Home Structural anisotropy and annealing-induced nanoscale atomic rearrangements in metamict titanite
Article
Licensed
Unlicensed Requires Authentication

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

  • Tobias Beirau EMAIL logo , Boriana Mihailova , Galina Matveeva , Ute Kolb , Thomas Malcherek , Lee A. Groat and Ulrich Bismayer
Published/Copyright: April 2, 2015
Become an author with De Gruyter Brill

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 TiO6 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 TiO6 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 SiO4-TiO6-SiO4-TiO6 rings comprising TiO6 octahedra from different chains, whereas the radiationinduced 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 SiO4-TiO6 connectivity within planes nearly perpendicular to the TiO6 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 × 1018 α-event/g.

Received: 2011-10-10
Accepted: 2012-4-27
Published Online: 2015-4-2
Published in Print: 2012-8-1

© 2015 by Walter de Gruyter Berlin/Boston

Articles in the same Issue

  1. Actinides in Geology, Energy, and the Environment. Petrography and geochronology of the Pele Mountain quartz-pebble conglomerate uranium deposit, Elliot Lake District, Canada
  2. Celadonite in continental flood basalts of the Columbia River Basalt Group
  3. Thermodynamics of manganese oxides: Effects of particle size and hydration on oxidation-reduction equilibria among hausmannite, bixbyite, and pyrolusite
  4. Grossular: A crystal-chemical, calorimetric, and thermodynamic study
  5. Redetermination of high-temperature heat capacity of Mg2SiO4 ringwoodite: Measurement and lattice vibrational model calculation
  6. Thermal behavior of realgar As4S4, and of arsenolite As2O3 and non-stoichiometric As8S8+x crystals produced from As4S4 melt recrystallization
  7. Thermodynamics of the magnetite-ulvöspinel (Fe3O4-Fe2TiO4) solid solution
  8. Raman spectroscopy of (Ca,Mg)MgSi2O6 clinopyroxenes
  9. In-situ Raman spectroscopic study of sulfur speciation in oxidized magmatic-hydrothermal fluids
  10. Structural anisotropy and annealing-induced nanoscale atomic rearrangements in metamict titanite
  11. Hydrous fluid as the growth media of natural polycrystalline diamond, carbonado: Implication from IR spectra and microtextural observations
  12. Metastable equilibrium in the C-H-O system: Graphite deposition in crustal fluids
  13. Controlled morphogenesis of amorphous silica and its relevance to biosilicification
  14. Structural relaxation in tetrahedrally coordinated Co2+ along the gahnite-Co-aluminate spinel solid solution
  15. Limitations of Fe2+ and Mn2+ site occupancy in tourmaline: Evidence from Fe2+- and Mn2+-rich tourmaline
  16. Isothermal compression of face-centered cubic iron
  17. Bonding and structural changes in siderite at high pressure
  18. Energetics and kinetics of carbonate orientational ordering in vaterite calcium carbonate
  19. Growth process and crystallographic properties of ammonia-induced vaterite
  20. Argesite, (NH4)7Bi3Cl16, a new mineral from La Fossa Crater, Vulcano, Aeolian Islands, Italy: A first example of the [Bi2Cl10]4− anion
  21. Experimental study of mineral equilibria in the system K2O(Li2O)-Al2O3-SiO2-H2O-HF at 300 to 600 °C and 100 MPa with application to natural greisen systems
  22. Tobelite and NH+4-rich muscovite single crystals from Ordovician Armorican sandstones (Brittany, France): Structure and crystal chemistry
  23. The enigmatic iron oxyhydroxysulfate nanomineral schwertmannite: Morphology, structure, and composition
  24. Ferric iron and water incorporation in wadsleyite under hydrous and oxidizing conditions: A XANES, Mössbauer, and SIMS study
  25. Kircherite, a new mineral of the cancrinite-sodalite group with a 36-layer stacking sequence: Occurrence and crystal structure
  26. Molecular models of birnessite and related hydrated layered minerals
  27. Letter: Gold-telluride nanoparticles revealed in arsenic-free pyrite
  28. Letter: XAS evidence for the stability of polytellurides in hydrothermal fluids up to 599 °C, 800 bar
Downloaded on 10.9.2025 from https://www.degruyterbrill.com/document/doi/10.2138/am.2012.4024/html
Scroll to top button