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Optically Stimulated Luminescence OSL dating has emerged within the last 20 years as a key Quaternary absolute dating tool, with a wide range of terrestrial and marine applications. Optical dating techniques employ ubiquitous quartz or feldspar grains to directly date the deposition of sedimentary units. As such, the optical dating methods allow the systematic chronological evaluation of Quaternary-age sedimentary sequences. Within the School of Geography and the Environment, the OLD Laboratory provides support particularly for the Landscape Dynamics research cluster, with a specific focus on low latitude environment and climate change, geoarchaeology and geomorphology. In addition our researchers continuously engage in efforts to improve and develop the methodology and to further advance our knowledge on the fundamental physical mechanisms underlying the dating method. The OLD Laboratory also provides a commercial luminescence dating service and works closely with clients in industry, archaeological organizations, environmental institutes and other academic groups.

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The Chairman will serve a maximum of four years. The major items comprise: Mandatory Annex 4 – Future Developments All future developments are planned around the advantages that will be afforded by the new AMS system to be delivered in the summer. Improved efficiency reduced turn-around times and higher throughput Improved precision allowing us to work towards higher precision dating – as the pre-treatment techniques develop Improved background allowing the reliable dating of older material, and perhaps more importantly the enhanced ability to study methodological issues arising with very old samples.

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The thermoluminescence technique is the only physical means of determining the absolute age of pottery presently available. It is an absolute dating method, and does not depend on comparison with similar objects as does obsidian hydration dating, for example. Most mineral materials, including the constituents of pottery, have the property of thermoluminescence TL , where part of the energy from radioactive decay in and around the mineral is stored in the form of trapped electrons and later released as light upon strong heating as the electrons are detrapped and combine with lattice ions.

By comparing this light output with that produced by known doses of radiation, the amount of radiation absorbed by the material may be found. When pottery is fired, it loses all its previously acquired TL, and on cooling the TL begins again to build up. Thus, when one measures dose in pottery, it is the dose accumulated since it was fired, unless there was a subsequent reheating.

If the radioactivity of the pottery itself, and its surroundings, is measured, the dose rate, or annual increment of dose, may be computed. A leaflet from Daybreak describing the TL technique in more detail and giving a bibliography will be provided to interested persons. The phenomenon of thermoluminescence was first described by the English chemist Robert Boyle in It was employed in the ‘s as a method for radiation dose measurement, and soon was proposed for archaeological dating.

By the mid ‘s, its validity as an absolute dating technique was established by workers at Oxford and Birmingham in England, Riso in Denmark, and at the University of Pennsylvania in the U. While not so accurate as radiocarbon dating, which cannot date pottery except from soot deposits on cooking pots , TL has found considerable usefulness in the authenticity of ceramic art objects where high precision is not necessary.

Since the university laboratories involved with TL are research facilities, they generally will not accept art objects for authentication on a routine basis. The TL laboratory at Daybreak was established in to make TL available to the art community in general.

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