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Annealing of -decay damage in zircon: a Raman spectroscopic study

dc.contributor.authorZhang, Mingen_US
dc.contributor.authorSalje, Ekhard K. H.en_US
dc.contributor.authorCapitani, Gian Carloen_US
dc.contributor.authorLeroux, Huguesen_US
dc.contributor.authorClark, Andrew M.en_US
dc.contributor.authorSchlüter, Jochenen_US
dc.contributor.authorEwing, Rodney C.en_US
dc.date.accessioned2006-12-19T18:56:21Z
dc.date.available2006-12-19T18:56:21Z
dc.date.issued2000-04-03en_US
dc.identifier.citationZhang, Ming; Salje, Ekhard K H; Capitani, Gian Carlo; Leroux, Hugues; Clark, Andrew M; Schlüter, Jochen; Ewing, Rodney C (2000). "Annealing of -decay damage in zircon: a Raman spectroscopic study." Journal of Physics: Condensed Matter. 12(13): 3131-3148. <http://hdl.handle.net/2027.42/48882>en_US
dc.identifier.issn0953-8984en_US
dc.identifier.urihttps://hdl.handle.net/2027.42/48882
dc.description.abstractRecrystallization and structural recovery in -decay damage in zircon samples have been studied using Raman spectroscopy. Fifteen zircon samples with different degrees of radiation damage have been thermally annealed between 600 K and 1800 K for up to 28 days and 8 hours. The experimental results from this study reveal that recrystallization in the damaged zircon samples is a multi-stage process that depends on the degree of initial damage of the samples. In partially damaged samples the lattice recovery of damaged crystalline ZrSiO4 takes place at temperatures as low as about 700 K, as shown by a remarkable band-sharpening and a significant increase in the frequencies of 1 and 3 Si-O stretching vibrations together with the external band near 357 cm-1 with increasing temperature. A dramatic increase of Raman scattering intensity of ZrSiO4 occurs in partially damaged samples near 1000 K due to a recrystallization process involving epitaxial growth. Heavily damaged samples tend to decompose into ZrO2 and SiO2 at high temperatures. Tetragonal ZrO2 has been observed under annealing between 1125 K and about 1600 K in heavily damaged samples while monoclinic ZrO2 appears above 1600 K. Weak signals from ZrSiO4 were detected at 1125 K in highly metamict zircon although the main recrystallization appears to occur near 1500 K accompanied by a decrease of the volumes of ZrO2 as well as SiO2 . This suggests that this recrystallization is associated with the reaction of ZrO2 with SiO2 to form ZrSiO4 . A possible intermediate phase has been observed, for the first time, by Raman spectroscopy in damaged zircons annealed at temperatures between 800 K and 1400 K. This phase is characterized by strong, broad Raman signals near 670, 798 and 1175 cm-1 . Prolonged isothermal annealing at 1050 K results in a decrease of these characteristic bands and eventually the disappearance of this intermediate phase.en_US
dc.format.extent3118 bytes
dc.format.extent561343 bytes
dc.format.mimetypetext/plain
dc.format.mimetypeapplication/pdf
dc.language.isoen_US
dc.publisherIOP Publishing Ltden_US
dc.titleAnnealing of -decay damage in zircon: a Raman spectroscopic studyen_US
dc.typeArticleen_US
dc.subject.hlbsecondlevelPhysicsen_US
dc.subject.hlbtoplevelScienceen_US
dc.description.peerreviewedPeer Revieweden_US
dc.contributor.affiliationumDepartment of Earth Sciences, University of Cambridge, Downing Street, Cambridge CB2 3EQ, UK Laboratoire de Structure et Propriétés de l'Etat Solide, Bâtiment C6, Université Sciences et Technologies de Lille, 59655 Villeneuve d'Ascq, France Department of Mineralogy, The Natural History Museum, Cromwell Road, London SW7 5BD, UK Mineralogisches Museum, Mineralogisch-Petrographisches Institut, Universität Hamburg, Grindelallee 48, D-20146 Hamburg, Germany Department of Nuclear Engineering and Radiological Sciences Department of Geological Sciences, University of Michigan, Ann Arbor, MI 48109-2104, USA M Zhang Ming Zhang, Ekhard K H Salje, Gian Carlo Capitani, Hugues Leroux, Andrew M Clark, Jochen Schlüter and Rodney C Ewingen_US
dc.contributor.affiliationumDepartment of Nuclear Engineering and Radiological Sciences Department of Geological Sciences, University of Michigan, Ann Arbor, MI 48109-2104, USAen_US
dc.contributor.affiliationotherDepartment of Earth Sciences, University of Cambridge, Downing Street, Cambridge CB2 3EQ, UKen_US
dc.contributor.affiliationotherDepartment of Earth Sciences, University of Cambridge, Downing Street, Cambridge CB2 3EQ, UKen_US
dc.contributor.affiliationotherLaboratoire de Structure et Propriétés de l'Etat Solide, Bâtiment C6, Université Sciences et Technologies de Lille, 59655 Villeneuve d'Ascq, Franceen_US
dc.contributor.affiliationotherLaboratoire de Structure et Propriétés de l'Etat Solide, Bâtiment C6, Université Sciences et Technologies de Lille, 59655 Villeneuve d'Ascq, Franceen_US
dc.contributor.affiliationotherDepartment of Mineralogy, The Natural History Museum, Cromwell Road, London SW7 5BD, UKen_US
dc.contributor.affiliationumcampusAnn Arboren_US
dc.description.bitstreamurlhttp://deepblue.lib.umich.edu/bitstream/2027.42/48882/2/c01321.pdfen_US
dc.identifier.doihttp://dx.doi.org/10.1088/0953-8984/12/13/321en_US
dc.identifier.sourceJournal of Physics: Condensed Matter.en_US
dc.owningcollnameInterdisciplinary and Peer-Reviewed


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