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Volume 7, issue 1 | Copyright
Solid Earth, 7, 249-284, 2016
https://doi.org/10.5194/se-7-249-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Review article 12 Feb 2016

Review article | 12 Feb 2016

A review on electrokinetically induced seismo-electrics, electro-seismics, and seismo-magnetics for Earth sciences

L. Jouniaux1 and F. Zyserman2 L. Jouniaux and F. Zyserman
  • 1Institut de Physique du Globe de Strasbourg, CNRS and Université de Strasbourg UMR7516, Strasbourg, France
  • 2CONICET and Facultad de Ciencias Astronómicas y Geofísicas, Universidad Nacional de La Plata, La Plata, Argentina

Abstract. The seismo-electromagnetic method (SEM) can be used for non-invasive subsurface exploration. It shows interesting results for detecting fluids such as water, oil, gas, CO2, or ice, and also help to better characterise the subsurface in terms of porosity, permeability, and fractures. However, the challenge of this method is the low level of the induced signals. We first describe SEM's theoretical background, and the role of some key parameters. We then detail recent studies on SEM, through theoretical and numerical developments, and through field and laboratory observations, to show that this method can bring advantages compared to classical geophysical methods.

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The seismo-electromagnetic method is used for non-invasive subsurface exploration, showing interesting results for detecting fluids such as water, oil, gas, CO2, or ice, and to better characterize the subsurface in terms of porosity, permeability, and fractures. We describe theoretical background, the role of key parameters, recent theoretical and numerical developments, and field and laboratory observations to show that this method can bring advantages compared to classical geophysical method.
The seismo-electromagnetic method is used for non-invasive subsurface exploration, showing...
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