Skip to main content
Log in

The splitting of the free oscillations of the Earth caused by the rheology

La moltiplicazione delle oscillazioni libere della Terra causata dalla reologia

  • Published:
Rendiconti Lincei Aims and scope Submit manuscript

Abstract

The knowledge of the rheological properties of the mantle of the Earth is one of the most important unsolved geophysical problems. Due to the strong depth dependence on temperature, composition, phase and pressure of the Earth, the study of the rheology is very difficult with the scarse information presently available and resulting mostly from surface waves and free modes decay. We report here of the new phenomenon of the splitting of the eigenfrequencies of the free modes of the Earth caused by the rheology. The separation of the lines of the predicted splitting is one order of magnitude larger than that caused by the flattening of the Earth. The observation of this splitting will produce new data for the determination of the rheology of the Earth.

Riassunto

La conoscenza delle proprietà Teologiche del mantello della terra è uno dei più importanti problemi della geofisica non ancora risolti. A causa della dipendenza di queste proprietà dalla temperatura, pressione, composizione e fasi delľinterno della terra, lo studio della reologia è molto difficile; esso è inoltre complicato ulteriormente dalla scarsità di informazioni oggi disponibili che risultano perloppiù dalľanalisi delle onde superficiali e delle oscillazioni libere. In questa nota si studia il fenomeno della moltiplicazione delle oscillazioni libere della terra causato dalla reologia calcolando la separazione delle righe spettrali che identificano i modi di oscillazione torsionale. Si trova che la separazione dei periodi di oscillazione è un ordine di grandezza maggiore di quella causata dallo schiacciamento terrestre e che pertanto la loro identificazione potrebbe essere possibile producendo nuovi dati per lo studio della reologia della terra.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Similar content being viewed by others

References

  • Alsop L. E., Sutton G. H. andEwing M., 1961.Free oscillations of the Earth observed on strain and pendulum seismographs. J. Geophys. Res., 66, 2: 631–641.

    Article  Google Scholar 

  • Bagley R. andTorvik P. J., 1983a.Fractional calculus: a different approach to the analysis of viscoelastically damped structures. Amer. Inst. Astron. Aeron. J., 21, 5: 741–748.

    Google Scholar 

  • Bagley R. andTorvik P. J., 1983b.A theoretical basis for the application of fractional calculus to viscoelasticity. J. of Rheology, 27, 3: 201–210.

    Article  CAS  Google Scholar 

  • Bagley R. andTorvik P. J., 1986.On the fractional calculus model of viscoelastic behavior. J. of Rheology, 30, 1: 133–155.

    Article  CAS  Google Scholar 

  • Bozzi Zadro M. andCaputo M., 1968.Spectral, bispectral analysis and Q of the free oscillations of the Earth. Suppl. Nuovo Cimento, 6: 67–81.

    Google Scholar 

  • Caputo M., 1963.Free modes of layered oblate planets. J. Geophys. Res., 68, 2: 497–503.

    Article  Google Scholar 

  • Caputo M., 1966.Linear models of dissipation whose Q is almost frequency independent. Annali di Geofisica, 21, 4: 383–393.

    Google Scholar 

  • Caputo M., 1967.Linear models of dissipation whose Q is almost frequency independent 2. Geophys. J. R. astr. Soc., 13: 529–539.

    Google Scholar 

  • Caputo M., 1989.The rheology of an anelastic medium studied by means of the splitting of its eigenfrequencies. J. Acoust. Soc. Am., in press.

  • Körntg M. andMüller G., 1989.Rheological models and interpretation of postglacial uplift. Geophysical Journal, 98: 243–253.

    Article  Google Scholar 

  • McDonald G. J. F. andNess N., 1961.A study of the free oscillations of the Earth. J. Geophys. Res., 66: 1865–1911.

    Article  Google Scholar 

  • Slichter L. B., McDonald G. J. F., Caputo M. andHager C. L., 1964.Report of Earth tide results and of other gravity results at UCLA. Obs. Royal Belgique, Comm. 236, Serie Geophys., 69: 124–130.

    Google Scholar 

  • Slighter L. B., 1968. Personal Communication.

  • Smith S., 1961.An investigation of the Earth’s free oscillation. Thesis Calif. Inst, of Technology, Pasadena.

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Additional information

Presentata nella seduta del 18 novembre 1989.

Rights and permissions

Reprints and permissions

About this article

Cite this article

Caputo, M. The splitting of the free oscillations of the Earth caused by the rheology. Rend. Fis. Acc. Lincei 1, 119–125 (1990). https://doi.org/10.1007/BF03001886

Download citation

  • Issue Date:

  • DOI: https://doi.org/10.1007/BF03001886

Key words

Navigation