The sensor is high sensitivity and high durability to detect the electric changes of alternative and direct components of electromotive forces (EMF) in the subsurface soils. Sensor construction is compact multi dipole system of cardinally new type of geoelectric observations. The idea underlying the project is proton permeation of geological structures laying beneath the sensor, which makes it available for recording of high and low electrical mobility phenomena in form of sudden changes in amplitude of electric signals recorded in the tectonosphere – atmosphere interface. The proposed study will allow the covering the region under study with grid of multielectrode observatories close to the faults, towns and villages which makes it available mapping electrical mobility phenomena through geological structure those of which in the proximity of measuring station. Extracting rich informative content might spot characteristics of the geological structure transparent to proton flux in like electrical active and non-active (‘silence’) form. An electric ‘silence’ area is a narrow shaping form around forthcoming calamity. Supporting this approach, we have found that Pizzoli multielectrode observatory (30 km of EQ epicenter) has pointed at the SW boundary of the strong Norcia earthquake’s epicenter. There were no any abrupt subterranean electrical changes in 30 days time window before Norcia earthquake. We suppose that geological structures beneath Pizzoli observatory were not permeable to proton migration. But geological structures beneath Chieti station (80 km of EQ epicenter) were permeable for proton migration and therefore, nonstationary electric changes have been recorded. For purpose of situational awareness multielectrode observatories should be utilized across Northern, Central and Southern parts of Italy. We suggest that covering the region under study with grid of special multielectrode observatories closest to the fault line, towns and villages will extracting data and mapping a electric ‘silence’ area. Therefore, it gives the good hope to determinate dynamically within operative 30 days time window the location (coordinates) of next strong seismic catastrophe.

In-situ Cosmetecor multielectrode electric observations in Abruzzo region before M6.2 Norcia earthquake 24.08.2016. First results.

STOPPA, Francesco;
2016-01-01

Abstract

The sensor is high sensitivity and high durability to detect the electric changes of alternative and direct components of electromotive forces (EMF) in the subsurface soils. Sensor construction is compact multi dipole system of cardinally new type of geoelectric observations. The idea underlying the project is proton permeation of geological structures laying beneath the sensor, which makes it available for recording of high and low electrical mobility phenomena in form of sudden changes in amplitude of electric signals recorded in the tectonosphere – atmosphere interface. The proposed study will allow the covering the region under study with grid of multielectrode observatories close to the faults, towns and villages which makes it available mapping electrical mobility phenomena through geological structure those of which in the proximity of measuring station. Extracting rich informative content might spot characteristics of the geological structure transparent to proton flux in like electrical active and non-active (‘silence’) form. An electric ‘silence’ area is a narrow shaping form around forthcoming calamity. Supporting this approach, we have found that Pizzoli multielectrode observatory (30 km of EQ epicenter) has pointed at the SW boundary of the strong Norcia earthquake’s epicenter. There were no any abrupt subterranean electrical changes in 30 days time window before Norcia earthquake. We suppose that geological structures beneath Pizzoli observatory were not permeable to proton migration. But geological structures beneath Chieti station (80 km of EQ epicenter) were permeable for proton migration and therefore, nonstationary electric changes have been recorded. For purpose of situational awareness multielectrode observatories should be utilized across Northern, Central and Southern parts of Italy. We suggest that covering the region under study with grid of special multielectrode observatories closest to the fault line, towns and villages will extracting data and mapping a electric ‘silence’ area. Therefore, it gives the good hope to determinate dynamically within operative 30 days time window the location (coordinates) of next strong seismic catastrophe.
2016
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11564/681153
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