D. Xirouchakis et al., SYNTHESIS METHODS AND UNIT-CELL VOLUME OF END-MEMBER TITANITE (CATIOSIO4), The American mineralogist, 82(7-8), 1997, pp. 748-753
Unit-cell parameters of synthetic, end-member titanite (CaTiOSiO4) cri
tically depend on the synthesis conditions, as is shown for studies re
ported in the literature and for new samples reported here. Our study
suggests that phase-pure samples are likely to be obtained only if the
y are synthesized entirely below the solidus. In contrast, samples syn
thesized either directly from melt or by annealing of glass tend to ha
ve higher unit-cell volumes, contain Si-rich and Ca-Si-rich phase impu
rities, 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 me
lts of stoichiometric composition and thus are suspect even though the
y have been determined carefully. To establish a reference point for f
uture studies concerned with the chemical and physical properties of t
his material we report our findings along with a redetermination of th
e unit-fell parameters [alpha = 7.062(1), b = 8.716(2), and c = 6.559(
1) Angstrom; beta = 113.802(9)degrees, V = 369.4(3) Angstrom(3)] from
powder X-ray data of synthetic, stoichiometric titanite.