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A measure is made of a natural signal which is then correlated with the saturating exponential growth curve. However, it is possible to identify saturated samples through measurement. Samples subjected to a high dose rate will become saturated more quickly, and fully saturated samples will not record the full duration of their burial history. 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. Consequently, samples analysed without consideration of their water content or using a low estimate of water content will return ages younger than samples corrected for this effect. With the assistance of Fugro UK we have developed a method for converting the measured water content to a time-averaged water content for each sample. Water Content Calibration Water within the soil has an attenuating effect on the ambient radiation. The point at which a sample becomes saturated depends on the dose rate of the sample. The quartz can be very fine grained c. Please contact us for more information. The total absorbed dose termed De, measured in units of Gy is measured using standard luminescence dating procedures Murray and Wintle, Requires precise measurement of sample water content and salinity.
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