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Formation enthalpies of rare earth titanate pyrochlores
Authors:K.B. Helean  S.V. Ushakov  A. Navrotsky  J. Lian  J.M. Farmer
Affiliation:
  • a Department of Chemical Engineering and Materials Science, Thermochemistry Facility, NEAT ORU, The University of California at Davis, One Sheilds Avenue, Davis, CA 95616, USA
  • b Department of Nuclear Engineering and Radiological Sciences, University of Michigan, Ann Arbor, MI 48109-2104, USA
  • c Department of Materials Science and Engineering, University of Michigan, Ann Arbor, MI 48109-2104, USA
  • d Oak Ridge National Laboratory, Solid State Division, Oak Ridge, TN 37831-6056, USA
  • Abstract:High-temperature oxide melt solution calorimetry and Rietveld refinements of powder X-ray diffraction data were used to investigate the structure (Fd3m; Z=8) and energetics of a series of RE2Ti2O7 (RE=Sm-Lu) compounds with the pyrochlore structure as well as La2Ti2O7 with a layered perovskite-type structure. All of the RE-titanates were found to be stable in enthalpy with respect to their oxides. In the pyrochlore series, Lu2Ti2O7 was least stable in enthalpy (ΔHf-ox at 298 K=−56.0±4.0 kJ/mol); the most stable materials were Gd-, Eu-, and Sm2Ti2O7 with ΔHf-ox at 298 K=−113.4±2.7, −106.1±4.2, −115.4±4.2 kJ/mol, respectively. In general, as the radius ratio of the A- to B-site cations, RA/RB, decreases, the pyrochlore structure becomes less stable. The trend of ionic radius of the RE3+ cation vs. ΔHf-ox at 298 K is non-linear and approximately parallels the increasing “resistance” to ion-beam-induced amorphization as RA/RB decreases.
    Keywords:Thermodynamics   Pyrochlore   Nuclear waste   Enthalpy
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