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Structural anisotropy and annealing-induced nanoscale atomic rearrangements in metamict titanite.

Authors :
Beirau, Tobias
Mihailova, Boriana
Matveva, Galina
Kolb, Ute
Malcherek, Thomas
Groat, Lee A.
Bismayer, Ulrich
Source :
American Mineralogist; Aug/Sep2012, Vol. 97 Issue 8/9, p1354-1365, 12p
Publication Year :
2012

Abstract

The structural state of metamict titanite was studied by Raman spectroscopy, complementary high-resolution transmission electron microscopy, and single-crystal X-ray diffraction. The results show that Raman scattering collected from metamict titanite is highly anisotropic, which is typical of single crystals. But surprisingly, the observed Raman-scattering dependence on the sample orientation is much more pronounced for heavily metamict than for weakly metamict titanite samples. These radiation-induced anisotropic effects are related to the specific atomic arrangements in metamict titanite. The Raman spectra collected in backscattering geometry from a plane nearly perpendicular to the chains of corner-sharing TiO<subscript>6</subscript> octahedra arise predominantly from phonon modes in crystalline nanoregions with radiation-induced defects, whereas the contribution of atomic vibrations in radiation-induced amorphous nanoregions is better pronounced in the Raman spectra collected from a plane containing TiO<subscript>6</subscript> chains. This difference provides a unique opportunity to study separately, the structural transformations of the crystalline and amorphous fractions in metamict titanite. The results show that the radiation-induced periodic faults in the crystalline matrix are related to the disturbance of SiO<subscript>4</subscript>-TiO<subscript>6</subscript>-SiO<subscript>4</subscript>-TiO<subscript>6</subscript> rings comprising TiO<subscript>6</subscript> octahedra from different chains, whereas the radiation-induced amorphization is related to the partial change of Ti coordination from octahedral to pyramidal and/or tetrahedral, which in turn violates the Ti-O-Ti intrachain linkages. This indicates that the plane containing Si-O-Ti-O bond rings is less susceptible to a self-accumulation of radiation-induced defects resulting in the development of amorphous regions as compared to the perpendicular plane containing Ti-O bond chains. Sample-orientation-dependent Raman spectroscopy was further applied to annealed metamict titanite to give further insight into the temperature-driven recovery processes in the crystalline and amorphous nanoregions. Multistep annealing by 50 K for 2 h per step gradually suppresses the structural defects in the crystalline fraction as the improvement of the SiO<subscript>4</subscript>-TiO<subscript>6</subscript> connectivity within planes nearly perpendicular to the TiO<subscript>6</subscript> chains reaches saturation near 900 K. The annealing-induced recrystallization of the radiation-induced amorphous nanoregions takes place in the temperature range between approximately 650 and 950 K, with a maximum near 750 K. Raman scattering shows that multistep annealing up to 1173 K is insufficient to recover the crystalline structure of the studied metamict titanite sample, which has an accumulated radiation dose of 1.2 x 10<subscript>18</subscript> α-event/g. [ABSTRACT FROM AUTHOR]

Details

Language :
English
ISSN :
0003004X
Volume :
97
Issue :
8/9
Database :
Complementary Index
Journal :
American Mineralogist
Publication Type :
Academic Journal
Accession number :
79268664
Full Text :
https://doi.org/10.2138/am.2012.4024