Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
European Journal of Mineralogy Signup for GSW Email News
JOURNAL HOME HELP FEEDBACK/COMMNET SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

European Journal of Mineralogy; July/August; v. 20; no. 4; p. 517-522; DOI: 10.1127/0935-1221/2008/0020-1842
© 2008 E. Schweizerbart'sche Verlagsbuchhandlung Science Publishers
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Krickl, R.
Right arrow Articles by Wirth, R.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Letters

Alpha-irradiation effects in SiO2

Robert Krickl1,*, Lutz Nasdala1, Jens Götze2, Dieter Grambole3 and Richard Wirth4

1 Institut für Mineralogie und Kristallographie, Universität Wien, 1090 Wien, Austria
2 Institut für Mineralogie, TU Bergakademie Freiberg, 09599 Freiberg, Germany
3 Forschungszentrum Dresden-Rossendorf, Institut für Ionenstrahlphysik und Materialforschung, 01328 Dresden, Germany
4 GeoForschungsZentrum Potsdam, 14473 Potsdam, Germany

* Corresponding author, e-mail: robert.krickl{at}univie.ac.at

Natural and synthetic crystalline {alpha}-quartz, as well as synthetic SiO2 glass, were irradiated with different doses of 8.8 MeV He2+ ions. The irradiation-induced alteration was characterised using Raman and cathodoluminescence (CL) spectroscopy, optical microscopy, transmission electron microscopy (TEM) and CL and electron microscope imaging. The initially dull bluish-violet CL colour of the two {alpha}-quartz samples was found to be transformed to bright yellow in the irradiated areas. The emission maximum was observed 45 µ m below the surface, which corresponds well with correlated helium trajectory lengths and defect density distribution. Both, total intensity and radial intensity distribution of the CL emission change with the irradiation dose. Observations suggest a nonlinear, approximately logarithmic increase of the CL intensity depending on the alpha dose. Significant broadening of Raman bands is only observed near the far end of helium trajectories. This broadening is not only caused by the structural radiation damage but also by strain between strongly and lowly damaged areas.

Key-words: Alpha-quartz, radiohalo, cathodoluminescence, Raman spectroscopy, He implantation, irradiation, radiation damage, transmission electron microscopy.




This article has been cited by other articles:


Home page
Mineral MagHome page
J. Gotze
Chemistry, textures and physical properties of quartz - geological interpretation and technical application
Mineralogical Magazine, November 13, 2009; 73(4): 645 - 671.
[Abstract] [Full Text] [PDF]


Home page
American MineralogistHome page
L. Nasdala
Pb+ irradiation of synthetic zircon (ZrSiO4): Infrared spectroscopic investigation--Discussion
American Mineralogist, May 1, 2009; 94(5-6): 853 - 855.
[Full Text] [PDF]




JOURNAL HOME HELP FEEDBACK/COMMNET SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2009 by E. Schweizerbart'sche Verlagsbuchhandlung Science Publishers