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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/10324

Authors: Masci, F.*
Thomas, J. N.*
Title: Evidence of underground electric current generation during the 2009 L’Aquila earthquake: Real or instrumental?
Title of journal: Geophysical Research Letters
Series/Report no.: /43 (2016)
Publisher: American Geophysical Union
Issue Date: 14-Jul-2016
DOI: 10.1002/2016GL069759
URL: http://onlinelibrary.wiley.com/doi/10.1002/2016GL069759/abstract
Keywords: Earthquake
seismoelectric effect
Abstract: We investigate magnetic effects in correspondence of the Mw6.1 L’Aquila earthquake. Magnetic and seismic records are analyzed. Rapid and distinct changes and an offset can be seen in magnetic field components after the main shock. We show that these effects result from electromagnetic induction due to the movement of the sensors through the Earth’s magnetic field and from a permanent displacement of the sensors from their original position caused by the passing seismic waves. A transient signal in total field data from an overhauser magnetometer apparently occurs in correspondence with the earthquake. Our analysis shows that the transient was not observed by other sensors that were operating in close proximity to the overhauser. Thus, the transient signal in the total magnetic field data, and the offset in the magnetic field components, cannot be associated with a hypothetical underground electric current generated by the earthquake, as suggested by Nenovski (2015).
Appears in Collections:04.05.08. Instruments and techniques
04.05.99. General or miscellaneous
04.05.04. Magnetic anomalies
Papers Published / Papers in press

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