Synthesis methods and unit-cell volume of end-member titanite (CaTiOSiO ₄ )

State University of New York at Stony Brook, Department of Earth and Space Sciences, Stony Brook, NY, United States

Unit-cell parameters of synthetic, end-member titanite (CaTiOSiO ₄ ) critically depend on the synthesis conditions, as is shown for studies reported in the literature and for new samples reported here. Our study suggests that phase-pure samples are likely to be obtained only if they are synthesized entirely below the solidus. In contrast, samples synthesized either directly from melt or by annealing of glass tend to have higher unit-cell volumes, contain Si-rich and Ca-Si-rich phase impurities, and may be nonstoichiometric. The observed variations in cell parameters among the samples strongly correlate with synthesis methods and can be explained by vacancies in the Ca or Si site or both. This result is particularly important because the thermodynamic properties currently in use for titanite are based on samples synthesized from melts of stoichiometric composition and thus are suspect even though they have been determined carefully. To establish a reference point for future studies concerned with the chemical and physical properties of this material we report our findings along with a redetermination of the unit-cell parameters [a = 7.062(1), b = 8.716(2), and c = 6.559(1) Aa; beta = 113.802(9) degrees , V = 369.4(3) Aa ³ ] from powder X-ray data of synthetic, stoichiometric titanite.

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This article has been cited by other articles:

				M. Kunz, T. Arlt, and J. Stolz In situ powder diffraction study of titanite (CaTiOSiO4) at high pressure and high temperature American Mineralogist, October 1, 2000; 85(10): 1465 - 1473. [Abstract] [Full Text] [PDF]