Environmental seismology: What can we learn on earth surface processes with ambient noise?
Environmental seismology consists in studying the mechanical vibrations that originate from, or that have been affected by external causes, that is to say causes outside the solid Earth. This includes for instance the coupling between the solid Earth and the cryosphere, or the hydrosphere, the anthr...
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Published in | Journal of applied geophysics Vol. 116; pp. 62 - 74 |
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Main Authors | , , , , , , , , , , , |
Format | Journal Article |
Language | English |
Published |
Elsevier B.V
01.05.2015
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Subjects | |
Online Access | Get full text |
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Abstract | Environmental seismology consists in studying the mechanical vibrations that originate from, or that have been affected by external causes, that is to say causes outside the solid Earth. This includes for instance the coupling between the solid Earth and the cryosphere, or the hydrosphere, the anthroposphere and the specific sources of vibration developing there. Environmental seismology also addresses the modifications of the wave propagation due to environmental forcing such as temperature and hydrology. Recent developments in data processing, together with increasing computational power and sensor concentration have led to original observations that allow for the development of this new field of seismology. In this article, we will particularly review how we can track and interpret tiny changes in the subsurface of the Earth related to external changes from modifications of the seismic wave propagation, with application to geomechanics, hydrology, and natural hazard. We will particularly demonstrate that, using ambient noise, we can track 1) thermal variations in the subsoil, in buildings or in rock columns; 2) the temporal and spatial evolution of a water table; 3) the evolution of the rigidity of the soil constituting a landslide, and especially the drop of rigidity preceding a failure event.
•Ambient seismic noise based monitoring reveals feeble perturbations of the subsurface.•Mechanical perturbations are related to temperature, stress, hydrological changes, or to damage.•Seismic noise from rivers and glaciers reveal new sources of seismic activity.•Glacier and fluvial seismology shed a new light on the mechanical process at work. |
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AbstractList | Environmental seismology consists in studying the mechanical vibrations that originate from, or that have been affected by external causes, that is to say causes outside the solid Earth. This includes for instance the coupling between the solid Earth and the cryosphere, or the hydrosphere, the anthroposphere and the specific sources of vibration developing there. Environmental seismology also addresses the modifications of the wave propagation due to environmental forcing such as temperature and hydrology. Recent developments in data processing, together with increasing computational power and sensor concentration have led to original observations that allow for the development of this new field of seismology. In this article, we will particularly review how we can track and interpret tiny changes in the subsurface of the Earth related to external changes from modifications of the seismic wave propagation, with application to geomechanics, hydrology, and natural hazard. We will particularly demonstrate that, using ambient noise, we can track 1) thermal variations in the subsoil, in buildings or in rock columns; 2) the temporal and spatial evolution of a water table; 3) the evolution of the rigidity of the soil constituting a landslide, and especially the drop of rigidity preceding a failure event.
•Ambient seismic noise based monitoring reveals feeble perturbations of the subsurface.•Mechanical perturbations are related to temperature, stress, hydrological changes, or to damage.•Seismic noise from rivers and glaciers reveal new sources of seismic activity.•Glacier and fluvial seismology shed a new light on the mechanical process at work. |
Author | Baillet, Laurent Guillier, Bertrand Garambois, Stéphane Larose, Eric Carrière, Simon Massey, Chris Jongmans, Denis Gimbert, Florent Voisin, Christophe Guéguen, Philippe Walter, Fabian Bottelin, Pierre |
Author_xml | – sequence: 1 givenname: Eric surname: Larose fullname: Larose, Eric organization: ISTerre, CNRS, BP 53, 38041 Grenoble Cedex 9, France – sequence: 2 givenname: Simon surname: Carrière fullname: Carrière, Simon organization: ISTerre, CNRS, BP 53, 38041 Grenoble Cedex 9, France – sequence: 3 givenname: Christophe surname: Voisin fullname: Voisin, Christophe organization: ISTerre, CNRS, BP 53, 38041 Grenoble Cedex 9, France – sequence: 4 givenname: Pierre surname: Bottelin fullname: Bottelin, Pierre organization: ISTerre, CNRS, BP 53, 38041 Grenoble Cedex 9, France – sequence: 5 givenname: Laurent surname: Baillet fullname: Baillet, Laurent organization: ISTerre, CNRS, BP 53, 38041 Grenoble Cedex 9, France – sequence: 6 givenname: Philippe surname: Guéguen fullname: Guéguen, Philippe organization: ISTerre, CNRS, BP 53, 38041 Grenoble Cedex 9, France – sequence: 7 givenname: Fabian surname: Walter fullname: Walter, Fabian organization: ISTerre, CNRS, BP 53, 38041 Grenoble Cedex 9, France – sequence: 8 givenname: Denis surname: Jongmans fullname: Jongmans, Denis organization: ISTerre, CNRS, BP 53, 38041 Grenoble Cedex 9, France – sequence: 9 givenname: Bertrand surname: Guillier fullname: Guillier, Bertrand organization: ISTerre, CNRS, BP 53, 38041 Grenoble Cedex 9, France – sequence: 10 givenname: Stéphane surname: Garambois fullname: Garambois, Stéphane email: eric.larose@ujf-grenoble.fr organization: ISTerre, CNRS, BP 53, 38041 Grenoble Cedex 9, France – sequence: 11 givenname: Florent surname: Gimbert fullname: Gimbert, Florent organization: Seismological Laboratory, California Institute of Technology, Pasadena, CA, USA – sequence: 12 givenname: Chris surname: Massey fullname: Massey, Chris organization: GNS Science, Lower Hutt 5040, New Zealand |
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