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The effect of single grain luminescence characteristics on single aliquot equivalent dose estimates
Institution:1. Institut für Geologie und Paläontologie, Westfälische Wilhelms-Universität Münster, Corrensstraße 24, 48149 Münster, Germany;2. Leibniz Institute for Applied Geophysics (LIAG), Geochronology & Isotope Hydrology, Stilleweg 2, 30655 Hannover, Germany;3. Institute of Tibetan Plateau Research, Chinese Academy of Sciences, 4A Datun Road, Chaoyang District, Beijing 100101, China;1. Department of Geology and Lithosphere Protection, Faculty of Earth Sciences and Spatial Management, Maria Curie-Skłodowska University, Aleja Kraśnicka 2 CD, 20-718 Lublin, Poland;2. Department of Soil Science and Soil Protection, Faculty of Earth Sciences and Spatial Management, Maria Curie-Skłodowska University, Aleja Kraśnicka 2 CD, 20-718 Lublin, Poland;3. Department of Geoecology and Palaeogeography, Faculty of Earth Sciences and Spatial Management, Maria Curie-Skłodowska University, Aleja Kraśnicka 2 CD, 20-718 Lublin, Poland;4. Department of Engineering Geology, Institute of Hydrogeology and Engineering Geology, Faculty of Geology, University of Warsaw, Żwirki i Wigury 93, 02-089 Warsaw, Poland
Abstract:We report an investigation of the effect of different single grain OSL behaviours on multiple-grain (single aliquot) De estimates. This was done by creating ‘synthetic aliquots’ in which signals are summed from collections of individual grains. The samples used were taken from aeolian linear dune sediments, from sites located in the Kalahari. We note this is a type of sample for which single multiple-grain aliquots are routinely used for dating. Several grain behavioural types were identified in our samples but the only grain type that systematically affected multiple-grain De estimates was the ‘over-saturating’ type (the case where the natural signal (Ln/Tn) is significantly greater than the regenerated Lx/Tx signal at saturation), the presence of which lead to higher estimates of De. The magnitude of this effect is controlled by the contribution of ‘over-saturating’ grains to the total light sum of the multiple-grain aliquot and the maximum increase observed in this study was ∼15 Gy. Of the four samples investigated here, inter-aliquot variations in the signal contribution of ‘over-saturating’ grains led to a significant increase in dispersion in just one of the samples. More generally, the presence/absence of these grains is considered to be a likely source of significant ‘intrinsic’ scatter in single aliquot dating and likely to broaden multiple-grain De distributions. We suggest all samples are screened for this behaviour before single aliquot dating is attempted.
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