| 2006 Philadelphia Annual Meeting (22–25 October 2006) | |
| Paper No. 62-3 | |
| Presentation Time: 8:30 AM-8:45 AM | ||
RADIATION DAMAGE IN LA- AND TH-DOPED YTTRIUM TITANATES | ||
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EWING, Rodney C., Geological Sciences, University of Michigan, 1100 N. University, Ann Arbor, MI 48109-1005, rodewing@umich.edu and LIAN, Jie, Geological Sciences, University of Michigan, 1100 N. University, Ann Arbor, MI 48103 Pyrochlore, A2B2O7, is a phase that has received considerable attention for the immobilization of plutonium and the “minor” actinides, Np, Cm, Am. Y2Ti2O2 pyrochlore, doped with La, have been sintered at 1373 K for 12 h with designed compositions of (LaxY1-x)2Ti2O7 (x = 0, 0.08, 0.5, and 1), and the phase compositions were analyzed by X-ray diffraction. Limited amounts of La were incorporated into yttrium titanate pyrochlore structure for La-doped samples; while, the end member composition of La2Ti2O7 formed a layered perovskite structure. Ion beam-induced amorphization occurred for all compositions in the (LaxY1-x)2Ti2O7 binary under 1 MeV Kr2+ irradiation at room temperature, and the critical amorphization dose decreased with increasing amounts of La3+. The critical amorphization temperatures for Y2Ti2O7, (La0.162Y0.838)2Ti2O7 and La2Ti2O7 were determined to be ~780, 890 and 920 K, respectively. Th4+ and Fe3+-doped yttrium titanate pyrochlores were synthesized at 1373 K by sintering Y2Ti2O7 with (ThO2+Fe2O3). Pyrochlore structures and the chemical composition were primarily identified by the X-ray diffraction and energy dispersive X-ray (EDX) measurements. The unit cell parameter and the critical amorphization dose (1 MeV Kr2+ at room temperature) increase for yttrium titanate pyrochlores with the addition of Th. The increasing “resistance” to amorphization with less La and greater Th and Fe contents for (Y1-xLax)2Ti2O7 and Y2Ti2O7-Fe2O3-ThO2 systems, respectively, are consistent with the changes in the average ionic radius ratio at the A-sites and B-sites. These results suggest that the addition of lanthanides and actinides (e.g., Th, U, or Pu) will affect the structural stability, as well as the radiation response behavior of the pyrochlore structure-type. | ||
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2006 Philadelphia Annual Meeting (22–25 October 2006)
General Information for this Meeting | ||
| Session No. 62 Mineralogy/Crystallography/Metamorphism Pennsylvania Convention Center: 112 A 8:00 AM-12:00 PM, Monday, 23 October 2006 Geological Society of America Abstracts with Programs, Vol. 38, No. 7, p. 167 | ||
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