EGU23-5995, updated on 10 Mar 2024
https://doi.org/10.5194/egusphere-egu23-5995
EGU General Assembly 2023
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.

Temporal variations in fumarole gas chemistry at Teide volcano, Tenerife, Canary Islands

Eleazar Padrón1,2, Gladys V. Melián1,2, María Asensio-Ramos1, Pedro A. Hernández1,2, Nemesio M. Pérez1,2, Fátima Rodríguez1, Cecilia Amonte1,2, Alba Martín1,2, Luca D'Auria1,2, and Hirochika Sumino3
Eleazar Padrón et al.
  • 1Instituto Volcanológico de Canarias (INVOLCAN), 38320 San Cristóbal de La Laguna, Tenerife, Canary Islands
  • 2Instituto Tecnológico y de Energías Renovables (ITER), 38600 Granadilla de Abona, Tenerife, Canary Islands
  • 3Department of General Systems Studies, Graduate School of Arts and Sciences, The University of Tokyo, Komaba, Meguro-ku,Tokyo, Japan

Monitoring the volcanic activity of Teide, the only active stratovolcano in Tenerife, the largest island of the Canary Islands, is extremely important for the prevention and reduction of the volcanic disasters of the island. As part of the geochemical monitoring of the Teide volcanic activity, during the last three decades the volcano has been the subject of a geochemical monitoring of the fumarole discharges, characterized by low flux emission of fluids with temperatures of ∼83°C, located at the Teide summit crater (Pérez et al., 1992 and 1996; Melián et al., 2012). Teide fumaroles show chemical compositions typical of hydrothermal fluids, i.e., meteoric steam dominates the gas composition, followed by CO2, N2, H2, H2S, HCl, Ar, CH4, He, and CO (Pérez et al., 1992). The temporal variations in fumarole gas chemistry at Teide volcano was useful to detect significant changes in the chemical composition of the Teide fumarole, including the appearance of SO2, and increases in the HCl and CO concentrations, one year before a seismic crisis that occurred in Tenerife Island between April and June 2004, what suggested that the associated temporal changes in seismic activity and magmatic degassing indicate that geophysical and fluid geochemistry signals in this system are unequivocally related (Melián et al., 2012). The average of the air-corrected 3He/4He ratio during the period 1991-2022 was 6.80 RA (being RA the atmospheric ratio), with the maximum value of the time series (7.57 RA) measured in August 2016, when an input of magmatic fluids triggered by an injection of fresh magma and convective mixing took place beneath Teide volcano (Padrón et al., 2021). After such input of magmatic fluids, increases in the CO2/H2O, C/S and He/CO2 ratios, a decrease in the CO/CO2 ratio were observed together with a significant increase in the seismic activity recorded in the island of Tenerife. This work highlights the important role of volcanic gases in the monitoring of volcanic activity, paying attention to different chemical and isotopic species in the fumarolic discharges.

 

Melián G.V. et al., (2012), Bull. VolcanoL. 74, 1465–1483.

Padrón E. et al., (2021), J. Geophys. Res. 126, e2020JB020318.

Pérez N.M. et al., (1992), Actas de las sesiones científicas. III Congreso Geológico de España, 1, 463–467.

Pérez N.M. et al., (1996), Geophys. Res. Lett. 23(24), 3531–3534.

 

 

How to cite: Padrón, E., Melián, G. V., Asensio-Ramos, M., Hernández, P. A., Pérez, N. M., Rodríguez, F., Amonte, C., Martín, A., D'Auria, L., and Sumino, H.: Temporal variations in fumarole gas chemistry at Teide volcano, Tenerife, Canary Islands, EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-5995, https://doi.org/10.5194/egusphere-egu23-5995, 2023.