HR: 0800h
AN: V41B-0604    [Abstracts]
TI: Fluid/Melt Partition Coefficients Of Halogens In Basaltic Melt
AU: * Alletti, M
EM: marina.alletti@tin.it
AF: CFTA, University of Palermo, Via Archirafi,36, Palermo, 90123, Italy
AU: Baker, D
EM: donb@eps.mcgill.ca
AF: Earth and Planetary Sciences, McGill University, 3450 rue Univeristy, Montreal, QC H3A2A7, Canada
AU: Scaillet, B
EM: bscaille@cnrs-orleans.fr
AF: ISTO-CNRS, 1a rue de la Ferollerie, Orleans, 45071, France
AU: Aiuppa, A
EM: aiuppa@unipa.it
AF: CFTA, University of Palermo, Via Archirafi,36, Palermo, 90123, Italy
AU: Moretti, R
EM: moretti@ov.ingv.it
AF: INGV-Napoli 'Osservatorio Vesuviano', Via Diocleziano 328, Napoli, 80124, Italy
AU: Ottolini, L
EM: ottolini@crystal.unipv.it
AF: CNR-Istituto di Geoscienze e Georisorse-Sezione di Pavia, Via Ferrata 1, Pavia, 27100, Italy
AB: Despite the importance of halogens (F, Cl) in volcanic degassing, solubility and fluid/melt partitioning of these elements have not been comprehensively studied in natural basaltic melts. Experimental determinations of halogen solubility in Mount Etna melts are lacking, despite this volcano being one of the most active and intensively monitored on Earth with an estimated output of thousands tonnes of halogens per day. In order to better understand halogen degassing, we present the results of a series of halogen partitioning experiments performed at different pressures (1-200 MPa), redox conditions (from Δ NNO = + 2 to Δ NNO = – 0.3) and fluid compositions. Experiments used a hawaiitic, glassy, alkaline basalt with Mg# = 0.59, sampled during the July 2001 eruption of Mount Etna. A series of experiments were conducted using H₂O-NaCl or H₂O-NaF solutions. The effect of CO2 in multi-component fluid H₂O-CO₂-NaCl or H₂O-CO₂-NaF was also investigated. The experimental run products were mostly glasses, but a few run products contained less than 10% crystals. The concentration of halogens in the fluid phase after the experiment was calculated from mass balance, and the partition coefficients for both Cl and F at the studied conditions determined. Using these measurements and thermodynamical models, the dependence of these partition coefficients on the fugacities of various gaseous species was investigated.
DE: 8410 Geochemical modeling (1009, 3610)
DE: 8430 Volcanic gases
SC: Volcanology, Geochemistry, Petrology [V]
MN: 2007 Fall Meeting