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Positron annihilation lifetime study of radiation-damaged natural zircons

dc.contributor.authorRoberts, Jason
dc.contributor.authorGaugliardo, P
dc.contributor.authorFarnan, I
dc.contributor.authorZhang, M
dc.contributor.authorVance, E R
dc.contributor.authorDavis, J
dc.contributor.authorKaratchevtseva, I
dc.contributor.authorKnott, Robert
dc.contributor.authorMudie, Stephen T.
dc.contributor.authorBuckman, Stephen
dc.contributor.authorSullivan, James
dc.date.accessioned2016-06-14T23:20:47Z
dc.date.issued2016
dc.date.updated2016-06-14T08:52:56Z
dc.description.abstractZircons are a well-known candidate waste form for actinides and their radiation damage behaviour has been widely studied by a range of techniques. In this study, well-characterised natural single crystal zircons have been studied using Positron Annihilation Lifetime Spectroscopy (PALS). In some, but not all, of the crystals that had incurred at least half of the alpha-event damage of ~1019 a/g required to render them structurally amorphous, PALS spectra displayed long lifetimes corresponding to voids of ~0.5 nm in diameter. The long lifetimes corresponded to expectations from published Small-Angle X-ray Scattering data on similar samples. However, the non-observation by PALS of such voids in some of the heavily damaged samples may reflect large size variations among the voids such that no singular size can be distinguished or. Characterisation of a range of samples was also performed using scanning electron microscopy, optical absorption spectroscopy, Raman scattering and X-ray scattering/diffraction, with the degree of alpha damage being inferred mainly from the Raman technique and X-ray diffraction. The observed void diameters and intensities of the long lifetime components were changed somewhat by annealing at 700 C; annealing at 1200 C removed the voids entirely. The voids themselves may derive from He gas bubbles or voids created by the inclusion of small quantities of organic and hydrous matter, notwithstanding the observation that no voidage was evidenced by PALS in two samples containing hydrous and organic matter.
dc.identifier.issn0022-3115
dc.identifier.urihttp://hdl.handle.net/1885/103551
dc.publisherElsevier
dc.sourceJournal of Nuclear Materials
dc.titlePositron annihilation lifetime study of radiation-damaged natural zircons
dc.typeJournal article
local.bibliographicCitation.lastpage50
local.bibliographicCitation.startpage44
local.contributor.affiliationRoberts, Jason, College of Physical and Mathematical Sciences, ANU
local.contributor.affiliationGaugliardo, P, University of Western Australia
local.contributor.affiliationFarnan, I, University of Cambridge
local.contributor.affiliationZhang, M, University of Cambridge
local.contributor.affiliationVance, E R, ANSTO
local.contributor.affiliationDavis, J, ANSTO
local.contributor.affiliationKaratchevtseva, I, ANSTO
local.contributor.affiliationKnott, Robert, Australian Nuclear Science and Technology Organisation
local.contributor.affiliationMudie, Stephen T., Australian Synchrotron
local.contributor.affiliationBuckman, Stephen, College of Physical and Mathematical Sciences, ANU
local.contributor.affiliationSullivan, James, College of Physical and Mathematical Sciences, ANU
local.contributor.authoruidRoberts, Jason, u4444321
local.contributor.authoruidBuckman, Stephen, u8300485
local.contributor.authoruidSullivan, James, u3551013
local.description.embargo2037-12-31
local.description.notesImported from ARIES
local.identifier.absfor020406 - Surfaces and Structural Properties of Condensed Matter
local.identifier.ariespublicationU3488905xPUB8361
local.identifier.citationvolume471
local.identifier.doi10.1016/j.jnucmat.2015.12.008
local.identifier.scopusID2-s2.0-84954412866
local.type.statusPublished Version

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