Many volcanoes show a change in chemical composition of the gas phase prior to
periods of eruptive activity. Fine‐grained tephra erupted from active vents and transported
through volcanic plumes can adsorb, and therefore rapidly scavenge, volatile elements
such as sulfur, halogens, and metal species in the form of soluble salts adhering to ash
surfaces. Analysis of such water‐soluble surface materials is a suitable supplement for
remote monitoring of volcanic gases at inaccessible volcanoes. In this work, ash samples
of the 2004 to 2009 eruptive activity of Stromboli volcano were sampled, leached, and
analyzed for major and trace elements. Data analysis and interpretation was focused
on determining the relationship between chemical composition of water‐soluble
components adhering to volcanic ash and the volcano’s activity state. First results show
significant temporal variations in ash leachate compositions, reflecting changes in the
eruptive style of the volcano. In particular, we reveal that ash leachates S/F and Mg/Na
ratios showed marked increases prior to a large‐scale explosion on 15 March 2007.PublishedD172041.2. TTC - Sorveglianza geochimica delle aree vulcaniche attiveJCR Journalreserve