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Composition and size characterisation of volcanic ash. Gemma Prata Supervisors: Tamsin Mather and David Pyle. Clarisse et al. 2010. Refractive index influence on retrievals. Francis et al. 2012, JGR. Eyjafjallajökull , 13 th May 2010. 1.5% Hematite dust Balkanski et al. 2007.
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Composition and size characterisation of volcanic ash Gemma Prata Supervisors: Tamsin Mather and David Pyle
Refractive index influence on retrievals Francis et al. 2012, JGR
Eyjafjallajökull, 13th May 2010 1.5% Hematite dust Balkanski et al. 2007 Andesite Pollack et al. 1973 Obsidian Pollack et al. 1973 Volcanic dust (basalt?) Volz 1973 Francis et al. 2012, JGR
Particle size measurement Malvern Mastersizer 2000 Size range: 0.02 – 2000 µm Uses Mie and Fraunhofer scattering Mie: requires sample refractive index Fraunhofer: refractive index not required Need about a teaspoon of sample
Effect of size distribution Volume percentage
Individual component composition Size-resolved composition Bulk composition
X-Ray Fluorescence(XRF) • quick and easy • bulk composition • assumes no size dependence of composition Melt whole sample Quench to glass
Electron Probe Microanalysis(EPMA) • gives composition at specific points • user selects points • beam diameter 10 µm
QEMSCAN Example from Etna 2006 Colour key: Sulphates (purple) Silicates (green, blue, pink) Sulphur/sulphides (yellow, claret) Martin et al. 2008, JGR
Complex index of refraction: n* = n + i · k n – real part k– imaginary part Literature values compiled from Narcisi & Vezzoli, Global and Planetary Change, 1999 P < 0.05