We present Linear-Modulation OSL (LM-OSL) curves from several different typ
es of quartz, including sedimentary quartz, bulk rock crystal and synthetic
quartz. The LM-OSL method consists of linearly increasing the intensity of
the stimulation light while continuously monitoring the OSL emission from
the sample. With this technique, one obtains peaks of luminescence intensit
y versus time (Bulur, 1996) in which the position of the peak is inversely
related to the photoionization cross-section of the trap. The shape of the
LM-OSL curve is directly related to the shape of the conventional OSL decay
curve in which the stimulating light source is maintained at constant inte
nsity (so-called Continuous-Wave OSL, or CW-OSL). In the latter, the OSL fr
om the traps with the highest photoionization cross-section decays most rap
idly with stimulation time, while OSL from those traps with smaller photoio
nization cross-sections is characterized by longer decay times. In this pap
er, data are presented comparing the CW-OSL and LM-OSL curves for several d
ifferent quartz types with particular focus on the changes in the shapes of
each of these curves with sample type pre-heat temperature, acid measureme
nt temperature. Several different LM-OSL components are found for each samp
le, each with different photoionization cross-sections, but a universal beh
avior for quartz is not observed; each sample is different. From the depend
ence upon pre-heat temperature, features associated with shallow traps can
be identified. Traps which empty very rapidly can be observed more easily i
n the LM-OSL curves than in the conventional CW-OSL curves, and the tempera
ture dependence of the photoionization cross-section for the various compon
ents can be clearly discerned. (C) 2000 Elsevier Science Ltd. All rights re
served.