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Soil radon concentration and effective stress variation at Mt. Etna (Sicily) in the period January 2003–April 2005
Affiliation:1. Dipartimento di Scienze Geologiche, Università degli Studi di Catania, Corso Italia 57, 95129 Catania, Italy;2. Osservatorio Meteorologico Geodinamico ed Ambientale, Via Paolo Vasta 158/c, 95024 Acireale (CT), Italy;3. Dipartimento di Fisica e Astronomia, Universita‘ di Catania, via S.Sofia, 64 I-95123 Catania, Italy
Abstract:In this study we discuss the relationship between the in-soil radon concentration and the effective stress variation at Mt. Etna volcano in the period January 2003–April 2005. The acquired radon concentration trend was compared with the one obtained by the b-value variation analysis in the frequency–magnitude relationship for earthquakes that occurred at Mt. Etna volcano (Sicily) during the investigation period. The b-value calculated using both the maximum likelihood and the least square methods shows a similar trend and, in particular, an increase starting a few months before the 7th September 2004 eruption and a decrease during the following 9 months. A similar trend was recorded during 2003 when a recharging magma phase of the volcano occurred. Results obtained by studying the b-value trend and the comparison with in-soil radon concentration are also discussed.
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