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European Journal of Mineralogy; September, October 2001; v. 13; no. 5; p. 985-993; DOI: 10.1127/0935-1221/2001/0013-0985
© 2001 E. Schweizerbart'sche Verlagsbuchhandlung Science Publishers
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Articles

The monoclinic I2 structure of bassanite, calcium sulphate hemihydrate (CaSO4 · 0.5H2O)

Paolo BALLIRANO1, Adriana MARAS1, Simone MELONI2 and Ruggero CAMINITI2

1 Dipartimento di Scienze della Terra, Università di Roma "La Sapienza", P.le A. Moro 5, I-00185 Roma, Italy
2 Dipartimento di Chimica, Istituto Nazionale per la Fisica della Materia, Università di Roma "La Sapienza", P.le A. Moro 5, I-00185 Roma, Italy

e-mail: paolo.ballirano{at}uniromal.it

A structural analysis of CaSO4 · 0.5H2O, a dehydration product of gypsum, has been carried out through the Rietveld method on X-ray powder diffraction data. A dehydrated powder of synthetic gypsum has been charged inside a non-hermetically sealed capillary in order to allow a slow rehydration. The starting material has been identified as {gamma}-anhydrite, space group P6222, cell parameters a = 6.9691(2) Å, c = 6.3033(2) Å. The final product of the rehydration of {gamma}-anhydrite is CaSO4 · 0.5H2O, space group I2 (unique axis b), cell parameters a = 12.0350(5) Å, b = 6.9294(3) Å, c = 12.6705(4) Å, β = 90.266(3)°. The structure of the hemihydrate is strongly pseudo-trigonal, space group P3121. The symmetry lowering arises from water molecules ordering inside the channels.

Key-words: {gamma}-anhydrite, CaSO4 · 0.5H2O, bassanite, gypsum, X-ray powder diffraction, Rietveld method.




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