0000000001137608

AUTHOR

Ben Kennedy

showing 2 related works from this author

Advances in Fourier transform infrared spectroscopy of natural glasses: From sample preparation to data analysis

2014

Fourier transform infrared spectroscopy (FTIR) is an analytical technique utilized to measure the concentrations of H and C species in volcanic glasses. Water and CO2 are the most abundant volatile species in volcanic systems. Water is present in magmas in higher concentrations than CO2 and is also more soluble at lower pressures, and, therefore it is the dominant volatile forming bubbles during volcanic eruptions. Dissolved water affects both phase equilibria and melt physical properties such as density and viscosity, therefore, water is important for understanding magmatic processes. Additionally, quantitative measurements of different volatile species using FTIR can be achieved at high s…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesResolution (electron density)Analytical techniqueMineralogyGeology010502 geochemistry & geophysics01 natural sciencesVolcanic glassVolcano13. Climate actionGeochemistry and PetrologySample preparationFourier transform infrared spectroscopyDiffusion (business)DissolutionGeology0105 earth and related environmental sciencesLithos
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Halogen (Cl, F) release during explosive, effusive, and intrusive phases of the 2011 rhyolitic eruption at Cordón Caulle volcano (Chile)

2019

We investigate sulphur, chlorine and fluorine release during explosive, effusive and intrusive phases of the 2011 Cordon Caulle eruption, with a focus on halogen devolatilization. Petrological analysis shows halogen release to have been promoted by isobaric crystallization in slowly-cooled magma that was emplaced in a lava flow and sub-vent intrusion. Fluorine in particular mobilized only after extensive groundmass crystallization and incipient devitrification. By 2017, the gas emitted from vent-proximal fumaroles had hydrothermal compositions, with HCl/HF ratios decreasing with decreasing temperature. We estimate that the eruption could eventually emit up to 0.84 Mt of SO2, 6.3 Mt of HCl, …

Explosive materialLavaGeochemistryrhyolitevolatile budgetvolatileHydrothermal circulationGeochemistry and PetrologyRhyolitehalogensEarth and Planetary Sciences (miscellaneous)QE1-996.5geographygeography.geographical_feature_categoryChemistrydegassingGeologyhalogenFumarolevolatilesGeophysicsDevitrificationVolcanoCordón CaulleMagmaPuyehue
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