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Eur. Phys. J. Appl. Phys. 47, 12705 (2009)
DOI: 10.1051/epjap:2008186
Seismo-ionosphere detection by underground SQUID in low-noise environment in LSBB-Rustrel, France
G. Waysand1, P. Barroy2, R. Blancon3, S. Gaffet4, C. Guilpin5, J. Marfaing6, E.P. Di Borgo3, M. Pyée7, M. Auguste1, D. Boyer1 and A. Cavaillou11 Université de Nice Sophia-Antipolis, Observatoire de la Côte d'Azur, Laboratoire Souterrain Bas Bruit de Rustrel-Pays d'Apt (LSBB), La Grande Combe, 84400 Rustrel, France
2 Université Paris XIII, LPMTM, Institut Galilée, 93430 Villetaneuse, France
3 Université d'Avignon et des Pays de Vaucluse, Département de Physique, Rue Louis Pasteur, 84000 Avignon, France
4 Université de Nice Sophia-Antipolis, GéoSciences-Azur, 250 rue Albert Einstein, 06500 Sophia-Antipolis, France
5 Université Paris7-Denis Diderot, 2 Place Jussieu, 75005 Paris, France
6 Universites Aix-Marseille IM2NP, UMR 6242 CNRS, Faculté des Sciences et Techniques, Avenue Normandie Niemen, 13397 Marseille Cedex 20, France
7 Université d'Orléans, LPCE CNRS, 3A av. de la Recherche Scientifique, 45071 Orléans, France
georges.waysand@oca.eu
Received: 30 May 2008 / Received in final form: 4 July 2008 / Accepted: 14 October 2008 / Published online: 17 February 2009
Abstract
The permanent operation of a 3 axes
SQUID magnetometer in the LSBB below 550 m of calcite rock is a unique system
of magnetic observation: a rejection rate better than 3 fT/
Hz over
40 Hz. The observation of magneto-ionosphere responses to P wave emissions
both at the epicentre and at their arrival at LSBB for earthquakes of
magnitude larger than 3 is reported. A simple model predicts the starting
time of these events. These results are compared with those provided by
Doppler sounders for ionosphere responses to Rayleigh waves.
91.10.Vr - Ocean/Earth/atmosphere/ hydrosphere/cryosphere interactions; mass balance.
94.20.Bb - Wave propagation.
85.25.Dq - Superconducting quantum interference devices (SQUIDs).
© EDP Sciences 2009
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