Annealing behaviour of ion tracks in olivine, apatite and britholite
dc.contributor.author | Afra, Boshra | |
dc.contributor.author | Lang, M | |
dc.contributor.author | Bierschenk, Thomas | |
dc.contributor.author | Rodriguez, Matias | |
dc.contributor.author | Weber, William | |
dc.contributor.author | Trautmann, Christina | |
dc.contributor.author | Ewing, R. C. | |
dc.contributor.author | Kirby, N | |
dc.contributor.author | Kluth, Patrick | |
dc.date.accessioned | 2015-12-10T23:36:37Z | |
dc.date.issued | 2014 | |
dc.date.updated | 2015-12-10T11:55:40Z | |
dc.description.abstract | Ion tracks were created in olivine from San Carlos, Arizona (95% Mg2SiO4), apatite (Ca5(PO4)3(F,Cl,O)) from Durango, Mexico, and synthetic silicates with the apatite structure: Nd8Sr2(SiO4)6O2 and Nd8Ca2(SiO4)6O2 using 1.6 and 2.2 GeV Au ions. The morphology and annealing behaviour of the tracks were investigated by means of synchrotron based small angle X-ray scattering in combination with ex situ annealing. Tracks in olivine annealed above ∼400 °C undergo a significant change in track radius due to recrystallisation of the damage tracks. At temperatures higher than 620°C, the scattering images indicate fragmentation of the track cylinders into smaller subsections. Ion tracks were annealed at elevated temperatures up to 400°C in the Durango and Ca-britholite, and up to 560°C in Sr-britholite. While there was a significant change in the track radii in the Durango apatite, tracks in the two synthetic samples remained almost unchanged. | |
dc.identifier.issn | 0168-583X | |
dc.identifier.uri | http://hdl.handle.net/1885/70218 | |
dc.publisher | Elsevier | |
dc.source | Nuclear Instruments and Methods in Physics Research: Section B | |
dc.title | Annealing behaviour of ion tracks in olivine, apatite and britholite | |
dc.type | Journal article | |
local.bibliographicCitation.lastpage | 130 | |
local.bibliographicCitation.startpage | 126 | |
local.contributor.affiliation | Afra, Boshra, College of Physical and Mathematical Sciences, ANU | |
local.contributor.affiliation | Lang, M, University of Michigan | |
local.contributor.affiliation | Bierschenk, Thomas, College of Physical and Mathematical Sciences, ANU | |
local.contributor.affiliation | Rodriguez, Matias, College of Physical and Mathematical Sciences, ANU | |
local.contributor.affiliation | Weber, William, University of Tennessee | |
local.contributor.affiliation | Trautmann, Christina, Gesellschaft fur Schwerionenforschung | |
local.contributor.affiliation | Ewing, R. C., University of Michigan | |
local.contributor.affiliation | Kirby, N, Australian Synchrotron | |
local.contributor.affiliation | Kluth, Patrick, College of Physical and Mathematical Sciences, ANU | |
local.contributor.authoremail | u4905535@anu.edu.au | |
local.contributor.authoruid | Afra, Boshra, u4565723 | |
local.contributor.authoruid | Bierschenk, Thomas, u4905535 | |
local.contributor.authoruid | Rodriguez, Matias, u4105856 | |
local.contributor.authoruid | Kluth, Patrick, u4054452 | |
local.description.embargo | 2037-12-31 | |
local.description.notes | Imported from ARIES | |
local.identifier.absfor | 020406 - Surfaces and Structural Properties of Condensed Matter | |
local.identifier.absseo | 970102 - Expanding Knowledge in the Physical Sciences | |
local.identifier.ariespublication | U3488905xPUB2255 | |
local.identifier.citationvolume | 326 | |
local.identifier.doi | 10.1016/j.nimb.2013.10.072 | |
local.identifier.scopusID | 2-s2.0-84899438936 | |
local.identifier.thomsonID | 000335631300031 | |
local.identifier.uidSubmittedBy | U3488905 | |
local.type.status | Published Version |
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