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Publications (11/11 displayed)
- 2019 An experimental study of SO 2 reactions with silicate glasses and supercooled melts in the system anorthite–diopside–albite at high temperature citations
- 2018SO2 gas reactions with silicate glassescitations
- 2015Porphyry copper deposit formation by sub-volcanic sulphur dioxide flux and chemisorptioncitations
- 2013Development of a new laboratory technique for high-temperature thermal emission spectroscopy of silicate meltscitations
- 2013A micro-reflectance IR spectroscopy method for analyzing volatile species in basaltic, andesitic, phonolitic, and rhyolitic glassescitations
- 2013Volatile-rich silicate melts from Oldoinyo Lengai volcano (Tanzania)citations
- 2011Methods to analyze metastable and microparticulate hydrated and hydrous iron sulfate mineralscitations
- 2009Effect of SiO2, total FeO, Fe3+/Fe2+ and alkali elements in basaltic glasses on mid-infrared spectracitations
- 2007Resolution of bridging oxygen signals from O 1s spectra of silicate glasses using XPScitations
- 2006A new approach to determine and quantify structural units in silicate glasses using micro-reflectance Fourier-Transform infrared spectroscopycitations
- 2002CO2 solubility and speciation in intermediate (andesitic) meltscitations
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article
SO2 gas reactions with silicate glasses
Abstract
Sulfur dioxide (SO2(g)) is an important gas species in most common volcanic settings on Earth including subduction zones (Shinohara 2013). The relative abundances of SO2(g) may vary at a volcano over time with the highest rates of SO2(g) emissions occurring during eruptive degassing and lesser amounts emitted continuously during quiescent degassing, resulting in a large total amount of SO2(g) integrated over time of the order of 10 Mt/a (McCormick et al. 2013; Shinohara 2013; Henley and Hughes 2016). Much of the emitted SO2(g) is released at high temperatures