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.