Micro-Raman and micro-infrared spectroscopic studies of Pb- and Au-irradiated ZrSiO4: Optical properties, structural damage, and amorphization
Creators
- 1. Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge CB2 3EQ (United Kingdom)
- 2. Materials Science and Technology Division, Oak Ridge National Laboratory, Oak Ridge, Tennessee 37831-6056 (United States)
- 3. Department of Geological Sciences, University of Michigan, Ann Arbor, Michigan 48109-1005 (United States)
- 4. Laboratoire de Physique de l'Etat Condense (LPEC), UMR CNRS 6087, Universite du Maine-Faculte des Sciences, Avenue Olivier Messiaen-72085 Le Mans Cedex 9 (France)
- 5. Pacific Northwest National Laboratory, P.O. Box 999, Richland, Washington 99352 (United States)
Description
The optical properties of damaged periodic and aperiodic domains created by Pb+ (280 keV) and Au4+ (10 MeV) implantation of zircon were studied using micro-infrared (IR) and micro-Raman spectroscopy. The Pb+ and Au4+ irradiations caused a dramatic decrease in the IR reflectivity similar to that observed for metamict natural zircon. The irradiation with 10 MeV Au4+ ions (to fluences of 1x1015 Au4+ ions/cm2) also results in the formation of an amorphized phase similar to that observed in metamict zircon. These results show that high-energy, heavy-ion irradiations provide a good simulation of the ballistic effects of the recoil nucleus of an alpha-decay event and, in both cases, the result is the creation of aperiodic domains. Additional IR and Raman features were recorded in samples irradiated with 280 keV Pb+ ions (to fluences of 1x1014 and 1x1015 Pb+ ions/cm2), indicating the formation of an irradiation-induced additional phase(s). The frequencies of the features are consistent with lead silicates, ZrO2, and SiO2. The results show that spectral features of the Au4+- and Pb+-irradiated zircon are different from those of quenched ZrSiO4 melts, and the finding further confirms that the amorphous state produced by high-energy ion irradiations is structurally different from the glassy state that results from quenching a high temperature melt. In contrast to significant changes in the frequency and width of the Raman ν3 band observed in metamict zircon, the Pb+ and Au4+ irradiations do not cause similar variations, indicating that the remaining zircon crystalline domains in irradiated samples have a crystalline structure with fewer defects than those of metamict zircon
Additional details
Identifiers
Publishing Information
- Journal Title
- Physical Review. B, Condensed Matter and Materials Physics
- Journal Volume
- 77
- Journal Issue
- 14
- Journal Page Range
- p. 144110-144110.13
- ISSN
- 1098-0121
INIS
- Country of Publication
- United States
- Country of Input or Organization
- International Atomic Energy Agency (IAEA)
- INIS RN
- 40023183
- Subject category
- S36: MATERIALS SCIENCE;
- Descriptors DEI
- ALPHA DECAY; AMORPHOUS STATE; CRYSTAL DEFECTS; CRYSTAL STRUCTURE; GOLD IONS; HEAVY IONS; INFRARED SPECTRA; ION BEAMS; ION IMPLANTATION; IRRADIATION; KEV RANGE 100-1000; LEAD IONS; LEAD SILICATES; MEV RANGE 01-10; MULTICHARGED IONS; OPTICAL PROPERTIES; PERIODICITY; PHYSICAL RADIATION EFFECTS; RAMAN SPECTRA; RAMAN SPECTROSCOPY; REFLECTIVITY; SILICA; SILICON OXIDES; SIMULATION; TEMPERATURE RANGE 0400-1000 K; ZIRCON; ZIRCONIUM OXIDES; ZIRCONIUM SILICATES
- Descriptors DEC
- BEAMS; CHALCOGENIDES; CHARGED PARTICLES; CRYSTAL STRUCTURE; DECAY; ENERGY RANGE; IONS; KEV RANGE; LASER SPECTROSCOPY; LEAD COMPOUNDS; MEV RANGE; MINERALS; NUCLEAR DECAY; OPTICAL PROPERTIES; OXIDE MINERALS; OXIDES; OXYGEN COMPOUNDS; PHYSICAL PROPERTIES; RADIATION EFFECTS; SILICATE MINERALS; SILICATES; SILICON COMPOUNDS; SPECTRA; SPECTROSCOPY; SURFACE PROPERTIES; TEMPERATURE RANGE; TRANSITION ELEMENT COMPOUNDS; VARIATIONS; ZIRCONIUM COMPOUNDS
Optional Information
- Notes
- (c) 2008 The American Physical Society