Nonstationary electrical activity in the tectonosphere-atmosphere interface retrieving by multielectrode sensors: case study of three major earthquakes in Central Italy with M>6

• Published in: Earth Science Informatics
• Main Authors: Bobrovskiy, V. S., Nicoli, L., Losyeva, Y., STOPPA, Francesco
• Other Authors: Stoppa, Francesco
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2017
• Subjects: Amatrice; Central Italy; Earthquake; Nonstationary electric proce; Proton permeability; Earth and Planetary Sciences (all); Kamchatka Peninsula; Kamchatka
• Online Access: http://hdl.handle.net/11564/681137; https://doi.org/10.1007/s12145-017-0296-4; http://www.springer.com/geosciences/computer+%26+mathematical+applications/journal/12145

We present data analysis of multi-electrode measurements performed in the tectonosphere-atmosphere interface at Pizzoli and Chieti observatories located at distances 30–50 km and 90–110 km from earthquakes epicenters in Central Italy accordingly. Time intervals include 30 days of observations before earthquakes occurred on 24 August (M6.2), on 26 October (M6.1) and on 30 October, 2016 (M6.6). The recorded signals are two component time series with time step 1 s representing alternative and direct electromotive force components. Alternative electromotive force component in frequency band of 0.01 Hz to 4000 Hz is being recorded. Basic study has been carried out since 1989 at Kamchatka peninsula and since 2012 across Eurasia. The observation of nonstationary electric processes illustrates the nucleation of seismogenetic activity. We propose the hypothesis that nonstationary (sudden, abrupt in amplitude) electrical signals illustrate the proton permeability of rocks laying underneath the measuring sensor including a unique phenomenon of anomalous spontaneous deformation due to combination of proton environment and polymorphic transformation in condensed media. One of the interesting results is distinguishing the main zone of major earthquake nucleation which is corresponding as the earthquakes epicenters in Central Italy with M > 6. We suggest that by covering the northern, central and southern parts of Italy with a network of multi-electrode observatories near fault lines, towns and villages could pinpoint the possible coordinates of earthquake epicenter in a 30 day time window. The Chieti and Pizzoli observatories can form the basis of an extended network.