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Titel Space Earthquake Perturbation Simulation (SEPS) an application based on Geant4 tools to model and simulate the interaction between the Earthquake and the particle trapped on the Van Allen belt
VerfasserIn Filippo Ambroglini, William Jerome Burger, Roberto Battiston, Vincenzo Vitale, Yu Zhang
Konferenz EGU General Assembly 2014
Medientyp Artikel
Sprache Englisch
Digitales Dokument PDF
Erschienen In: GRA - Volume 16 (2014)
Datensatznummer 250099264
Publikation (Nr.) Volltext-Dokument vorhandenEGU/EGU2014-15024.pdf
 
Zusammenfassung
During last decades, few space experiments revealed anomalous bursts of charged particles, mainly electrons with energy larger than few MeV. A possible source of these bursts are the low-frequency seismo-electromagnetic emissions, which can cause the  precipitation of the electrons  from the lower boundary of their inner belt. Studies of these bursts reported also a short-term pre-seismic excess. Starting from  simulation tools traditionally  used on high energy physics we  developed a dedicated application SEPS (Space Perturbation Earthquake Simulation), based on the Geant4 tool and PLANETOCOSMICS program, able to model and simulate the electromagnetic interaction between the earthquake and the particles trapped in the inner Van Allen belt. With SEPS one can study the transport of  particles trapped in the Van Allen belts through  the Earth's magnetic field also taking into account possible interactions with the Earth's atmosphere. SEPS provides the possibility of: testing different models of interaction between electromagnetic waves and trapped particles, defining the mechanism of interaction as also shaping  the area in which this takes place,assessing the effects of perturbations in the magnetic field on the particles path, performing back-tracking analysis and also modelling  the interaction with electric fields. SEPS is in advanced development stage, so that it could be already exploited  to test in details the results of correlation analysis between particle bursts and earthquakes based on NOAA and SAMPEX data. The test was performed  both with a  full simulation analysis, (tracing from the position of the earthquake and going to see if there were paths compatible with the burst revealed)  and with a back-tracking analysis (tracing from the burst detection point and checking the compatibility with the position of associated earthquake).