Premium
S, Cl and F degassing as an indicator of volcanic dynamics: The 2001 eruption of Mount Etna
Author(s) -
Aiuppa Alessandro,
Federico Cinzia,
Paonita Antonio,
Pecoraino Giovannella,
Valenza Mariano
Publication year - 2002
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2002gl015032
Subject(s) - volcano , geology , plume , magma , earth science , basalt , explosive eruption , volcanology , geochemistry , phreatic eruption , mineralogy , meteorology , physics
The recent eruption of Mount Etna (July 2001) offered the opportunity to analyze magma‐derived volatiles emitted during pre‐ and syn‐eruptive phases, and to verify whether their composition is affected by changes in volcanic dynamics. This paper presents the results of analyses of F, Cl and S in the volcanic plume collected by filter‐packs, and interprets variations in the composition based on contrasting solubility in magmas. A Rayleigh‐type degassing mechanism was used to fit the acquired data and to estimate Henry's solubility constant ratios in Etnean basalt. This model provided insights into the dynamics of the volcano. Abundances of sulfur and halogens in eruptive plumes may help predict the temporal evolution of an ongoing effusive eruption.