Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/10324
AuthorsMasci, F.* 
Thomas, J. N.* 
TitleEvidence of underground electric current generation during the 2009 L’Aquila earthquake: Real or instrumental?
Issue Date14-Jul-2016
Series/Report no./43 (2016)
DOI10.1002/2016GL069759
URIhttp://hdl.handle.net/2122/10324
KeywordsEarthquake
seismoelectric effect
Subject Classification04. Solid Earth::04.05. Geomagnetism::04.05.99. General or miscellaneous 
04. Solid Earth::04.05. Geomagnetism::04.05.04. Magnetic anomalies 
04. Solid Earth::04.05. Geomagnetism::04.05.08. Instruments and techniques 
AbstractWe 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).
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