Measurement of volatile concentrations in volcanic glasses using thermogravimetric analysis: comparison with micro-analytical methods

• Main Authors: Tuffen, Hugh, Owen, Jacqueline, Applegarth, Louisa
• Format: Conference Object
• Language: unknown
• Published: 2012
• Subjects: Torfajökull; Iceland
• Online Access: https://eprints.lancs.ac.uk/id/eprint/54738/

Thermogravimetric analysis-mass spectrometry (TGA-MS) is potentially a powerful tool for measurement of multi-species volatile concentrations in volcanic rock samples and characterisation of degassing patterns that relate to volatile speciation. Simultaneous differential scanning calorimetry (DSC) provides information on thermal transformations such as crystallisation or melting. However no study has addressed whether the TGA technique can be used to quantify water speciation or separate water from other volatile species such as halogens. We have carried out TGA-DSC-MS experiments on a suite of compositionally homogeneous, variably-degassed rhyolitic obsidian samples from Blahnukur, Torfajökull, Iceland[1]. Sample water contents, as measured by infra-red spectroscopy, range from 0.19-0.81 wt %; F and Cl concentrations, measured using electron microprobe, range from 0.26-0.35 and 0.18-0.22 wt % respectively. Other volatile species concentrations (e.g. CO2, S) were beneath detection limits. The TGA results show an excellent correlation between the total volatile content measured using TGA (TVCTGA) and the total volatile content (H2OT + F + Cl) measured by other techniques (TVCTGA = 0.992TVCFTIR,EPMA, with R2 = 0.94). This shows that both water and halogen species are degassed during TGA measurements, even though halogen species are not detected through MS analyses. Patterns of volatile release indicate a link between water speciation, as measured using FTIR, and the temperature of degassing, and allow identification of hydrated samples. There are strong correlations between TGA weight loss over the 250-550 ° C interval and [H2Om] concentration, and between weight loss >550 ° C and the -OH content. The total volatile loss above 550 ° C far exceeds -OH concentrations alone (TGA>550 = 1.9126 [-OH] + 0.1693), but closely matches the sum of -OH, F and Cl in glasses, with TGA>550= 1.02 [-OH+F+Cl]. This indicates that halogen release occurs at high temperatures and accompanies -OH degassing. Simple models of ...