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|Title: ||Ion irradiation of the TiO2 polymorphs and cassiterite.|
|Authors: ||Lumpkin, GR|
Transmission Electron Microscopy
|Issue Date: ||Jan-2010|
|Publisher: ||Mineralogical Society of America|
|Citation: ||Lumpkin, G. R., Blackford, M. G., Smith, K. L., Whittle, K. R., Zaluzec, N. J., Ryan, E. A., et al. (2010). Ion irradiation of the TiO2 polymorphs and cassiterite. American Mineralogist, 95(1), 192-195.|
|Abstract: ||Thin crystals of rutile, brookite, anatase, and cassiterite were irradiated in situ in the transmission electron microscope using 1.0 MeV Kr ions at 50–300 K. Synthetic rutile and natural cassiterite, with 0.1–0.2 wt% impurities, remain crystalline up to a fluence of 5 x 1015 ions cm–2 without evidence for amorphization at 50 K. Natural brookite and anatase, with 0.3–0.5 wt% impurities, become amorphous at fluences of 8.1 x 1014 and 2.3 x 1014 ions cm–2, respectively. We have also studied two natural rutile samples containing ~1.7 and 1.2 wt% impurities. These samples became amorphous at 9.2 x 1014 and 8.6 x 1014 ions cm–2 at 50 K, respectively. Further analyses of the fluence-temperature data for natural brookite, rutile, and anatase give critical amorphization temperatures of 168 ± 11, 209 ± 8, and 242 ± 6 K, respectively. Results are briefly discussed with respect to several criteria for radiation resistance, including aspects of the structure, bonding, and energetics of defect formation and migration. © 2010, Mineralogical Society of America|
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