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  5. Emission of gas and atmospheric dispersion of SO2 during the December 2013 eruption at San Miguel volcano (El Salvador, Central America).
 
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Emission of gas and atmospheric dispersion of SO2 during the December 2013 eruption at San Miguel volcano (El Salvador, Central America).

Author(s)
Granieri, D.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Pisa, Pisa, Italia  
Salerno, G.  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia  
Liuzzo, M.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italia  
La Spina, A.  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia  
Caltabiano, T.  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia  
Giudice, G.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italia  
Giuffrida, G.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italia  
Gutierrez, E.  
MARN  
Montalvo, F.  
MARN  
Burton, M.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Pisa, Pisa, Italia  
Papale, P.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Pisa, Pisa, Italia  
Language
English
Obiettivo Specifico
3V. Dinamiche e scenari eruttivi
Status
Published
JCR Journal
JCR Journal
Peer review journal
Yes
Journal
Geophysical Research Letters  
Issue/vol(year)
14/42 (2015)
ISSN
0094-8276
Electronic ISSN
1944-8007
Publisher
American Geophysical Union
Pages (printed)
5847–5854
Date Issued
2015
DOI
10.1002/2015GL064660
URI
https://www.earth-prints.org/handle/2122/10257
Subjects
04. Solid Earth::04.08. Volcanology::04.08.01. Gases  
Subjects

SO2 flux, Clorine and...

Abstract
Abstract San Miguel volcano, El Salvador, erupted on 29 December 2013, after a 46 year period
characterized by weak activity. Prior to the eruption a trend of increasing SO2 emission rate was observed,
with all values measured after mid-November greater than the average value of the previous year (~310 t d 1).
During the eruption, SO2 emissions increased from the level of ~330 t d 1 to 2200 t d 1, dropping after the
eruption to an average level of 680 t d 1. Wind measurements and SO2 emission rates during the preeruptive,
syneruptive, and posteruptive stages were used to model SO2 dispersion around the volcano. Atmospheric
SO2 concentration exceeded the dangerous threshold of 5 ppm in the crater region and in some sectors with
medium elevation of the highly visited volcanic cone. Combining the SO2 emission rate with measured
CO2/SO2, HCl/SO2, and HF/SO2 plume gas ratios, we estimate the CO2, HCl, and HF outputs for the first time
on this volcano.
Type
article
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Granieri et al., 2015.pdf

Size

2.32 MB

Format

Adobe PDF

Checksum (MD5)

00048308fc417833b3ac71a34dee66dc

rome library|catania library|milano library|napoli library|pisa library|palermo library
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