Abstract
We performed measurements using an SO2 imaging camera of the SO2 gas mass emitted during five discrete explosive events on Stromboli volcano on 3 October 2006. The SO2 gas mass released during discrete explosions was 15-40 kg per explosion, producing 3-8% of the total daily SO2 gas emission, demonstrating that in terms of gas flux Strombolian explosions are a second-order phenomenon compared with quiescent degassing. Using the typical gas composition measured with OP-FTIR allows us to determine the total gas mass released during an explosion as 360-960 kg with a volume of 1500-4100 m(3) at 1 bar. At the probable source pressure of gas slug formation of 75 MPa this gas amount would occupy a volume equivalent to a sphere with a radius of 0.8-1 m, comparable with estimates of Stromboli's conduit geometry. (C) 2009 Elsevier B.V. All rights reserved.
Original language | English |
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Pages (from-to) | 395-400 |
Number of pages | 6 |
Journal | Journal of Volcanology and Geothermal Research |
Volume | 188 |
Issue number | 4 |
DOIs | |
Publication status | Published - 2009 |
Keywords
- magmatic degassing
- remote sensing
- gas imaging
- stromboli
- strombolian explosions
- volcanic gas
- 2007 eruption
- magmatic gas
- insights
- driven