Skip to main content

Monitoring of Deformation Processes by Means of Electric Field Observation

  • Conference paper
Mud Volcanoes, Geodynamics and Seismicity

Part of the book series: NATO Science Series ((NAIV,volume 51))

Abstract

Generation of the electrotelluric field (ETF) by geodynamic processes in the earth crust is considered. It is supposed that the ETF arises due to the electrokinetic effect caused by deformation of the earth crust. Based on this model, a new technique for ETF measurement is proposed. The possibility to use electrical fields caused by the tidal waves for calibration of the measurements is also considered. It is shown that the tidal variations of pore pressure and electrical fields essentially depend on medium permeability, porosity, and viscosity of a liquid. It is shown that by using observations of the vertical electrical field it is possible in principle to determine the mechanical properties of deformable medium. All effects reach a maximum near the earth surface and can be measured.

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

Access this chapter

Chapter
USD 29.95
Price excludes VAT (USA)
  • Available as PDF
  • Read on any device
  • Instant download
  • Own it forever
eBook
USD 169.00
Price excludes VAT (USA)
  • Available as PDF
  • Read on any device
  • Instant download
  • Own it forever
Softcover Book
USD 219.99
Price excludes VAT (USA)
  • Compact, lightweight edition
  • Dispatched in 3 to 5 business days
  • Free shipping worldwide - see info
Hardcover Book
USD 219.99
Price excludes VAT (USA)
  • Durable hardcover edition
  • Dispatched in 3 to 5 business days
  • Free shipping worldwide - see info

Tax calculation will be finalised at checkout

Purchases are for personal use only

Institutional subscriptions

Preview

Unable to display preview. Download preview PDF.

Unable to display preview. Download preview PDF.

References

  1. Sobisievich, L.E., Milyukov, V.K., Sobisievish, A.L. 2000. Mechanic-mathematical monitoring magmatic of structures of the Elbrus volcano. In: Geophysics and mathematicians, Moscow, 223–248.

    Google Scholar 

  2. Latynina, L.A., Karmaleeva, P.M., 1978. Deformografic of measurement. Moscow, Nauka.

    Google Scholar 

  3. Landau, L.D., Lifshits, E.M., 1982. Electrodynamics of continuous media. Moscow, Nauka.

    Google Scholar 

  4. Gershenzon, N. and Bambakidis, G., 2001. Modeling of seismo-electromagnetic phenomena, Russian Journal of Earth Sciences, 3, No 4, 247–275.

    Google Scholar 

  5. Detournay, E., Cheng, A. H.-D., 1993. Fundamentals of Poroelasticity, in Comprehensive Rock Engineering: Principle, Practice and Projects, Vol. II, Analysis and Design Method, Fairhurst, C. (ed.), Pergamon Press, 113–171.

    Google Scholar 

  6. Swolf, H.S., Walsh, J.B., 1990. The theory and prototype development of a stress-monitoring system., Bull. Seism. Soc. Amer., 80, No 1, 197–208.

    Google Scholar 

  7. Gershenzon, N. I., Gokhberg, M.B., 1994. On the origin of anomalous ultra low-frequency geomagnetic disturbances prior to Loma Prieta, California, earthquake. Phisics of the Solid Earth, 30, 112–118

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Editor information

Editors and Affiliations

Rights and permissions

Reprints and permissions

Copyright information

© 2005 Springer

About this paper

Cite this paper

Garagash, I.A., Gokhberg, M.B., Kolosnitsyn, N.I. (2005). Monitoring of Deformation Processes by Means of Electric Field Observation. In: Martinelli, G., Panahi, B. (eds) Mud Volcanoes, Geodynamics and Seismicity. NATO Science Series, vol 51. Springer, Dordrecht. https://doi.org/10.1007/1-4020-3204-8_15

Download citation

Publish with us

Policies and ethics