Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/9822
AuthorsPedone, M.* 
Aiuppa, A.* 
Giudice, G.* 
Grassa, F.* 
Francofonte, V.* 
Bergsson, B.* 
Ilyinskaya, E.* 
TitleTunable diode laser measurements of hydrothermal/volcanic CO2 and implications for the global CO2 budget
Issue Date2-Dec-2014
Series/Report no./5(2014)
DOI10.5194/se-5-1209-2014
URIhttp://hdl.handle.net/2122/9822
Keywordsvolcanic CO2 fluxes
Hekla volcano
Krýsuvík hydrothermal area
Nea Kameni
Vulcano island
tunable diode lasers
Subject Classification04. Solid Earth::04.08. Volcanology::04.08.01. Gases 
04. Solid Earth::04.08. Volcanology::04.08.06. Volcano monitoring 
04. Solid Earth::04.08. Volcanology::04.08.07. Instruments and techniques 
AbstractQuantifying the CO2 flux sustained by lowtemperature fumarolic fields in hydrothermal/volcanic environments has remained a challenge, to date. Here, we explored the potential of a commercial infrared tunable laser unit for quantifying such fumarolic volcanic/hydrothermal CO2 fluxes. Our field tests were conducted between April 2013 and March 2014 at Nea Kameni (Santorini, Greece), Hekla and Krýsuvík (Iceland) and Vulcano (Aeolian Islands, Italy). At these sites, the tunable laser was used to measure the path-integrated CO2 mixing ratios along cross sections of the fumaroles’ atmospheric plumes. By using a tomographic post-processing routine, we then obtained, for each manifestation, the contour maps of CO2 mixing ratios in the plumes and, from their integration, the CO2 fluxes. The calculated CO2 fluxes range from low (5.7 +/- 0.9 t d-1; Krýsuvík) to moderate (524 +/-108 t d-1; La Fossa crater, Vulcano). Overall, we suggest that the cumulative CO2 contribution from weakly degassing volcanoes in the hydrothermal stage of activity may be significant at the global scale.
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