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Temperature dependence of ion track formation in quartz and apatite

Schauries, D. ; Lang, M. ; Pakarinen, O. H. ; Botis, S. ; Afra, B. ; Rodriguez, M. D. ; Djurabekova, F. ; Nordlund, K. ; Severin, D. ; Bender, M. ; Li, W. X. ; Trautmann, C. ; Ewing, R. C. ; Kirby, N. ; Kluth, P. (2013)
Temperature dependence of ion track formation in quartz and apatite.
In: Journal of Applied Crystallography, 46 (6)
doi: 10.1107/S0021889813022802
Artikel, Bibliographie

Kurzbeschreibung (Abstract)

Ion tracks were created in natural quartz and fluorapatite from Durango, Mexico, by irradiation with 2.2 GeV Au ions at elevated temperatures of up to 913 K. The track radii were analysed using small-angle X-ray scattering, revealing an increase in the ion track radius of approximately 0.1 nm per 100 K increase in irradiation temperature. Molecular dynamics simulations and thermal spike calculations are in good agreement with these values and indicate that the increase in track radii at elevated irradiation temperatures is due to a lower energy required to reach melting of the material. The post-irradiation annealing behaviour studied for apatite remained unchanged.

Typ des Eintrags: Artikel
Erschienen: 2013
Autor(en): Schauries, D. ; Lang, M. ; Pakarinen, O. H. ; Botis, S. ; Afra, B. ; Rodriguez, M. D. ; Djurabekova, F. ; Nordlund, K. ; Severin, D. ; Bender, M. ; Li, W. X. ; Trautmann, C. ; Ewing, R. C. ; Kirby, N. ; Kluth, P.
Art des Eintrags: Bibliographie
Titel: Temperature dependence of ion track formation in quartz and apatite
Sprache: Englisch
Publikationsjahr: 2013
Titel der Zeitschrift, Zeitung oder Schriftenreihe: Journal of Applied Crystallography
Jahrgang/Volume einer Zeitschrift: 46
(Heft-)Nummer: 6
DOI: 10.1107/S0021889813022802
Kurzbeschreibung (Abstract):

Ion tracks were created in natural quartz and fluorapatite from Durango, Mexico, by irradiation with 2.2 GeV Au ions at elevated temperatures of up to 913 K. The track radii were analysed using small-angle X-ray scattering, revealing an increase in the ion track radius of approximately 0.1 nm per 100 K increase in irradiation temperature. Molecular dynamics simulations and thermal spike calculations are in good agreement with these values and indicate that the increase in track radii at elevated irradiation temperatures is due to a lower energy required to reach melting of the material. The post-irradiation annealing behaviour studied for apatite remained unchanged.

Freie Schlagworte: temperature dependence, ion track formation, quartz, apatite
Fachbereich(e)/-gebiet(e): 11 Fachbereich Material- und Geowissenschaften > Materialwissenschaft > Fachgebiet Ionenstrahlmodifizierte Materialien
11 Fachbereich Material- und Geowissenschaften > Materialwissenschaft
11 Fachbereich Material- und Geowissenschaften
Hinterlegungsdatum: 21 Mär 2014 13:27
Letzte Änderung: 21 Mär 2014 13:27
PPN:
Sponsoren: PK acknowledges the Australian Research Council for financial support., ML and RCE were supported by the Office of Basic Energy Sciences of the USDOE (DE-FG02-97ER45656).
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