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Rare-earth perovskites along the CaTiO3-Na0.5La0.5TiO3 join: Phase transitions, formation enthalpies, and implications for loparite minerals

  • Dawei Feng , Radha Shivaramaiah and Alexandra Navrotsky EMAIL logo
From the journal American Mineralogist

Abstract

The mineral loparite is the principal ore of the light rare earth elements (LREE) with solid solution compositions in the quaternary system perovskite-lueshite-tausonite-loparite (CaTiO3-NaNbO3-SrTiO3-Na0.5Ln0.5TiO3) (Ln = La, Ce, Pr, Nd). In this study, perovskite solid solutions Ca1-2xNaxLaxTiO3 (0 ≤ x ≤ 0.50) along the perovskite-loparite join were synthesized using solid-state sintering methods. XRD analysis indicates that as the Na+La content increases, the structure changes from orthorhombic to tetragonal. The enthalpies of formation at 298 K from the constituent oxides (ΔH°f, ox) and from the elements (ΔH°f, el) have been determined using high-temperature oxide melt solution calorimetry in molten 3Na2O.4MoO3 at 973 K. Enthalpy of formation from oxides ΔH°f, ox becomes more exothermic with increasing Na+La content, suggesting a stabilization effect of the substitution Ca2+ → 0.5Na+ + 0.5La3+. The observed trend of increasing thermodynamic stability with decreasing structural distortion is in agreement with that seen in many other ABO3 perovskites. The thermodynamic stability of perovskite solid solutions Ca1-2xNaxLaxTiO3 (0 ≤ x ≤ 0.50) along the CaTiO3-Na0.5La0.5TiO3 join provides insights into the natural occurrence of loparite minerals (La, Na, Sr, Ca)(Ti, Nb, Ta, Fe3+)O3.

Acknowledgments

This work was supported by the National Science Foundation, Division of Earth Sciences with contributions from the NSF-wide SUSchem initiative (Grant EAR-1321410).

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Received: 2016-2-26
Accepted: 2016-5-2
Published Online: 2016-9-1
Published in Print: 2016-9-1

© 2016 by Walter de Gruyter Berlin/Boston

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