The glass transition and the non-Arrhenian viscosity of carbonate melts

Dingwell, Donald B.; Hess, Kai-Uwe; Wilding, Martin C.; Brooker, Richard A.; Di Genova, Danilo; Drewitt, James W. E.; Wilson, Mark und Weidendorfer, Daniel (2022): The glass transition and the non-Arrhenian viscosity of carbonate melts. In: American Mineralogist, Bd. 107, Nr. 6: S. 1053-1064

Abstract

We report the first calorimetric observation of the glass transition for a carbonate melt. A carbonate glass [55K(2)CO(3)-45MgCO(3) (molar)] was quenched from 780 degrees C at 0.1 GPa. The activation energy of structural relaxation close to the glass transition was derived through a series of thermal treatments comprising excursions across the glass transition at different heating rates. Viscosities just above the glass transition temperature were obtained by applying a shift factor to the calorimetric results. These viscosity measurements (in the range of 10(9) Pa center dot s) at supercooled temperatures (ca. 230 degrees C) dramatically extend the temperature range of data for carbonates, which were previously restricted to superliquidus viscosities well below 1 Pa center dot s. Combining our calorimetrically derived results with published alkaline-earth carbonate melt viscosities at high temperatures yields a highly non-Arrhenian viscosity-temperature relationship and confirms that carbonate liquids are fragile. Based on simulations, fragile behavior is also exhibited by Na2CO3 melt. In both cases, the fragility presumably relates to the formation of temperature-dependent low-dimensional structures and Vogel-Fulcher-Tammann (VFT) curves adequately describe the viscosity-temperature relationships of carbonate melts below 1000 degrees C.

• Dokumententyp: Zeitschriftenartikel
• Fakultät: Geowissenschaften > Department für Geo- und Umweltwissenschaften
• Themengebiete: 500 Naturwissenschaften und Mathematik > 550 Geowissenschaften, Geologie
• ISSN: 0003-004X
• Sprache: Englisch