1887
Volume 36 Number 4
  • E-ISSN: 1365-2478

Abstract

ABSTRACT

The quantity of energy that is radiated as sound by marine seismic sources is examined. When more than one source is used, the total radiated acoustic energy depends on the separation of the sources and is not constant, even when the separation is sufficiently large that the individual signatures are substantially unaffected. We believe that this long‐range interaction has not been described before in the literature and have called it energy‐interaction.

The existence of energy‐interaction is demonstrated experimentally for airguns. In. the experiment presented, the acoustic output is more than doubled because of energy‐interaction.

Two methods are described for computing the energy of the wavefield of an array of sources. One method is simple and direct; the energy that is radiated into the far field is calculated by integrating the directivity pattern over all directions. The other method finds the energy that is radiated into the near field. Because the medium is assumed lossless, these two energies are the same. Although the near‐field method is conceptually more difficult, it is faster, more accurate and provides a more detailed description of the energy budget.

Loading

Article metrics loading...

/content/journals/10.1111/j.1365-2478.1988.tb02167.x
2006-04-27
2024-04-18
Loading full text...

Full text loading...

References

  1. BERKHOUT, A.J.1982. Seismic Migration: Imaging Acoustic Energy by Wavefield Extrapolation, A, Theoretical Aspects.Elsevier Science Publishing Co.
    [Google Scholar]
  2. FUJIKAWA, S. and TAKAHIRA, H.1986. Interaction between two spherical bubbles. Acustica61, 188–199.
    [Google Scholar]
  3. KINSLER, L., FREY, R., COPPENS, B. and SANDERS, V.1982. Fundamentals of Acoustics.John Wiley and Sons, Inc.
    [Google Scholar]
  4. LOVERIDGE, M.M.1985. Marine seismic signatures: directivity and the ghost. Ph.D. thesis, University of Oxford .
  5. NOOTEBOOM, J.1978. Signature and amplitude of linear airgun arrays. Geophysical Prospecting26, 194–201.
    [Google Scholar]
  6. PARKES, G.E. and HATTON, L.1986. The Marine Seismic Source.D. Reidel, The Netherlands .
    [Google Scholar]
  7. PARKES, G.E., ZIOLKOWSKI, A.M., HATTON, L. and HAUGLAND, T.‐A.1984. The signature of an airgun array: computation from near‐field measurements including interactions‐practical considerations. Geophysics49, 105–111.
    [Google Scholar]
  8. PROSPERETTI, A.1984. Bubble phenomena in sound fields: part one. Ultrasonics22, 69–77.
    [Google Scholar]
  9. SAFAR, M.1976a. The radiation of acoustic waves from an airgun. Geophysical Prospecting24, 756–772.
    [Google Scholar]
  10. SAFAR, M.1976b. Efficient design of airgun arrays. Geophysical Prospecting24, 773–787.
    [Google Scholar]
  11. VAAGE, S., URSIN, B. and HAUGLAND, K.1984. Interaction between airguns. Geophysical Prospecting32, 676–689.
    [Google Scholar]
  12. ZIOLKOWSKI, A.M., PARKES, G.E., HATTON, L. and HAUGLAND, T.‐A.1982. The signature of an airgun array: computation from near‐field measurements including interactions. Geophysics47, 1413–1421.
    [Google Scholar]
http://instance.metastore.ingenta.com/content/journals/10.1111/j.1365-2478.1988.tb02167.x
Loading
  • Article Type: Research Article

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