Environmental and Volcanic Implications of Volatile Output in the Atmosphere of Vulcano Island Detected Using SO2 Plume (2021-23)

被引:3
|
作者
Vita, Fabio [1 ]
Schiavo, Benedetto [2 ]
Inguaggiato, Claudio [3 ]
Inguaggiato, Salvatore [1 ]
Mazot, Agnes [4 ]
机构
[1] Ist Nazl Geofis & Vulcanol, Sez Palermo, Via Ugo La Malfa 153, I-90146 Palermo, Italy
[2] Univ Autonoma Mexico, Inst Geofis, Mexico City 04510, Mexico
[3] Ctr Invest Cient & Educ Super Ensenada Baja Califo, Dept Geol, Ensenada 22860, Mexico
[4] GNS Sci Wairakei Res Ctr, 114 Karetoto Rd,Private Bag 2000, Wairakei 3352, Taupo, New Zealand
关键词
SO2; output; soil CO2 fluxes; air pollutant; Vulcano Island; geochemical crisis; summit degassing; SO2 map dispersion; extensive parameters; INDUSTRIAL SOURCE APPLICATIONS; CARBON-DIOXIDE EMISSIONS; DISPERSION MODEL; AERMOD; STROMBOLI; PERFORMANCE; NETWORK; FLUXES; CO2;
D O I
10.3390/rs15123086
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The volatiles released by the volcanic structures of the world contribute to natural environmental pollution both during the passive and active degassing stages. The Island of Vulcano is characterized by solfataric degassing mainly localized in the summit part (Fossa crater) and in the peripheral part in the Levante Bay. The normal solfataric degassing (high-temperature fumarolic area of the summit and boiling fluids emitted in the Levante Bay area), established after the last explosive eruption of 1888-90, is periodically interrupted by geochemical crises characterized by anomalous degassing that are attributable to increased volcanic inputs, which determine a sharp increase in the degassing rate. In this work, we have used the data acquired from the INGV (Istituto Nazionale di Geofisica e Vulcanologia) geochemical monitoring networks to identify, evaluate, and monitor the geochemical variations of the extensive parameters, such as the SO2 flux from the volcanic plume (solfataric cloud) and the CO2 flux from the soil in the summit area outside the fumaroles areas. The increase in the flux of volatiles started in June-July 2021 and reached its maximum in November of the same year. In particular, the mean monthly flux of SO2 plume of 22 tons day(-1) (t d(-1)) and of CO2 from the soil of 1570 grams per square meter per day (g m(2) d(-1)) increased during this event up to 89 t d(-1) and 11,596 g m(2) d(-1), respectively, in November 2021. The average annual baseline value of SO2 output was estimated at 7700 t d(-1) during normal solfataric activity. Instead, this outgassing increased to 18,000 and 24,000 t d(-1) in 2021 and 2022, respectively, indicating that the system is still in an anomalous phase of outgassing and shows no signs of returning to the pre-crisis baseline values. In fact, in the first quarter of 2023, the SO2 output shows average values comparable to those emitted in 2022. Finally, the dispersion maps of SO2 on the island of Vulcano have been produced and have indicated that the areas close to the fumarolic source are characterized by concentrations of SO2 in the atmosphere higher than those permitted by European legislation (40 & mu;g m(-3) for 24 h of exposition) on human health.
引用
收藏
页数:15
相关论文
共 13 条
  • [1] Health risk analysis of volcanic SO2 hazard on Vulcano Island (Italy)
    Christian D. Klose
    Natural Hazards, 2007, 43 : 303 - 317
  • [2] Health risk analysis of volcanic SO2 hazard on Vulcano Island (Italy)
    Klose, Christian D.
    NATURAL HAZARDS, 2007, 43 (03) : 303 - 317
  • [3] The volcanic activity changes occurred in the 2021–2022 at Vulcano island (Italy), inferred by the abrupt variations of soil CO2 output
    Salvatore Inguaggiato
    Fabio Vita
    Iole Serena Diliberto
    Claudio Inguaggiato
    Agnes Mazot
    Marianna Cangemi
    Marco Corrao
    Scientific Reports, 12
  • [4] The volcanic activity changes occurred in the 2021-2022 at Vulcano island (Italy), inferred by the abrupt variations of soil CO2 output
    Inguaggiato, Salvatore
    Vita, Fabio
    Diliberto, Iole Serena
    Inguaggiato, Claudio
    Mazot, Agnes
    Cangemi, Marianna
    Corrao, Marco
    SCIENTIFIC REPORTS, 2022, 12 (01)
  • [5] Hydrothermal buffering of the SO2/H2S ratio in volcanic gases:: Evidence from La Fossa Crater fumarolic field, Vulcano Island
    Aiuppa, A.
    Federico, C.
    Giudice, G.
    Gurrieri, S.
    Valenza, M.
    GEOPHYSICAL RESEARCH LETTERS, 2006, 33 (21)
  • [6] A NEURAL NETWORK APPROACH FOR SIMULTANEOUS RETRIEVAL OF VOLCANIC SO2 AND PLUME HEIGHT USING HYPERSPECTRAL MEASUREMENTS.
    Piscini, A.
    Carboni, E.
    Del Frate, F.
    Grainger, R. G.
    2014 6TH WORKSHOP ON HYPERSPECTRAL IMAGE AND SIGNAL PROCESSING: EVOLUTION IN REMOTE SENSING (WHISPERS), 2014,
  • [7] Volcanic SO2, BrO and plume height estimations using GOME-2 satellite measurements during the eruption of Eyjafjallajokull in May 2010
    Rix, M.
    Valks, P.
    Hao, N.
    Loyola, D.
    Schlager, H.
    Huntrieser, H.
    Flemming, J.
    Koehler, U.
    Schumann, U.
    Inness, A.
    JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2012, 117
  • [8] Volcanic SO2 plume height retrieval from UV sensors using a full-physics inverse learning machine algorithm
    Efremenko, Dmitry S.
    Loyola, Diego G.
    Hedelt, Pascal
    Spurr, Robert J. D.
    INTERNATIONAL JOURNAL OF REMOTE SENSING, 2017, 38 : 1 - 27
  • [9] Computed tomography reconstruction of SO2 concentration distribution in the volcanic plume of Miyakejima, Japan, by airborne traverse technique using three UV spectrometers
    Kazahaya, Ryunosuke
    Mori, Toshiya
    Kazahaya, Kohei
    Hirabayashi, Jun-ichi
    GEOPHYSICAL RESEARCH LETTERS, 2008, 35 (13)
  • [10] Theoretical Study on Volcanic Plume SO2 and Ash Retrievals Using Ground TIR Camera: Sensitivity Analysis and Retrieval Procedure Developments.
    Corradini, Stefano
    Tirelli, Cecilia
    Gangale, Gabriele
    Pugnaghi, Sergio
    Carboni, Elisa
    IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING, 2010, 48 (03): : 1619 - 1628