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http://hdl.handle.net/2122/2493
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| Authors: | Aiuppa, A.* Federico, C.* Giudice, G.* Gurrieri, S.* Liuzzo, M.* Shinohara, H.* Favara, R.* Valenza, M.* |
| Title: | Rates of carbon dioxide plume degassing from Mount Etna volcano |
| Title of journal: | J. Geophys. Res. |
| Series/Report no.: | / 111 (2006) |
| Publisher: | Agu |
| Issue Date: | 2006 |
| DOI: | 10.1029/2006JB004307 |
| Keywords: | carbon dioxide Mt. Etna |
| Abstract: | We report here on the real-time measurement of CO2 and SO2 concentrations in the
near-vent volcanic gas plume of Mount Etna, acquired by the use of a field portable gas
analyzer during a series of periodic field surveys on the volcano’s summit. During the
investigated period (September 2004 to September 2005), the plume CO2/SO2 ratio ranged
from 1.9 to 10.8, with contrasting composition for Northeast and Voragine crater plumes.
Scaling the above CO2/SO2 ratios by UV spectroscopy determined SO2 emission
rates, we estimate CO2 emission rates from the volcano in the range 0.9–67.5 kt d 1
(average, 9 kt d 1). About 2 kt of CO2 were emitted daily on average during quiescent
passive degassing, whereas CO2 emission rates from Etna’s summit were 10–40 times
larger during the 2004–2005 effusive event (with a cumulative CO2 release of 3800 kt
during the 6 months of the eruption). Such a syneruptive increase, ascribed to the
replenishment of the shallow (<6 km) volcanic plumbing system by CO2-rich (0.25 wt %)
more primitive magmas, supports the potential of CO2 output rates as key parameters for
volcanic hazard assessment. |
| Appears in Collections: | Papers Published / Papers in press 04.04.12. Fluid Geochemistry
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