Optically stimulated luminescence

In physics, optically stimulated luminescence (OSL) is a method for measuring doses from ionizing radiation.

The method makes use of electrons trapped between the valence and conduction bands in the crystalline structure of certain types of matter (such as quartz, feldspar, and aluminum oxide). The trapping sites are imperfections of the lattice - impurities or defects. The ionizing radiation produces electron-hole pairs - electrons are in the conduction band and holes in the valence band. The electrons which have been excited to the conduction band may become entrapped in the electron or hole traps. Under stimulation of light the electrons may free themselves from the trap and get into the conduction band. From the conduction band they may recombine with holes trapped in hole traps. If the centre with the hole is a luminescence centre (radiative recombination centre) emission of light will occur. The photons are detected using a photomultiplier tube. The signal from the tube is then used to calculate the dose that the material had absorbed.

OSL is used in at least two different applications:

• optical dating of ancient materials: mainly geological sediments, but also sometimes fired pottery, bricks etc., although in the latter case thermoluminescence dating is used more often
• radiation dosimetry, which is the measurement of accumulated radiation dose in the tissues of health care, nuclear, research and other workers, as well as in building materials in regions of nuclear disaster

In order to carry out OSL dating, mineral grains have to be extracted from the sample. Most commonly these are so-called coarse grains - 100-200 μm, or fine grains - 4-11 μm. Occasionally other grain sizes are used.

The difference between radiocarbon dating and OSL is that the former is used to date organic materials, while the latter is used to date minerals. Events that can be dated using OSL are, for example, the mineral's last exposure to sunlight; Mungo Man, Australia's oldest human find, was dated in this manner. It is also used for dating the deposition of geological sediments after they have been transported by air (eolian sediments) or rivers (fluvial sediments). In archaeology, OSL dating is applied to the dating of ceramics: the dated event is the time of their last heating to a high temperature (in excess of 400 °C).

Recent OSL dating of stone tools in Arabia pushed the "out-of-Africa" date hypothesis of human migration back 50,000 years and added a possible path of migration from the African continent to the Arabian peninsula instead of through Europe.^{[1] [2]}

The most popular OSL method is called single-aliquot regeneration, or SAR.

References

1. ^ "Man Out Of Africa". Financial Times (requires registration) (London). 2010-11-27. http://www.ft.com/cms/s/2/56a08c08-2a36-11e0-b906-00144feab49a.html#axzz1CHIVzVhW. 
2. ^ Schmid, Randolph E. (2011-01-27). "Humans may have left Africa earlier than thought". http://news.yahoo.com/s/ap/20110127/ap_on_sc/us_sci_out_of_africa.