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Authors: Aiuppa, A.*
Shinohara, H.*
Tamburello, G.*
Giudice, G.*
Liuzzo, M.*
Moretti, R.*
Title: Hydrogen in the gas plume of an open‐vent volcano, Mount Etna, Italy
Title of journal: Journal of Geophysical Research
Series/Report no.: /116(2011)
Publisher: AGU
Issue Date: 2011
DOI: 10.1029/2011JB008461
Keywords: Hydrogen
Mount Etna
Open-vent volcano
Abstract: We report here on the first hydrogen determinations in the volcanic gas plume of Mount Etna, in Italy, which we obtained during periodic field surveys on the volcano’s summit area with an upgraded MultiGAS. Using a specific (EZT3HYT) electrochemical sensor, we resolved H2 concentrations in the plume of 1–3 ppm above ambient (background) atmosphere and derived H2‐SO2 and H2‐H2O plume molar ratios of 0.002–0.044 (mean 0.013) and 0.0001–0.0042 (mean 0.0018), respectively. Taking the above H2‐SO2 ratios in combination with a time‐averaged SO2 flux of 1600 Gg yr−1, we evaluate that Etna contributes a time‐averaged H2 flux of ∼0.65 Gg yr−1, suggesting that the volcanogenic contribution to the global atmospheric H2 budget (70,000–100,000 Gg yr−1) is marginal. We also use our observed H2‐H2O ratios to propose that Etna’s passive plume composition is (at least partially) representative of a quenched (temperatures between 750°C and 950°C) equilibrium in the gas‐magma system, at redox conditions close to the nickel‐nickel oxide (NNO) mineral buffer. The positive dependence between H2‐SO2, H2‐H2O, and CO2‐SO2 ratios suggests that H2 is likely supplied (at least in part) by deeply rising CO2‐rich gas bubbles, fluxing through a CO2‐depleted shallow conduit magma.
Appears in Collections:04.02.01. Geochemical exploration
04.08.01. Gases
04.08.06. Volcano monitoring
01.01.07. Volcanic effects
04.04.12. Fluid Geochemistry
Papers Published / Papers in press

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