness components are specified at the start point, and the ray path is the solution of ODEs with the initial conditions. The ray arrives to some proximity of the destination, and the start direction is then successively refined, so that the ray path eventually includes the destination point. Eigenray tracing, however, is a boundary-value problem, rather than an initial-value problem. The boundary conditions are two endpoint locations, and the ray trajectory satisfies Fermat’s principle of least traveltime. In this study, we apply the non-linear Finite Element Analysis to find the least-time ray path. The ray trajectory is split into a number of three-nodal segments with quadratic interpolation of trajectory points, traveltime and other functions between the nodes. For each segment, we compute the traveltime, and its first and second derivatives with respect to the nodal locations. The local derivatives (related to a single segment) are combined into the global derivatives of the entire path. For the least time, the first derivatives vanish. Knowledge of the second derivatives makes it possible to apply the Newton method for ray path optimization.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609.201801325
2018-06-11
2024-04-19
Loading full text...

Full text loading...

References

  1. Bóna, A., Slawinski, M., and Smith, P.
    [2009]. Ray tracing by simulated annealing: Bending method. Geophysics, 74, no. 2, T25–T32.
    [Google Scholar]
  2. Farra, V.
    [1992]. Bending method revisited: a Hamiltonian approach. Geophysical Journal International, 109, no. 1, 138–150.
    [Google Scholar]
  3. Moser, T.
    [1991]. Shortest path calculation of seismic rays, Geophysics, 56, no. 1, 59–67.
    [Google Scholar]
  4. Moser, T., Nolet, G., and Snieder, R.
    [1992]. Ray bending revisited, Bulletin of the Seismological Society of America, 82, no. 1, 259–288.
    [Google Scholar]
  5. Shashidhar, N., and Anand, G.
    [1995]. Eigenray tracing in an ocean using Fermat’s principle. Journal of Sound and Vibration, 186, no. 2, 231–243.
    [Google Scholar]
  6. Sripanich, Y., and Fomel, S.
    [2014]. Two-point seismic ray tracing in layered media using bending, SEG Technical Program Expanded Abstracts, 453–457.
    [Google Scholar]
  7. Waltham, D.
    [1988]. Two-point ray tracing using Fermat’s principle. Geophysical Journal International, 93, no. 3, 575–582
    [Google Scholar]
  8. Westwood, E., and Vidmar, P.
    [1987]. Eigenray funding and time series simulation in a layered-bottom ocean. The Journal of the Acoustical Society of America, 81, no. 4, 912–924.
    [Google Scholar]
http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201801325
Loading
/content/papers/10.3997/2214-4609.201801325
Loading

Data & Media loading...

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