TY - JOUR
T1 - Variability of infrared stimulated luminescence properties from fractured feldspar grains
AU - Huot, S.
AU - Lamothe, M.
N1 - Funding Information:
This work was financially supported by ‘Fonds pour la Formation de Chercheurs et l'Aide á la Recherche, Québec (FCAR)’ and by NSERC (Canada). The University of Arizona and the National Science Foundation are acknowledged for the radiocarbon date. Marie Auclair and Dave Huntley have kindly reviewed an earlier version of the manuscript.
PY - 2003/8
Y1 - 2003/8
N2 - A series of OSL properties of fragments from split feldspar grains have been investigated. These are (1) the response to a radiation dose, (2) the recycling of corrected induced luminescence (Li/Ti), (3) the corrected natural luminescence (LN/TN), (4) the corrected thermal transfer luminescence (termed herein Ltt/Ttt) and, (5) the rate of anomalous fading ("g"). It was found that the parameters of different parts of the same grain are the same. The relative uncertainty, at the 2 sigma level, at which we can claim that the measured parameters are correlated, is generally less than 5% but is ca 40% for the anomalous fading rate due to measurement uncertainty. For young partially bleached sediments, the result is that one could use one fragment to evaluate the equivalent dose and another to assess the contribution of thermal transfer resulting from preheating the natural luminescence.
AB - A series of OSL properties of fragments from split feldspar grains have been investigated. These are (1) the response to a radiation dose, (2) the recycling of corrected induced luminescence (Li/Ti), (3) the corrected natural luminescence (LN/TN), (4) the corrected thermal transfer luminescence (termed herein Ltt/Ttt) and, (5) the rate of anomalous fading ("g"). It was found that the parameters of different parts of the same grain are the same. The relative uncertainty, at the 2 sigma level, at which we can claim that the measured parameters are correlated, is generally less than 5% but is ca 40% for the anomalous fading rate due to measurement uncertainty. For young partially bleached sediments, the result is that one could use one fragment to evaluate the equivalent dose and another to assess the contribution of thermal transfer resulting from preheating the natural luminescence.
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U2 - 10.1016/S1350-4487(03)00014-3
DO - 10.1016/S1350-4487(03)00014-3
M3 - Article
AN - SCOPUS:0038141914
SN - 1350-4487
VL - 37
SP - 499
EP - 503
JO - Radiation Measurements
JF - Radiation Measurements
IS - 4-5
ER -