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European Journal of Mineralogy Email Content Delivery
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European Journal of Mineralogy; October/November; v. 21; no. 5; p. 985-993; DOI: 10.1127/0935-1221/2009/0021-1973
© 2009 E. Schweizerbart'sche Verlagsbuchhandlung Science Publishers
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Articles

Thermal behaviour and kinetics of dehydration in air of bassanite, calcium sulphate hemihydrate (CaSO4·0.5H2O), from X-ray powder diffraction

Paolo Ballirano* and Elisa Melis

Dipartimento di Scienze della Terra, Sapienza Università di Roma, P.le Aldo Moro 5, I-00185 Roma, Italy

* Corresponding author, e-mail: paolo.ballirano{at}uniroma1.it

Thermal behaviour and kinetics of dehydration in air of bassanite (calcium sulphate hemihydrate, CaSO4·0.5H2O) have been investigated in situ real-time using laboratory parallel-beam X-ray powder diffraction data. Thermal expansion has been analyzed between 303 and 383 K at increments of 5 K. The bassanite -> {gamma}-anhydrite conversion starts at 388 K and is completed at 408 K. Thermal expansion of hemihydrate is isotropic and not related to the expansion of CaO8–9 polyhedra. Lattice parameters and volume dependence from T is linear within the studied temperature range. Kinetics of dehydration has been investigated from isothermal diffraction data collected at 10 temperatures between 378 and 423 K with steps of 5 K using a fresh sample at each temperature. Transformed fraction {alpha} vs. t curves were fitted with seven different kinetic models. The best fit was found for the Avrami-Erofe’ev equation that provided an empirical activation energy Ea of the process of 73(5) kJ/mol. Ea was found to be substantially independent from the kinetic model selected.

Key-words: bassanite, CaSO4·0.5H2O, thermal behaviour, kinetics of dehydration, X-ray powder diffraction, Rietveld method.







JOURNAL HOME HELP FEEDBACK/COMMNET SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2009 by E. Schweizerbart'sche Verlagsbuchhandlung Science Publishers