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The CaO-TiO{sub 2}-ZrO{sub 2} system at 1200 C and the solubilities of Hf and Gd in zirconolite

Book ·
OSTI ID:264439
;  [1];  [2]
  1. Lawrence Livermore National Lab., CA (United States). Chemistry and Materials Science
  2. Univ. of Wisconsin, Madison, WI (United States). Dept. of Geology and Geophysics
Phase equilibria are established in the CaO-TiO{sub 2}-ZrO{sub 2} system at 1,200 C, using X-ray diffraction and electron probe microanalysis. The existence of two previously reported ternary phases, zirconolite (CaZrTi{sub 2}O{sub 7}) and calzirtite (Ca{sub 2}Zr{sub 5}Ti{sub 2}O{sub 16}), is confirmed. Each of these phases exhibits a significant range of homogeneity between TiO{sub 2} and ZrO{sub 2} while maintaining a nearly constant concentration of CaO. The ternary solubilities of the constituent binary phases are found to be negligible, with the exceptions of the perovskites, which display mutual solubility of at least 22 mol.% and may in fact form a series of continuous solid solutions. The solubilities of Hf and Gd in zirconolite are also investigated. While Hf-bearing samples did not reach thermodynamic equilibrium under the experimental conditions employed, the existence of a Hf analog to zirconolite, CaHfTi{sub 2}O{sub 7}, is conclusively demonstrated. The phase is stable at the stoichiometric composition, and its lattice parameters are very close to those reported in the literature for stoichiometric zirconolite. A Gd-bearing sample of the composition Ca{sub 0.88}Zr{sub 0.88}Gd{sub 0.24}Ti{sub 2}O{sub 7} is found to be essentially single phase zirconolite, in agreement with previous investigations at higher temperatures.
DOE Contract Number:
W-7405-ENG-48
OSTI ID:
264439
Report Number(s):
CONF-951155--; ISBN 1-55899-315-0
Country of Publication:
United States
Language:
English