6533b7d3fe1ef96bd1261560

RESEARCH PRODUCT

Rates of carbon dioxide plume degassing from Mount Etna volcano,

Cinzia FedericoGaetano GiudiceSergio GurrieriRocco FavaraMarco LiuzzoMariano ValenzaHiroshi ShinoharaAlessandro Aiuppa

subject

Atmospheric ScienceVolcanic hazardsSoil ScienceMineralogyAquatic ScienceOceanographyAtmospheric scienceschemistry.chemical_compoundImpact craterGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)PanacheEarth-Surface ProcessesWater Science and Technologygeographygeography.geographical_feature_categoryEcologyPaleontologyForestryGas analyzerPlumeGeophysicsVolcanochemistrySpace and Planetary ScienceMagmaCarbon dioxideEtnaCO2Geology

description

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. Copyright 2006 by the American Geophysical Union.

10.1029/2006jb004307http://hdl.handle.net/10447/23757