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Optically stimulated luminescence dating methods

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Optically stimulated luminescence

This article needs additional citations for verification. Please help improve this article by adding citations to reliable sources. Unsourced material may be challenged and removed. March Learn how and when to remove this template message In physics , optically stimulated luminescence OSL is a method for measuring doses from ionizing radiation. It is used in at least two applications: The ionizing radiation produces electron-hole pairs:

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Two types of procedures can be distinguished: However, their precision is restricted due to methodological limits the use of several aliquots to obtain only one equivalent dose, obtained by extrapolation of the natural signal on a curve derived from various laboratory doses. On the contrary, the regenerative procedures provide more precise ages as they make it possible to obtain by interpolation a similar number of equivalent dose measurements to aliquot measurements. It was recently developed for quartz grains Murray and Wintle, and and applied also to feldspars Wallinga et al. We consequently describe in the present paper its general principles and its application to the case-study samples LUM and LUM

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Optically stimulated luminescence is a method of determining the age of burial of quartz or feldspar bearing sediments based upon principles of radiation and excitation within crystal lattices, and stems from the fact that imperfections in a crystal lattice have the ability to store ionizing energy Aitken, ; Botter-Jensen et al. Radiation within sediments comes from alpha, beta, and gamma radiation emitted during the decay of U, U, Th, 40K, and 87Rb, and their daughter products, both within the mineral grains and in their surroundings Lian, , and from cosmic rays Figure 1. Under controlled laboratory conditions, assuming the sample was collected under light-restricted conditions, controlled exposure of the sample to photons yields a luminescence response the equivalent dose, De , the intensity of which is a function of the dose rate within the sediment, and the length of time the sample was exposed to the background radiation. In order to measure the age, two factors must be known; 1 the environmental dose rate, and 2 the laboratory dose of radiation that produces the same intensity of luminescence as did the environmental radiation dose the equivalent dose. Dividing the equivalent dose by the dose rate yields time. Samples for OSL analysis are typically collected from opaque core tubes aluminum or black pvc tubes that are pushed into the sediment using coring equipment vibracore, geoprobe, etc.

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Luminescence dating

How do we measure the radiation dose rate? OSL is used on glacial landforms that contain sand, such as sandur or sediments in glacial streams. The OSL signal is reset by exposure to sunlight, so the signal is reset to zero while the sand is being transported such as in a glacial meltwater stream.

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