Geochemistry of sulfur in Mount Etna plume
Author(s) -
Martin D.,
Ardouin B.,
Bergametti G.,
Carbonnelle J.,
FaivrePierret R.,
Lambert G.,
Le Cloarec M. F.,
Sennequier G.
Publication year - 1986
Publication title -
journal of geophysical research: solid earth
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/jb091ib12p12249
Subject(s) - volcano , lava , impact crater , plume , geology , dilution , sulfur , basalt , panache , geochemistry , atmospheric sciences , environmental science , mineralogy , earth science , meteorology , astrobiology , chemistry , geography , organic chemistry , thermodynamics , physics
Aircraft measurements of sulfur compounds and trace elements including Po 210 were carried out in the plume of the Mount Etna volcano, at distances 10 to 260 km from the crater. The experiment was performed in September 1983 following the large lava emission of March–August 1983. Trace elements, particularly Po 210 and Si, were measured with the aim of calculating their atmospheric dilution and evaluating their outputs. This study enabled us to determine the SO 2 to SO 4 conversion rates to be between 2.2 × 10 −6 and 4.0 × 10 −5 s −1 in a cloud free anticyclonic situation. The main process of SO 2 removal in a volcanic plume should be a heterogeneous process of adsorption of this gas onto large particles. Emission fluxes of SO 2 were found to vary between 27 and 38 kg s −1 , leading to a mean Po 210 output of 0.4 Ci/d.
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