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  5. Statistical moments of power spectrum: a fast tool for the classification of seismic events recorded on volcanoes
 
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Statistical moments of power spectrum: a fast tool for the classification of seismic events recorded on volcanoes

Author(s)
Galluzzo, Danilo  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia  
Nardone, Lucia  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia  
La Rocca, Mario  
Dipartimento di Biologia, Ecologia e Scienze della Terra, Università della Calabria, Via Pietro Bucci, 87036 Rende (CS), Italy  
Esposito, Antonietta  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia  
Manzo, Roberto  
DISTAR, Unina, Naples  
Di Maio, Rosa  
DISTAR, Unina, Naples  
Language
English
Obiettivo Specifico
1SR TERREMOTI - Sorveglianza Sismica e Allerta Tsunami
Status
Published
JCR Journal
N/A or not JCR
Peer review journal
Yes
Journal
Advances in Geosciences (ADGEO)  
Issue/vol(year)
/52 (2020)
ISSN
1680-7340
Publisher
EGU - Copernicus
Pages (printed)
67–74
Date Issued
2020
DOI
10.5194/adgeo-52-67-2020
URI
https://www.earth-prints.org/handle/2122/14314
Subjects
04.06. Seismology  
Subjects

Vesuvius

Spectral Analisys

Abstract
Spectral analysis has been applied to almost thou-sand seismic events recorded at Vesuvius volcano (Naples,southern Italy) in 2018 with the aim to test a new tool fora fast event classification. We computed two spectral pa-rameters, central frequency and shape factor, from the spec-tral moments of order 0, 1, and 2, for each event at sevenseismic stations taking the mean among the three compo-nents of ground motion. The analyzed events consist ofvolcano-tectonic earthquakes, low frequency events and un-classified events (landslides, rockfall, thunders, quarry blasts,etc.). Most of them are of low magnitude, and/or low maxi-mum signal amplitude, therefore the signal to noise ratio isvery different between the low noise summit stations andthe higher noise stations installed at low elevation aroundthe volcano. The results of our analysis show that volcano-tectonic earthquakes and low frequency events are easily dis-tinguishable through the spectral moments values, particu-larly at seismic stations closer to the epicenter. On the con-trary, unclassified events show the spectral parameters valuesdistributed in a broad range which overlap both the volcano-tectonic earthquakes and the low frequency events. Since thecomputation of spectral parameters is extremely easy and fastfor a detected event, it may become an effective tool for eventclassification in observatory practice.
Type
article
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adgeo-52-67-2020.pdf

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Checksum (MD5)

18d0d75446cc7dda1dc5abe2cde7b2ba

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