The substitution of rare-earth ions into insulating host crystals introduce
s lattice strains and, for non-trivalent sites, a need for charge compensat
ion. Such effects alter the site symmetry and this is reflected in properti
es such as the wavelength, linewidth, lifetime and relative intensity of th
e rare-earth transitions. Equally clear, but less well documented, is the i
nfluence on second-harmonic generation (even from cubic crystal lattices).
For example, in bismuth germanate, second-harmonic generation efficiency va
ries by factors of more than 100 as a result of different rare-earth dopant
ions. The ions are variously incorporated as substitutional ions, pairs, c
lusters, or even as precipitates of new phases, but the detailed modelling
is often speculative. This article summarizes some recent studies which exp
lore the role of rare-earth ions in thermoluminescence and second-harmonic
generation. There are numerous differences in glow peak temperature, for no
minally the same defect sites, which are thought to indicate charge trappin
g and recombination within coupled defect sites, or within a large complex.
Size and cluster effects can be modified by heat treatments. This review c
onsiders the similarity and trends seen between numerous host lattices whic
h are doped with rare-earth ions. For thermoluminescence there are trends i
n the variation in glow peak temperature with ion size, with movements of 2
0 to 50 It. Examples are seen in many hosts with extreme effects being sugg
ested for zircon, with peak shifts of 200 K (probably from precipitate phas
es).