Radioluminescence and thermoluminescence of rare earth element and phosphorus-doped zircon

Citation
T. Karali et al., Radioluminescence and thermoluminescence of rare earth element and phosphorus-doped zircon, AM MINERAL, 85(5-6), 2000, pp. 668-681
Citations number
32
Categorie Soggetti
Earth Sciences
Journal title
AMERICAN MINERALOGIST
ISSN journal
0003004X → ACNP
Volume
85
Issue
5-6
Year of publication
2000
Pages
668 - 681
Database
ISI
SICI code
0003-004X(200005/06)85:5-6<668:RATORE>2.0.ZU;2-7
Abstract
The radioluminescence and thermoluminescence spectra of synthetic zircon cr ystals doped with individual trivalent rare earth element (REE) ions (Pr, S m, Eu, Gd, Dy, Ho Er, and Yb) and P are reported in the temperature range 2 5 to 673 K. Although there is some intrinsic UV/blue emission from the host lattice, the dominant signals are from the rare-earth sites, with signals characteristic of the REE3+ states. The shapes of the glow curves are diffe rent for each dopant, and there are distinct differences between glow peak temperatures for different rare-earth lines of the same element. Within the overall set of signals there are indications of linear trends in which som e glow peak temperatures vary as a function of the ionic size of the rare e arth ions. The temperature shifts of the peaks are considerable, up to 200 degrees, and much larger than those cited in other rare-earth-doped crystal s of LaF3 and Bi4Ge3O12. The data clearly suggest that the rare-earth ions are active both in the trapping and luminescence steps, and hence the TL oc curs within localized defect complexes that include REE3+ ions.