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  5. High time resolution fluctuations in volcanic carbon dioxide degassing from Mount Etna
 
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High time resolution fluctuations in volcanic carbon dioxide degassing from Mount Etna

Author(s)
Pering, T. D.  
University of Sheffield, Dept. of Geography, Winter Street, S10 2TN, United Kingdom  
Tamburello, G.  
DiSTeM, Università di Palermo, via Archirafi, 22, 90123 Palermo, Italy  
McGonigle, A. J. S.  
University of Sheffield, Dept. of Geography, Winter Street, S10 2TN, United Kingdom  
Aiuppa, A.  
University of Sheffield, Dept. of Geography, Winter Street, S10 2TN, United Kingdom  
Cannata, A.  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia  
Giudice, G.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italia  
Patanè, D.  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia  
Language
English
Obiettivo Specifico
2V. Dinamiche di unrest e scenari pre-eruttivi
Status
Published
JCR Journal
JCR Journal
Journal
Journal of volcanology and geothermal research  
Issue/vol(year)
/270 (2014)
ISSN
0377-0273
Electronic ISSN
1872-6097
Publisher
Elsevier Science Limited
Pages (printed)
115–121
Date Issued
2014
DOI
10.1016/j.jvolgeores.2013.11.014.
URI
https://www.earth-prints.org/handle/2122/8904
Subjects
04. Solid Earth::04.08. Volcanology::04.08.07. Instruments and techniques  
Subjects

Carbon dioxide

Passive degassing

Volcanic remote sensi...

Plume imaging

Volcano seismology

Abstract
We report here on thefirst record of carbon dioxide gas emission rates from a volcano, captured at≈1 Hz. These
data were acquired with a novel technique, based on the integration of UV camera observations (to measure SO2
emission rates) and field portable gas analyser readings of plume CO2/SO2 ratios. Our measurements were
performedat the North East crater of Mount Etna, southern Italy, and the data reveal strong variability in CO2
emissions over timescales of tens to hundreds of seconds, spanning two orders of magnitude. This carries
importantimplications for attempts to constrain global volcanic CO2 release to the atmosphere, and will lead to
an increased insight into short term CO2 degassing trends. A common oscillation in CO2 and SO2 emission rates
in addition to the CO2/SO2 ratios was observed at periods of ≈89 s. Our results are furthermore suggestive of
an intriguing temporal lag between oscillations in CO2 emissions and seismicity at periods of ≈300–400 s,
with peaks and troughs in the former series leading those in the latter by ≈150 s. This work opens the way to
the acquisition of further datasets with this methodology across a range of basaltic systems to better our
understandingof deep magmatic processes and of degassing links to manifest geophysical signals
Type
article
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