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  • 1
    Publication Date: 2021-06-22
    Description: The peripheral area of Stromboli Island, Italy, named “Scari”,was continuously studied between January 2009 and December 2010. Data on soil CO2 flux and the partial pressure of CO2 (pCO2) in equilibrium with the thermal aquifer linked to the magmatic system are presented. Soil CO2 fluxes range from 20 to 370 g m−2 d−1 and have been strongly affected by soil temperature variations. Soil CO2 flux data were filtered with respect to the soil temperature and the calculated values, called “residuals”, were considered to detect changes induced by the magmatic system. The pCO2 values change in a wide range from 0.03 to 0.6 (atm), showing rapid variations. The results of this study showthat in the volcanic peripheral area, the degassing process of soil CO2 is determined not only by the CO2 released directly from the magma but also by gas–water interactions in the aquifer. The aquifer is able to dissolve the high amount of CO2 discharged by the magmatic system. Moreover, the “residuals” of CO2 flux diffused from the soil show a delay on the order of ~1 month with respect to the pCO2 in equilibrium with the aquifer. The soil CO2 flux is therefore not directly linked to the uprising of magmatic CO2 but instead depends on the CO2 discharged fromthe aquifer, which buffers and modulates the volatile changes released by the magmatic system. © 2016 Elsevier B.V. All rights reserved
    Description: Istituto Nazionale di Geofisica e Vulcanologia – Palermo (INGV)
    Description: Published
    Description: 110-116
    Description: 4V. Dinamica dei processi pre-eruttivi
    Description: JCR Journal
    Keywords: Soil CO2 flux ; Gas-water interaction ; pCO2 in water Volcano-hydrothermal system ; Volcano-hydrothermal system ; natural degassing in volcanic peripheral areas
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 2
    Publication Date: 2021-06-22
    Description: Since 2016, Stromboli volcano has shown an increase of both frequency and energy of the volcanic activity; two strong paroxysms occurred on 3 July and 28 August 2019. The paroxysms were followed by a series of major explosions, which culminated on January 2021 with magma overflows and lava flows along the Sciara del Fuoco. This activity was monitored by the soil CO2 flux network of Istituto Nazionale di Geofisica e Vulcanologia (INGV), which highlighted significant changes before the paroxysmal activity. The CO2 flux started to increase in 2006, following a long-lasting positive trend, interrupted by short-lived high amplitude transients in 2016–2018 and 2018–2019. This increasing trend was recorded both in the summit and peripheral degassing areas of Stromboli, indicating that the magmatic gas release affected the whole volcanic edifice. These results suggest that Stromboli volcano is in a new critical phase, characterized by a great amount of volatiles exsolved by the shallow plumbing system, which could generate other energetic paroxysms in the future.
    Description: Published
    Description: 169
    Description: 4V. Processi pre-eruttivi
    Description: JCR Journal
    Keywords: Stromboli volcano; paroxysmal activity; soil CO2 fluxes
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 3
    Publication Date: 2020-09-10
    Description: Paroxysmal explosions are some of the most spectacular evidence of volcanism on Earth andare triggered by the rapid ascent of volatile-rich magma. These explosions often occur in persistentlyerupting basaltic volcanoes located in subduction zones and represent a major hazard due to thesudden occurrence and wide impact on the neighboring populations. However, the recognition ofsignals that forecast these blasts remains challenging even in the best-monitored volcanoes. Here, wepresent the results of the regular monitoring of soil CO2flux from a fumarole field at the summit ofStromboli (Italy), highlighting that the 2016–2019 period was characterized by two important phasesof strong increases of volatile output rate degassing (24 g m2d−2and 32 g m2d−2, respectively)and moreover by significant changes in the degassing style few months before the last paroxysmalexplosions occurred in the summer 2019 (3 July and 28 August). Establish that the deep portionsof a volcano plumbing system are refilled by new volatiles-rich magma intruding from the mantleis therefore a key factor for forecasting eruptions and helping in recognizing possible precursors ofparoxysmal explosions and could be highlighted by the monitoring of soil CO2flux. The abruptincrease of degassing rate coupled with the strong increase of fluctuating signal (daily naturaldeviation) recorded during 2019 at Stromboli could be the key to predicting the occurrence ofparoxysmal events.
    Description: Published
    Description: id 4757
    Description: 4V. Processi pre-eruttivi
    Description: JCR Journal
    Keywords: Stromboli volcano; geochemical monitoring; CO2degassing; paroxysmal activity
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 4
    Publication Date: 2020-03-06
    Description: The last increased volcanic activity of the Stromboli volcano, from 2016 to 2018, was characterized by increases in the number and frequency of crater explosions and by episodes of lava overflow. The volcanic activity was monitored utilizing CO2 soil fluxes acquired from the Stromboli summit area (STR02 station). To better understand the behavior of the shallow plumbing system of the Stromboli volcano in the period of 2016–2018, we utilized a large data set spanning from 2000 to 2018. The data in this last period confirm a long growing trend of CO2 summit degassing, already observed in the years since 2005 (reaching 23,000 g m􀀀2 d􀀀1). Moreover, within this increasing trend, episodes of sudden and sharp increases in the degassing rate, up to 24.2 g m􀀀2 d􀀀2 were recorded, which are correlated with the observed paroxysmal activity (increased summit explosions and overflow).
    Description: Published
    Description: id 176
    Description: 4V. Processi pre-eruttivi
    Description: JCR Journal
    Keywords: Stromboli volcano; geochemical monitoring; summit soil; CO2 degassing; Strombolian activity
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 5
    Publication Date: 2022-03-14
    Description: On Vulcano Island (Italy), many geochemical crises have occurred during the last 130 years of solfataric activity. The main crises occurred in 1978–1980, 1988–1991, 1996, 2004–2007, 2009–2010 and the ongoing 2021 anomalous degassing activity. These crises have been characterized by early signals of resuming degassing activity, measurable by the increase of volatiles and energy output emitted from the summit areas of the active cone, and particularly by increases of gas/water ratios in the fumarolic area at the summit. In any case, a direct rather than linear correspondence has been observed among the observed increase in the fluid output, seismic release and ground deformation, and is still a subject of study. We present here the results obtained by the long-term monitoring (over 13 years of observations) of three extensive parameters: the SO2 flux monitored in the volcanic plume, the soil CO2 flux and the local heat flux, monitored in the mild thermal anomaly located to the east of the high-temperature fumarole. The time variations of these parameters showed cyclicity in the volcanic degassing and a general increase in the trend in the last period. In particular, we focused on the changes in the mass and energy output registered in the period of June–December 2021, to offer in near-real-time the first evaluation of the level and duration of the actual exhalative crisis affecting Vulcano Island. In this last event, a clear change in degassing style was recorded for the volatiles emitted by the magma. For example, the flux of diffused CO2 from the soils reached the maximum never-before-recorded value of 34,000 g m−2 d −1 and the flux of SO2 of the plume emitted by the fumarolic field on the summit crater area reached values higher than 200 t d−1 . The interpretation of the behavior of this volcanic system, resulting from the detailed analyses of these continuous monitoring data, will complete the framework of observations and help in defining and possibly forecasting the next evolution of the actual exhaling crisis.
    Description: This research was funded by the INGV-DPCN (Italian National Institute of Geophysics and Volcanology—Italian National Department for Civil Protection) volcanic surveillance program of Vulcano island, ObFu 0304.010. Moreover, this investigation was partially funded by the TORS project in the framework of institutional INGV projects “Ricerca Libera” ObFu 9999.549; and Pianeta Dinamico Task V2, ObFu 1020.010.
    Description: Published
    Description: 1283
    Description: 4V. Processi pre-eruttivi
    Description: JCR Journal
    Keywords: : SO2 flux; CO2 flux; heat flux; Vulcano Island; geochemical crisis; extensive parameters
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 6
    Publication Date: 2021-11-09
    Description: Stromboli volcano is characterized by a persistent strombolian activity thatwas interrupted by effusive eruptions in 1985, 2002–2003, 2007, and 2014. The considerable amount of soil CO2 flux data acquired by the continuous geochemical network installed in the summit and peripheral areas of Stromboli Island have allowed us to thoroughly investigate and to model the plumbing system. This study analyzed 16 years of soil CO2 fluxes from the summit area, which showed a wide range of values (from 2000 to 85,000 g m−2 day−1). A set of discontinuous pCO2 data (ranging from 0.1 to 0.35 atm) from a dedicated thermal well (COA) drilled in the Stromboli village has been taken into account for the peripheral degassing evaluation. One of the major accomplishments of this study is the confirmation of the previous formulated geochemical model based on of the soil CO2 fluxes database and the recent effusive eruptions. The analysis of soil summit degassing data recorded at the summit STR02 station throughout the monitoring period (2000–2015) revealed that the log(CO2 flux) values conformed to a polimodal distribution with different mean values of CO2 fluxes being recorded for each sub-period during the different effusive eruptions. The three selected periods (2000–2004, 2005–2010, and 2011–2015) were characterized by considerable increases in soil CO2 degassing coinciding with the periods of effusive eruptions, indicating volatiles overpressure and disequilibrium of the volcanic system. Moreover, the CO2 output evaluations based on soil CO2 fluxes and pCO2 values of thermal waters (COA), have showed a long increasing trend both in the summit and peripheral areas. From 2007 to 2014, culminating in the last effusive eruption (August–November 2014).
    Description: Published
    Description: 69-84
    Description: 3V. Proprietà dei magmi e dei prodotti vulcanici
    Description: 6V. Pericolosità vulcanica e contributi alla stima del rischio
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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