Abstract

Titanite varieties doped with rare earth elements (REE) have been prepared by ceramic synthesis and quenching in air. Their crystal structure was determined by Rietveld analysis of the powder X-ray diffraction patterns. Two different substitution schemes, Ca1− x Na x /2Sm x /2TiSiO5 and Ca1− x Dy x Ti1− x $Fe_{x^{3+}}$ SiO5, are studied at x = 0.2. Both synthetic varieties of titanite adopt space group A2/a. This implies that both single-site and complex multivalent substitutional schemes destroy the coherence of the off-centering of octahedral chains in the titanite structure resulting in a P21/a→A2/a phase transition. Unit cell dimensions obtained for the REE-bearing titanite varieties are as follows: a = 7.0541(1)A; b = 8.7247(1)A; c = 6.5664(1)A; β = 113.732(1)° for Ca0.8Na0.1Sm0.1TiSiO5; and a = 7.0021(1)A; b = 8.7256(1)A; c = 6.5427(1)A; β = 113.294(1)° for ${\rm Ca}_{0.8}{\rm Dy}_{0.2}{\rm Ti}_{0.8}{\rm Fe}_{0.2}^{3+} {\rm SiO}_5$ . Both REE-doped titanite samples and a control sample of the pure titanite end member have similar unit cell parameters and consist of polyhedra distorted to a similar extent with the exception of more-distorted SiO4 tetrahedron in CaSiTiO5. The structural data suggest that the Ca1− x Na x /2Sm x /2TiSiO5 and Ca1− x Dy x Ti1− x Fe x SiO5 solid solutions adopting the titanite structure might extend to x sufficiently greater than 0.2 and involve both heavier and lighter trivalent rare earth elements.

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