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  • 11
  • 12
    Publication Date: 1998-04-01
    Print ISSN: 0969-8043
    Electronic ISSN: 1872-9800
    Topics: Energy, Environment Protection, Nuclear Power Engineering
    Published by Elsevier
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  • 13
    Publication Date: 2020-12-07
    Description: The main aim of this work is to recognize the occurrence of seismic VT activity and its discrimination among other active and persistent natural and/or artificial sources, such as meteo-marine and anthropogenic noise. This task is of interest because it would support the routine practices of the observatories, considering that on the hourly scale events of very small energy are often completely hidden and not even the tedious work of operators can be resolved. To achieve that goal we adopt a robust automatic method, namely the Convolutive Independent Component Analysis (CICA), which in involves higher-order statistics in frequency domain. This technique is successful in seismological framework in the case of seismic signals, which can be considered as the convolution of time delayed source signals. In this work, we focus on Volcano Tectonic (VT) activity at Campi Flegrei Caldera (Italy) during the 2006 ground uplift. The activity is characterized approximately by 300 low-magnitude (Md 〈 2; for the definition of duration magnitude, see Petrosino et al., [2008]) VT earthquakes. Most of them were concentrated in distinct seismic sequences with hypocentres mainly clustered beneath the Solfatara-Accademia area, at depths ranging between 1 and 4 km b.s.l.. CICA is fruitfully applied to massive data on hourly scale obtaining a separation among different independent sources. Specifically, the identification of meteo-marine (〈 1 Hz), anthropogenic noise (mainly affecting [8-14] Hz frequency range), and hydrothermal tremor (at about 0.8 Hz) is achieved in absence of VT activity, defining the background level. Variations of that underlying condition appear in approaching to the period of intense low-energy VT activity. Namely, a further component in 13-15 Hz compatible with the typical corner frequency of VTs is extracted. We propose a coarse-grained procedure directly applied to massive data separated through CICA, which would provide fast alert on the occurrence of even very-small VTs representing a suitable “observable” to monitor in the observatory practice.
    Description: Published
    Description: Naples
    Description: 8T. Sismologia in tempo reale
    Keywords: Campi Flegrei ; ICA
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Conference paper
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  • 14
    Publication Date: 2020-11-17
    Description: We analyze the volcano seismicity recorded during the 2007 eruption of Stromboli. Data-set is composed of the continuous recordings of a three-component broad-band seismometer and of a strainmeter. Starting from the characterization of the standard activity as a stationary phase of equilibrium, we investigate the non-equilibrium phase of the effusive process. A statistical analysis of the explosions reveals that the occurrence is always driven by a Poisson process as for the standard activity, even approaching the effusion phase, with the only difference in shortening the inter-times just during the effusion. A slightly different process can be advocated for the swarms of the explosions, because a maximum in the distribution of inter-times can be evidenced. Regarding the amplitudes of the explosion-quakes, they have a log-normal distribution until the effusion onset as in the standard Strombolian activity. The actual departure from that stationarity seems to be traced by an early deformative response at very long period. It appears as a transient oscillating signal characterized by a period of about three days that modulates the explosion amplitudes. In a conceptual organ pipe-like model it is related to the chocking of the pipe. The successive activity can be interpreted as the response of volcano to restore the equilibrium condition.
    Description: Published
    Description: B09312
    Description: 1V. Storia eruttiva
    Description: JCR Journal
    Description: open
    Keywords: Stromboli ; eruption ; 04. Solid Earth::04.06. Seismology::04.06.08. Volcano seismology
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 15
    Publication Date: 2020-12-07
    Description: A novel procedure is proposed in order to analyse continuous seismic signal on hourly scale to have a prompt discrimination among the different sources. The case study regards the Campi Flegrei caldera during the year 2006 when a swarm of volcano-tectonic earthquakes occurred. The necessity to analyse a massive data set has required applying a robust methodology and the introduction of suitable parameters to be monitored over the time. Specifically we apply the Convolutive Independent Component Analysis to the seismic recording at four broadband stations. As a result, we obtain a clear separation among meteo-marine, anthropogenic noise, hydrothermal tremor in absence of volcano-tectonic activity, whereas in non-stationary conditions a contribution connected to the corner frequency of the earthquakes emerges. We introduce a coarse-grained variable to be monitored continuously, i.e. the frequency associated with the maximum amplitude of the power spectral density of the deconvolutive independent components. This parameter is sensitive to the variation in the frequency bands of interest (e.g. that corresponding to the corner frequencies of volcano-tectonic events) and can be used as marker of the insurgence of seismic activity. We propose the following procedure to be applied routinely in the observatory practice: namely, estimate CICs on hourly series; then represent the distribution of the FMPSDA. Significative variations in the frequency bands of interest can be indicative of the insurgence of a renewed activity (e.g. VTs). Once individuated the “hot” periods, then one can go deeper with finer distinctions at a single event scale by using a simple STA/LTA (Short Time Average vs. Long Time Average) technique in order to detect events. This coarse-grained procedure on massive data through CICA would provide fast alert on the occurrence of even very-small VTs and FMPSDA may represent a suitable “observable” to monitor in the observatory practice. Finally, this approach can be employed for the prompt detection in massive data of other kinds of seismic signals such as LP, tremor, fluid-induced seismicity buried in noisy environments.
    Description: Published
    Description: Rome
    Description: 8T. Sismologia in tempo reale
    Keywords: Campi Flegrei ; ICA
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Conference paper
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  • 16
    Publication Date: 2019-10-11
    Description: We show how to obtain a clear separation of seismic phases in volcanic environments. Specifically we investigated the Long-Period (LP) and Volcano Tectonic (VT) seismic signals recorded at Campi Flegrei Caldera (Italy). We adopt an innovative Independent Component Analysis (ICA) algorithm for mixed seismic series adapted and improved to give automatic procedures for detecting seismic events often buried in the high-level ambient noise. We reconstruct the radiation patterns of the extracted LP events in order to link the individuated signals directly to the sources. We take advantage from ICA that provides basic signals along the three directions of motion so that a direct polarization analysis can be performed with no other filtering procedures. We show that the extracted signals are mainly composed of P waves with radial polarization pointing to the seismic source of the main LP swarm, i.e. a small area in the Solfatara, also in the case of the small-events, that both precede and follow the main activity. From a dynamical point of view, they can be described by two degrees of freedom, indicating a low-level of complexity associated with the vibrations from a superficial hydrothermal system. Additionally, we also focus on VTs, obtaining a clear separation of P and S phases: the technique not only allows the identification of the interval time P-S giving the timing of both phases but also provides the independent waveforms of the P and S. The proposed approach (ICAP) can represent an useful tool to obtain the polarization properties on seismic signals both originated from the interaction fluid-solid or by the rock fracturing.
    Description: Published
    Description: Naples
    Description: 3T. Sorgente sismica
    Keywords: Campi Flegrei ; ICAP ; polarization
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Conference paper
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  • 17
    Publication Date: 2017-04-04
    Description: The Long-Period (LP) seismicity is common at active volcanoes and is usually modeled as due to pressurized magmatic fluids flowing through rock cavities. These signals are sensitive to the thermodynamic conditions of the magma-gas mixture in the shallow plumbing system and can thus be adopted as “detectors” of an impelling eruption. We found that at Stromboli (Italy) before and/or during recent volcanic crises the LP events can occur in swarms, which show different statistics, higher energy and shallower location than the stationary LP activity. We imputed the LP swarms to a quick depressurization (|ΔP|≥105 Pa) of the shallowest (〈0.8 km) part of the conduit. At Shishaldin (Alaska) the 2004 eruption is anticipated by a migration towards the surface of the LP source, which moves from ~8 km to ≾5 km below the crater rim. By simple assumptions, we modeled this source change as produced by an increase of the confining pressure within the plumbing system of ~5x107 Pa, possibly induced by an upward migration of ~108-1010 kg of magma.
    Description: Published
    Description: GFZ Potsdam
    Description: 4T. Fisica dei terremoti e scenari cosismici
    Description: open
    Keywords: Long-period events ; Volcano seismicity ; Eruption precursors ; 04. Solid Earth::04.06. Seismology::04.06.08. Volcano seismology
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Poster session
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  • 18
    Publication Date: 2019-10-11
    Description: Una delle sfide di grande interesse in sismologia vulcanica è inferire informazioni sulla sorgente sismica determinando, ad esempio, la geometria, la dinamica e l’evoluzione di sistemi vulcanici al fine di comprenderne comportamenti eruttivi e determinare parametri di rischio. Le informazioni relative alla sorgente sono dedotte da serie temporali spesso degradate dalla presenza di sorgenti concomitanti e/o spesso corrotte da alti livelli di rumore di fondo. Inoltre, il monitoraggio dell’attività di un vulcano richiede l’acquisizione di dati in continuo. Dati massivi in cui agiscono differenti sorgenti concomitanti rendono difficili le pratiche di osservatorio. Da qui la necessità di migliorare le procedure di early warning.... [continua nel file allegato]
    Description: Published
    Description: Lecce
    Description: 8T. Sismologia in tempo reale
    Keywords: Campi Flegrei ; ICA
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Conference paper
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  • 19
    Publication Date: 2019-10-11
    Description: We have investigated the seismic dynamical state of Ischia volcanic Island before and after the August 21, 2017 earthquake, by applying classical and innovative techniques to the background seismic noise. First, we searched for the presence of independent signal sources by performing the Independent Component Analysis (ICA). Over 60 days of recordings, from 26 August to 25 October 2017, the application of ICA algorithm successful separated two stable components: IC1, the most energetic and persistent, picked at ~1 Hz; and IC2, concentrated in 3-4 Hz band. The root mean square (RMS) of continuous recordings during three months of the years 2016 and 2017, was estimated in order to investigate coherence properties of the background seismic signal before and after the August 2017 earthquake, for both raw and filtered data in the frequency ranges corresponding to the two ICs. The results show no variations in the patterns. The polarization properties of the same dataset were obtained by applying the covariance matrix method. The polarization parameters were estimated by filtering the signals in the 1-2 and 3-4 Hz frequency bands. The time evolution of the mean values of the polarization pattern does not show any variation during the analysed time intervals. The statistical properties of the polarization pattern were further investigated by analysing the rose plots of the azimuth of the polarization vector. All the obtained results were interpreted taking into account the existing literature on volcanological, morphological, structural and geochemical studies. IC1 seems conditioned by tectonic and volcanic structures and by the Island morphology. It could be associated with the persistent activity of the hydrothermal system. The signal amplitude of IC2 clearly shows 24h periodicities, likely related to anthropogenic activities.
    Description: Published
    Description: Naples
    Description: 4V. Processi pre-eruttivi
    Keywords: Ischia ; ICA
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Conference paper
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  • 20
    Publication Date: 2020-04-09
    Description: This work is devoted to the study of both earthquakes and background seismic noise at Ischia Island (Italy) recorded pre and post the Md 4.0 earthquake occurred on 21 August 2017 (18:57 UTC). We compare and characterize noise and earthquakes in terms of Independent Component Analysis, energy and polarization properties. The earthquakes’ waveforms and the background noise are decomposed into a few independent components with two main common signals peaked around 1–2 and 3–4 Hz, respectively. A slight increase of the energy of the background seismic noise is observed comparing samples recorded in 2016 and 2017, whereas no variations are detected in 2017 pre and post the main earthquake. The polarization analysis, performed in the frequency bands individuated by Independent Component Analysis and applied to the background seismic noise, indicates a shallow propagation and the azimuthal pattern is mainly controlled by the local structural features. These results suggest that noise and earthquakes are ascribable to a common phenomenon of fluid-solid interaction in the hydrothermal system of Ischia Island.
    Description: Published
    Description: 19-28
    Description: 3T. Sorgente sismica
    Description: 4V. Processi pre-eruttivi
    Description: JCR Journal
    Keywords: Ischia volcano ; Source dynamics ; Data analysis ; 04.08. Volcanology ; 04.06. Seismology
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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