This is a seven-year study (1/7/2011-31/12/2017) of radon monitoring at two sites of Campi Flegrei caldera (Neaples, Southern Italy) that in the last 70 years experienced repeated phases of volcanic unrest. The sites are equipped with devices for radon detection, based on the spectrometry analysis of the α-particles of radon daughters. A hybrid method, as combination of three known methods, is applied for the identification of residuals (anomalies) and trends of the time series of Radon. The results are compared with the following indicators of current caldera unrest: the tremor caused by the major fumarolic vent registered by a seismic station; the cumulative of background seismicity; the maximum vertical deformation acquired by GPS networks during the current phase of uplift; the temperature-pressure of the hydrothermal system estimated based on gas geo-indicators. The comparisons show strong correlation among independent signals and suggest that the extension of the area affected by current Campi Flegrei crisis is larger than the area of seismicity and of intense hydrothermal activity from which the radon stations are 1–4 km away. These results represent an absolute novelty in the study of a such calderic area and mark a significant step forward in the use and interpretation of the radon signal.
Radon (222Rn) is a radioactive element with a half-life of 3.82 days, formed in the Earth’s Crust by the radioactive decay of 226Ra in the 238U decay series. Faults and fractures are preferential migration pathways for radon gas and carrier gases (CO2), from the deep layers of the Earth’s Crust to the surface1,2,3. The radon signal monitored in soils contains both local and remote information and is influenced by many environmental factors4,5,6,7. It is well established that radon can provide useful information if it is continuously recorded at a given site. The continuous monitoring allows us to characterize the local background signal and recognize the complete trends of local and remote effects on the signal8,9. The local effects due to sudden changes in temperature, pressure or water content in the soil (heavy rain or no rain for long periods) can be so predominant and often create large variations in the signal10,11,12 to hide components due to remote geophysical sources5,6,13,14,15,16.
In recent years, interest of the international scientific community towards the study of radon emission as a tracer of natural endogenous phenomena (seismic and volcanic activity) has considerably grown17,18,19,20,21,22,23,24,25,26,27,28,29,30,31,32,33.
The present study focuses on the analysis of radon activity concentration time series over a period of about seven years, from 1 July 2011 until 31 December 2017, obtained by continuous monitoring in soils at two sites of the Campi Flegrei caldera (Naples, Italy). The two sites are located in Monte Olibano, in the central area of the caldera, and Monte Sant’Angelo, where the Department of Physics ‘E. Pancini’ of the University of Naples “Federico II” is located (Fig. 1).
Campi Flegrei is a caldera of about 120 km2 located on a NE–SW-trending structure in the Campanian Plain. The caldera formed from the collapses associated to the large size eruptions of the Campanian Ignimbrite and of the Neapolitan Yellow Tuff34,35,36 (Fig. 1). The structural setting of Campi Flegrei is characterised by NE-SW and NW-SE trending faults that control the distribution of volcanic centres. Since the middle of the 20th century, the caldera has been subjected to a long-term crisis characterized by numerous episodes of ground uplift and correspondent seismic activity with a maximum total ground uplift of about 4 m in 1983–198437. After that period the caldera subsided until 2004–2005 when a new uplifting phase started. In the 2012–2013 period, there was an increase in the acceleration of the deformation of the soil in the caldera area38,39, interpreted as the effect of the intrusion at shallow depth38 of magma within a sill-like structure.
This renewed uplift is still ongoing and is accompanied by large variation in the degassing rate and fumarolic composition at Solfatara and by earthquakes mostly located at shallow depth (<2 km) in the subsoil of Solfatara40,41,42,43,44. The caldera is characterized by the emission of hydrothermal-volcanic fluids from both fumarolic vents, with temperature as high as 160–165 °C, and process of soil diffuse degassing. The associated deeply derived CO2 fluxes are considerably high being estimated in the range 1000–3000 tons/day40,41,42. The emission of geothermal fluids, both through diffuse degassing and vents, dominate the present-day Campi Flegrei caldera energy budget with the emission of several kilotons of vapour every day and with a cumulative thermal energy output of about 5 ∙ 1016 J45.
Here, the time series analysis of the radon signal was performed using a well-proven hybrid method that has successfully been applied to the identification of anomalies and trends in time series8,9,25,46,47,48,49. The hybrid method is formed by sequential aggregation of: (i) the Multiple Linear Regression (MLR) for filtering the known modulations out from the time series, (ii) the Empirical Mode Decomposition (EMD) techniques for the signal decomposition, and (iii) the Support Vector Regression (SVR) technique for forecasting the time series. The forecasting results are then used in comparison with raw time series in order to identify the anomalies (see Methods)8,9,25. The aim of this study is to investigate the trends and anomalies in the radon signals in comparison with other geo-indicators of the caldera unrest: seismicity, ground deformation44 and, for the first time in the literature, the seismic tremor of the main fumarole that has been identified as a powerful indicator of the changes affecting the hydrothermal system41,50.
Our analysis of the radon signal was focused on distinguishing and extracting the desired information including the estimation of the different components and trends and the recognition of the possible anomalies46,47,51,52. The analysis was performed using a hybrid method that aggregates multiple separate methods and combines the advantages of the single ones with optimized algorithms48,49,52,53,54, which are described in the Methods section.
The two daily time series (1/7/2011-31/12/2017) of 222Rn activity concentration in soils recorded at Monte Olibano (OLB) and Monte Sant’Angelo (MSA) stations are displayed in Fig. 2. The signals were corrected for the recorded influencing outside driving forces, i.e. temperature, relative humidity and pressure, through MLR method8,9.
The 222Rn signals were investigated with the Empirical Mode Decomposition (EMD, see Methods), a method not significantly affected by the lack of data in the time series thanks to self-consistent regression estimator53. Most of the components obtained by applying the EMD method (not showed for brevity) are due to meteorological and seasonal phenomena.
We focus here on the trends and the residuals of the two signals. The trend is the last component obtained by the EMD decomposition method25,54 while the residuals (i.e. anomalies) refer to those values of the radon time series that are out of the 95% confidence interval of the differences between the measured signals and the forecasted time series. The forecasting of the two radon time series is obtained by the application of the forecasting Support Vector Regression (SVR) method8,9,49 on the components obtained from MLR + EMD hybrid method, and hence on their sum (see Methods).
The trends (Fig. 3a) reflect an increasing pattern of 222Rn activity concentration during the entire monitoring period at both OLB and MSA sites. Instead, radon residuals concentrate in 4 well defined periods (March-November 2013, May-September 2014, April-November 2015 and August 2016-Decemner 2017; Fig. 3b). It is worth noting how the radon residuals occur almost contemporaneously at OLB and MSA, two sites 3.87 km apart, even if with different intensity possibly due to the different distance from the centre of the current unrest that roughly coincides with the central area of the caldera where the hydrothermal activity is concentrated and where the maximum ground uplift and the highest seismicity are recorded.
The radon signals, monitored during 2011–2017, refer to the current period of Campi Flegrei volcanic unrest (post 2004–2005 period) characterised by soil uplift, increasing seismic activity and marked variation in the hydrothermal activity. The trends and residuals obtained from the radon signals monitored in soils of OLB and MSA sites are thus comp ared with independent data that were recently used to characterise the current phase of Campi Flegrei volcanic unrest (Fig. 4a,b). In particular we considered the following data sets:
the cumulative number of days with earthquakes since 2000, i.e. the background seismicity as defined in ref. 45;
the fumarolic tremor (RSAM) of Pisciarelli fumarole50 registered by the CPIS seismic station (40°49'45.8” N, 14°08'49.9” E).
Fumaroles are in fact known to generate seismic (and infrasonic) tremor, whose temporal changes quantitatively correlates with the variations of the fumarole activity and ground shaking55,56. In particular, the RSAM at Pisciarelli was recognised as a powerful indicator of the current unrest of Campi Flegrei41,50. The RSAM is in fact controlled by the gas fluxes from the fumarolic vent (currently the main vent of Campi Flegrei) as suggested by the high correlations with both direct flux measurements and the CO2 air concentration continuously measured at the site (see Fig. 11 in ref. 41).
The correlation of the radon trends with ground deformation (Fig. 4a) and the background seismicity (Fig. 4b) suggests in general the high potentiality of the radon as an additional indicator of the current crisis of Campi Flegrei. The increased permeability of the media due to the increased number of earthquakes can significantly contribute to outgassing variations57,58 and ultimately to the increase of the radon trends. However, the MSA radon station is ~ 4 km distant from the seismic zone that is currently restricted to the Solfatara and Pisciarelli hydrothermal sites (see Fig. 1 in ref. 45). Also, for this reason, we think that a general increase of the temperature and the pressure of the Campi Flegrei hydrothermal system50,59 is the central parameter explaining the correlation among the different independent variables. The temperature increase may induce thermal devolatilization phenomena on radon60 and the fluid pressure increase favours deformation, earthquakes and the flux of the hydrothermal gas from depth to the surface. For example, it was measured by various authors a strong increase in the hydrothermal-volcanic CO2 both diffusively emitted at Solfatara (from 900–1000 t/d in 2010–2011 to 1500–3000 t/d in 2015–201643) and emitted by Pisciarelli vent (from 150–200 t/d in 2012–2013 to 400–600 t/d in 2017–201944, Fig. 4c).
In this context, it is particularly indicative the correlation between the radon residuals and the RSAM (Fig. 4c), a signal directly controlled by the Pisciarelli emission. The radon residuals mimic the prominent fumarolic tremor enhancement peaks during the entire monitoring time because the four periods of high radon residuals practically coincide with the periods of highest seismic tremor of the hydrothermal area.
This evident correlation proves that, independently from its generation-propagation mechanisms, the RSAM signal is actually linked to dynamic changes in gas flow regime within the Campi Flegrei caldera system. In particular, the 2012 to 2017 increasing CO2 emission of Pisciarelli vent44 testifies a general increase of the fluid pressure of the Campi Flegrei hydrothermal system and consequently in the hydrothermal CO2 fluxes affecting the caldera, a process that in some way can control the 222Rn increasing trends and residuals.
The carrier gases, like CO2, play, in fact, a critical role in controlling the migration and transport of trace gases such as 222Rn towards the surface1,17,51,61,62,63,64. Due to the diffusion coefficient in dry soil (5 ∙ 10−6 m2/s)65 and half-life (3.82 days), the large ranges of soil 222Rn activities can be explained by a double origin1: (i) the radon is generated by the decay of 238U accumulated in the soil (usually low activity concentration of several Bq/m3); (ii) the radon produced by the decay of 238U from deeper levels migrates upward, transferred by carrier gases through faults and fractures (high activity concentration up to several ten thousand Bq/m3). The OLB and MSA data (222Rn activity concentrations of 104–105 Bq/m3) point to this second type of origin and their trends and residuals, well correlated with independent geophysical data, are well explained by variation in the flux of the hydrothermal-volcanic CO2 that at Campi Flegrei acts as carrier gas.
The different intensities of radon trend curves and residuals, lower in MSA than in OLB, are likely due to the different distance of the two sites from the main active degassing area, i.e. Pisciarelli fumarole and Solfatara crater, where the CO2 flux is higher. Furthermore, OLB is inside the area of current seismicity, where gas fluxes can be increased also by earthquake induced fracturing. Hence, the lower intensity of radon trend and residuals at MSA with respect to OLB, is most likely due to a lower carrier gas effect.
All the signals that we have discussed are thus likely controlled by the temperature-pressure of the hydrothermal system whose increase strongly characterises the activity of the Campi Flegrei in these early decades of the XXI century (Fig. 5). The T-P of the hydrothermal system, estimated by applying a gas-equilibria approach to the fumaroles of highest temperature45,50,66 (BG and BN, ~160 °C and ~145 °C, respectively; Fig. 1), started to increase since the beginning of 2000’s in a process that is still ongoing (Fig. 5).
Since 2004–2005 Campi Flegrei caldera is in a new unrest period characterised by ground uplift, seismicity, changes on fumarolic fluid composition and a general increase of the emission of volcanic-hydrothermal fluids. The long data series, acquired since 2011, highlight how this crisis in some way affects also the 222Rn activity in the soils. The data suggest two main considerations: (i) the first regards the extension of the area affected by the current unrest that results much larger than the area of seismicity and the area of intense hydrothermal activity of Pisciarelli and Solfatara (e.g. MSA site is in Napoli city, 4 km east from the centre of the crisis); (ii) the second consideration regards the 222Rn and its potential as an indicator of the evolution of a volcanically-induced crisis: the radon signals show, in fact, a pattern very similar to that of the more classic geophysical and geochemical parameters routinely monitored for the surveillance of volcanic systems. These results represent an absolute novelty in the study of a such calderic area and mark a significant step forward in the use and interpretation of the radon signal, and also indicate that long-term observation of the radon signal at multiple sites in a seismic-volcanic area could help improve the characterization of the region.
222Rn activity concentration (Bq/m3) in soil gas of Campi Flegrei caldera is continuously monitored, at Monte Olibano and Monte Sant’Angelo sites (Fig. 1), by RaMonA system67,68. It is based on electrostatic collection of the ionized descendants of the gas on a Silicon detector inside a cylindrical metallic chamber and provides the complete alpha spectrum of 220Rn and 222Rn that is analysed by FORTAS software67. Here, only 222Rn is considered, although 220Rn could be used to discriminate the source coming from deeper levels8. The continuous monitoring is performed by 1 l/min pumping the soil gas from a depth of 0.80 m to the inlet of the detector19. The time interval of detected and processed data is 1 h, but the daily average of the data is used in the analysis. The device also monitors temperature, relative humidity and pressure inside the detection chamber and in the surface soil of the measurement site. The values of the climatic parameters measured internally are used to correct the rough result on the basis of the variability of the detection efficiency7; while externally measured values are used to search for correlations with radon through the MLR method9,19.
The seismic tremor is monitored from a station located 8 m away from the Pisciarelli fumarole (Fig. 1), which measures changes in ground vibration, in m/s, in real time (real-time seismic amplitude measurement - RSAM). Analytical methodologies and uncertainties are described in refs. 50,69. A characteristic RSAM value is computed daily by assuming as representative the minimum value registered during the night, which corresponds to the time of the day when anthropogenic noise is lowest (lower than during daylight hours).
The chemical composition (μmol/mol) of Solfatara fumaroles (Bocca Grande, Bocca Nuova) is monitored by systematic sampling (Fig. 1). The analytical methods and their uncertainties are available in the refs. 64,70. The time series of the CO/CO2 ratio is calculated since it is an excellent indicator of the temperature variations at depth42.
The background seismicity is referred to the cumulative distribution of Campi Flegrei seismicity, which simply corresponds to the sum of the days in which at least one earthquake has occurred43. The current permanent seismic network of Campi Flegrei (Fig. 1) is composed of a total of 23 stations that transmit data in real time to the Osservatorio Vesuviano (Istituto Nazionale di Geofisica e Vulcanologia) monitoring center. The reference station for Campi Flegrei seismicity is located close to the Pisciarelli hydrothermal area where the post-2000 seismicity is concentrated. A full description of Campi Flegrei network is reported in ref. 45.
The ground deformation (cm) is monitored through the NeVoCGPS (Neapolitan Volcanoes Continuous GPS) network (Fig. 1), which provides measurements of the 3D time changes in 20 stations operating at Campi Flegrei45. A full description of NeVoCGPS network is reported in refs. 71,72. The reference GPS station for the Campi Flegrei area is close to the zone of maximum vertical displacement, near the Solfatara crater, because it is representative of the time pattern of ground deformations.
Time series analysis
Hybrid methods are an effective methodology that can aggregate multiple separate methods, combining the advantages of each one with optimized algorithms and achieving greater accuracy since the absolute uncertainty is lower than that obtained by every single method48,49,54,73.
The hybrid method Multiple Linear Regression + Empirical Mode Decomposition + Support Vector Regression (MLR + EMD + SVR) used for radon time series analysis, to obtain the trends and anomalies detection, is here developed and tuned in MATLAB environment. This appropriate combination coming from previous works8,9,25,73,74,75 that studied the analytical performance and advantages of each component method, tested on several time series, in order to obtain the best performance with lower uncertainty. The signal trend extraction is performed by using the MLR + EMD method. The MLR technique estimates the contribution of the recorded environmental parameters (i.e. temperature, relative humidity and pressure, which influence the signal) to the time series, via a multiple linear regression model based on the least-squares fit. The final correct time series are obtained as the difference between the unprocessed time series and that obtained from the model. The procedure is fully described in refs. 19,46. On the correct time series the EMD technique is applied to further differentiate the seasonal-periodic modulations within the signal, by decomposition. The signal is decomposed into a collection of components, progressively in frequency (unless constancy or monotony), obtained by iterative differences between the signal and the mean envelope of the upper and lower envelopes from the spline interpolation among all the local maxima and the local minima, respectively. The last component is the representative trend of the time-series. The detailed analytical description is reported in refs. 76,77. The EMD method is improved to deal with time series with missing data78: self-consistent regression estimator recursively imputes missing values and decomposes the signal efficiently under EMD framework47. The anomalies identification, which underlines the specific values not attributable to the normal evolution of the studied time series, is performed by observing the raw signal outside the two 95% confidence bounds of the forecasted signal obtained using the SVR technique combined to the output of MLR + EMD hybrid method. The SVR method makes a regression model based on a set of non-linear training data, in order to predict them with a function (i) having lowest deviation from the original data set and (ii) being as flat as possible. This regression problem is commonly used in its Lagrange dual formulation: it allows to extend from non-linear functions into a high-dimension dual space where linear techniques are available, using a Gaussian kernel mapping function. The SVR method is here applied first on each output component from MLR + EMD hybrid method, and finally on the sum of all predicted components; this is the expected forecasting result of the raw time series. A complete analytical description of the forecasting process used by the SVR method is available in refs. 73,79, with numerous explanatory examples. A datum in the raw time series is considered an anomaly if it is beyond one of the two forecasted time series at 95% CI that contain the same raw signal: then, the residuals (i.e. anomalies values) are obtained by subtracting the two forecasted signals at 95% CI from the raw time series, in absolute terms.
The two forecasted time series at 95% CI are calculated as the forecasted signal results from SVR method ± the confidence coefficient 1.96 multiplied by the mean squared errors of the forecasting. To better understand the anomalies detection, two examples are shown in Fig. 6 where two parts of the 222Rn activity concentration time series of Monte Olibano are analysed: one with (20 July-24 August 2013) and another without anomalies (10 May-10 June 2016). The anomalies identification process is reported in refs. 74,80.
All the recorded data (Radon, temperature, humidity and atmospheric pressure) their graphs are reported in the Supplementary Material.
Chen, Z. et al. Radon emission from soil gases in the active fault zones in the Capital of China and its environmental effects. Sci. Rep. 8, 16772 (2018).
Kamişlioğlu, M. & Külahci, F. Chaotic behavior of soil Radon gas and applications. Acta Geophys. 64(5), 1563–1592 (2016).
Sciarra, A. et al. Radon and carbon gas anomalies along the Watukosek Fault System and Lusi mud eruption, Indonesia. Mar. Petrol. Geol. 90, 77–90 (2018).
Choubey, V. M., Kumar, N. & Arora, B. R. Precursory signatures in the radon and geohydrological borehole data for M4.9 Kharsali earthquake of Garhwal Himalaya. Sci. Total Environ. 407(22), 5877–5883 (2009).
Iskandar, D., Yamazawa, H. & Iida, T. Quantification of the dependency of radon emanation power on soil temperature. Appl. Radiat. Isot. 60, 971–973 (2004).
Laiolo, M. et al. The effects of environmental parameters on diffuse degassing at Stromboli volcano: Insights from joint monitoring of soil CO2 flux and radon activity. J. Volcanol. Geotherm. Res. 315, 65–78 (2016).
Roca, V. et al. The influence of environmental parameters in electrostatic cell radon monitor response. Appl. Radiat. Isot. 61, 243–247 (2004).
Ambrosino, F., De Cesare, W., Roca, V. & Sabbarese, C. Mathematical and geophysical methods for searching anomalies of the Radon signal related to earthquakes. J. Phys.: Conf. Ser. 1226, 012025 (2019).
Ambrosino, F., Pugliese, M., Roca, V. & Sabbarese, C. Innovative methodologies for the analysis of radon time series. Nuovo Cimento C. 41(6), 223 (2018).
Barbosa, S. M., Zafrir, H., Malik, U. & Piatibratova, O. Multiyear to daily radon variability from continuous monitoring at the Amram tunnel. Southern Israel. Geophys. J. Int. 182, 829–842 (2010).
Garavaglia, M., Dal Moro, G. & Zadro, M. Radon and tilt measurements in a seismic area: temperature effects. Phys. Chem. Earth Part A 25(3), 233–237 (2000).
Ilić, R. et al. Radon in Antarctica. Radiat. Meas. 40, 415–422 (2005).
Arora, B. R. et al. Assesment of the response of the meteorological/hydrological parameters on the soil gas radon emission at Hsinchu, northern Taiwan: A prerequisite to identify earthquake precursors. J. Asian Earth Sci. 149, 49–63 (2017).
Richon, P. et al. Spatial and time variations of radon-222 concentration in the atmosphere of a dead-end horizontal tunnel. J. Environ. Radioact. 78(2), 179–198 (2005).
Gal, F. & Gadalia, A. Soil gas measurements around the most recent volcanic system of metropolitan France (Lake Pavin, Massif Central). C. R. Geosci. 343(1), 43–54 (2011).
Ambrosino, F., et al Analysis of geophysical and meteorological parameters influencing 222Rn activity concentration in Mladeč caves (Czech Republic) and in soils of Phlegrean Fields caldera (Italy). Appl. Radiat. Isot. 109140; https://doi.org/10.1016/j.apradiso.2020.109140 (2020).
Briestenský, M. et al. Radon, Carbon dioxide and fault displacements in central Europe related to the Tōhoku earthquake. Radiat. Prot. Dosim. 160(1–3), 68–82 (2014).
Deb, A., Gazi, M., Ghosh, J., Chowdhury, S. & Barman, C. Monitoring of soil radon by SSNTD in Eastern India in search of possible earthquake precursor. J. Environ. Radioact. 184-185, 63–70 (2018).
De Cicco, F. et al. Multi-parametric approach to the analysis of soil radon gas for its validation as geoindicator in two sites of the Phlegrean Fields caldera (Italy). Environ. Earth Sci. 76, 317–327 (2017).
Ghosh, D., Deb, A. & Sengupta, R. Anomalous radon emission as precursor of earthquake. J. Appl. Geophys. 69(2), 67–81 (2009).
Hauksson, E. & Goddard, J. G. Radon earthquake precursor studies in Iceland. J. Geophys. Res. 86(8), 7037–7054 (1981).
Jilani, Z., Mehmood, T., Alam, A., Awais, M. & Iqbal, T. Monitoring and descriptive analysis of radon in relation to seismic activity of Northern Pakistan. J. Environ. Radioact. 172, 43–51 (2017).
Neri, M. et al. Soil radon measurements as a potential tracer of tectonic and volcanic activity. Sci. Rep. 6, 24581 (2016).
Nevinsky, I. et al. Results of the simultaneous measurements of radon around the Black Sea for seismological applications. J. Environ. Radioact. 192, 48–66 (2018).
Sabbarese, C. et al. Signal decomposition and analysis for the identification of periodic and anomalous phenomena in Radon time-series. Radiat. Prot. Dosim. 177(1-2), 202–206 (2017).
Alonso, H. et al. Assessment of radon risk areas in the Eastern Canary Islands using soil radon gas concentration and gas permeability of soils. Sci. Total Environ. 664, 449–460 (2019).
Cigolini, C., Laiolo, M., Coppola, D. & Ulivieri, G. Preliminary radon measurements at Villarrica volcano. Chile. J. S. Am. Earth Sci. 46, 1–8 (2013).
Giustini, F., Ciotoli, G., Rinaldini, A., Ruggiero, L. & Voltaggio, M. Mapping the geogenic radon potential and radon risk by using Empirical Bayesian Kriging regression: A case study from a volcanic area of central Italy. Sci. Total Environ. 661, 449–464 (2019).
Baixeras, C. et al. Radon levels in the volcanic region of La Garrotxa, Spain. Radiat. Meas. 40(2–6), 509–512 (2005).
Immè, G., La Delfa, S., Lo Nigro, S., Morelli, D. & Patanè, G. Soil radon concentration and volcanic activity of Mt. Etna before and after the 2002 eruption. Radiat. Meas. 41(2), 241–245 (2006).
Lucchetti, C. et al. Integrating radon and thoron flux data with gamma radiation mapping in radon-prone areas. The case of volcanic outcrops in a highly-urbanized city (Roma, Italy). J. Environ. Radioact. 202, 41–50 (2019).
Laiolo, M., Cigolini, C., Coppola, D. & Gervino, G. Insights on radon survey at the Stromboli volcano. The European Physical Journal Conferences 24, 2100–014X (2012).
Laiolo, M., Cigolini, C., Coppola, D. & Gervino, G. Developments in real-time radon monitoring at Stromboli volcano. Journal of Environmental Radioactivity 105, 21–29 (2012).
Civetta, L. et al. Geo-chemical zoning mingling eruptive dynamics and depositional processes-the Campanian Ignimbrite, Campi Flegrei caldera, Italy. J. Volcanol. Geotherm. Res. 75, 183–219 (1997).
Di Vito, M. A. et al. Volcanism and deformation since12,000 years at the Campi Flegrei caldera (Italy). J. Volcanol. Geotherm. Res. 91, 221–246 (1999).
Orsi, G., De Vita, S. & Di Vito, M. The restless, resurgent Campi Flegrei nested caldera (Italy): constraints on its evolution and configuration. J. Volcanol. Geotherm. Res. 74, 179–214 (1996).
Del Gaudio, C., Aquino, I., Ricciardi, G. P., Ricco, C. & Scandone, R. Unrest episodes at Campi Flegrei: a reconstruction of vertical ground movements during 1905–2009. J. Volcanol. Geotherm. Res. 195(1), 48–56 (2010).
D’Auria, L. et al. Magma injection beneath the urban area of Naples: a new mechanism for the 2012–2013 volcanic unrest at Campi Flegrei caldera. Sci. Rep. 5, 13100 (2015).
Trasatti, E., Polcari, M., Bonafede, M. & Stramondo, S. Geodetic contraints to the source mechanism of the 2011–2013 unrest at Campi Flegrei (Italy) caldera. Geoph. Res. Lett. 42, 3847–3854 (2015).
Chiodini, G. et al. Long‐term variations of the Campi Flegrei, Italy, volcanic system as revealed by the monitoring of hydrothermal activity. J. Geophys. Res. 115, B03205 (2010).
Giudicepietro F. et. al. Insight Into Campi Flegrei Caldera Unrest Through Seismic Tremor Measurements at Pisciarelli Fumarolic Field. Geochemistry, Geophysics, Geosystems, https://doi.org/10.1029/2019GC008610 (2019).
Chiodini, G. et al. CO2 degassing and energy release at Solfatara volcano, Campi Flegrei, Italy. J. Geophys. Res. Solid Earth 106(B8), 16213–16221 (2001).
Cardellini, C. et al. Monitoring diffuse volcanic degassing during volcanic unrests: the case of Campi Flegrei (Italy). Sci. Rep. 7, 6757 (2017).
Tamburrello, G. et al. Escalating CO2 degassing at the Pisciarelli fumarolic system, and implications for the ongoing Campi Flegrei unrest. J. Volcanol. Geotherm. Res. 384, 151–157 (2019).
Chiodini, G. et al. Clues on the origin of post-2000 earthquakes at Campi Flegrei caldera (Italy). Sci. Rep. 7, 4472 (2017).
Singh, S., Jaishi, H. P., Tiwari, R. P. & Tiwari, R. C. Time series analysis of soil radondata using multiple linear regression and artificial neural network in seismic precursory studies. Pure Appl. Geophys. 174(7), 2793–2802 (2017).
Steinberg, L. On experiments using an auto-regressive moving-average model for predicting the monthly 50–100 kPa thickness anomalies. Pure Appl. Geophys. 123(5), 757–775 (1985).
Du, P., Wang, J., Yang, W. & Niu, T. Multi-step ahead forecasting in electrical power system using a hybrid forecasting system. Renew. Energ. 122, 533–550 (2018).
Wang, J., Yang, W., Du, P. & Li, Y. Research and application of a hybrid forecasting framework based on multi-objective optimization for electrical power system. Energy J. 148, 59–78 (2018).
Chiodini, G. et al. Fumarolic tremor and geochemical signals during a volcanic unrest. Geology 45(12), 1131–1134 (2017).
Sciarra, A., Mazzini, A., Inguaggiato, S., Vita, F. & Hadi, S. Radon and carbon gas anomalies along the Watukosek Fault System and Lusi mud eruption, Indonesia. Mar. Pet. Geol. 90, 77–90 (2018).
Virk, H. S., Walia, V. & Kumar, N. Helium/radon precursory anomalies of Chamoli earthquake, Garhwal Himalaya, India. J. Geodyn. 31(2), 201–210 (2001).
Cadenas, E. & Rivera, W. Wind speed forecasting in three different regions of Mexico, using a hybrid ARIMA-ANN model. Renew. Energy 35(12), 2732–2738 (2010).
Yu, C., Li, Y. & Zhang, M. Comparative study on three new hybrid models using Elman Neural Network and Empirical Mode Decomposition based technologies improved by Singular Spectrum Analysis for hour-ahead wind speed forecasting. Energy Convers. Manag. 147, 75–85 (2017).
Matoza, R. S., Fee, D., Neilsen, T. B., Gee, K. L. & Ogden, D. E. Aeroacoustics of volcanic jets: acoustic power estimation and jet velocity dependence. J. Geophys. Res. 118, 6269–6284 (2013).
McKee, K., Fee, D., Yokoo, A., Matoza, R. S. & Kim, K. Analysis of gas jetting and fumarole acoustics at Aso Volcano, Japan. J. Volcanol. Geotherm. Res. 340, 16–29 (2017).
Cigolini, C. et al. High-Resolution Radon Monitoring and Hydrodynamics at Mount Vesuvius. Geophy. Res. Letters 20, 4035–4038 (2001).
Cigolini, C. et al. The dynamics of a double-cell hydrothermal system in triggering seismicity at Somma-Vesuvius: Results from a high-resolution radon survey (revisited). Bull. Volc. 72, 693–704 (2010).
Chiodini, G. & Marini, L. Hydrothermal gas equilibria: The H2O-H2-CO2-CO-CH4 system. Geochim. Cosmochim. Acta 62, 2673–2687l (1998).
Mollo, S., Tuccimei, P., Galli, G., Iezzi, G. & Scarlato, P. The imprint of thermally induced devolatilization phenomena on radon signal: implications for the geochemical survey in volcanic areas. Geophys. J. Int. 211, 558–571 (2017).
Etiope, G. & Martinelli, G. Migration of carrier and trace gases in the geosphere: An overview. Phys. Earth Planet. Int. 129, 185–204 (2002).
Elío, J. et al. CO2 and Rn degassing from the natural analog of Campo de Calatrava (Spain): Implications for monitoring of CO2 storage sites. Int. J. Greenh. Gas Con. 32, 1–14 (2015).
Rodrigo-Naharro, J., Quindós, L. S., Clemente-Jul, C., Mohamud, A. H. & Del Villar, L. P. CO2 degassing from a Spanish natural analogue for CO2 storage and leakage: Implications on 222Rn mobility. Appl. Geochem. 84, 297–305 (2017).
Oh, Y. H. & Kim, G. A radon-thoron isotope pair as a reliable earthquake precursor. Sci. Rep. 5, 13084 (2015).
Fleischer, R. L. Risk of radon. Nature 293(5829), 180 (1981).
Chiodini, G. et al. Magmas near the critical degassing pressure drive volcanic unrest towards a critical state. Nat. Commun. l, 13712l (2016).
Sabbarese, C., Ambrosino, F., Buompane, R., Pugliese, M. & Roca, V. Analysis of alpha particles spectra of the Radon and Thoron progenies generated by an electrostatic collection detector using new software. Appl. Radiat. Isot. 122, 180–185 (2017).
Ambrosino, F., Buompane, R., Pugliese, M., Roca, V. & Sabbarese, C. RaMonA system for radon and thoron measurement. Nuovo Cimento C. 41(6), 222 (2018).
Endo, E. T. & Murray, T. Real-time seismic amplitude measurement (RSAM): A volcano monitoring and prediction tool. Bull. Volcanol. 53, 533–545 (1991).
Caliro, S. et al. The origin of the fumaroles of La Solfatara (Campi Flegrei, South Italy). Geochim. Cosmochim. Acta 71(12), 3040–3055 (2007).
De Martino, P., Tammaro, U. & Obrizo, F. GPS time series at Campi Flegrei caldera (2000–2013). Ann. Geophys. 57(2), S0213 (2014).
Tammaro, U. et al. Somma Vesuvius volcano: ground deformations from CGPS observations (2001–2012). Ann. Geophys. 56(4), S0456 (2013).
Duan, W. Y., Han, Y., Huang, L. M., Zhao, B. B. & Wang, M. H. A hybrid EMD-SVR model for the short-term prediction of significant wave height. Ocean Eng. 124, 54–73 (2016).
Ambrosino, F., Thinová, L., Briestenský, M. & Sabbarese, C. Anomalies identification of Earth’s rotation rate time series (2012-2017) for possible correlation with strong earthquakes occurrence. Geod. Geodyn. 10(6), 455–459 (2019).
Ambrosino, F., Thinová, L., Briestenský, M. & Sabbarese, C. Analysis of Radon time series recorded in Slovak and Czech caves for the detection of anomalies due to seismic phenomena. Radiat. Prot. Dosim. ncz245; https://doi.org/10.1093/rpd/ncz245 (2019).
Hong, L. Decomposition and forecast for financial time series with high-frequency based on Empirical Mode Decomposition. Energy Procedia 5, 1333–1340 (2011).
F. Crockett, R. G. M., Perrier, F. & Richon, P. Spectral-decomposition techniques for the identification of periodic and anomalous phenomena in radon time-series. Nat. Hazards Earth Syst. Sci. 10, 559–564 (2010).
Kim, D. & Oh, H. S. Empirical mode decomposition with missing values. Springerplus. 5(1), 2016 (2016).
Sousa, J. C., Jorge, H. M. & Neves, L. P. Short-term load forecasting based on support vector regression and load profiling. Int. J. Energ. Res. 38(3), 350–362 (2014).
Stránský, V. & Thinová, L. Radon concentration time series modeling and application discussion. Radiat. Prot. Dosim. 177(1-2), 155–159 (2017).
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Sabbarese, C., Ambrosino, F., Chiodini, G. et al. Continuous radon monitoring during seven years of volcanic unrest at Campi Flegrei caldera (Italy). Sci Rep 10, 9551 (2020). https://doi.org/10.1038/s41598-020-66590-w
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