Published October 2014 | Version v1
Journal article

The a-value of polymineral fine grain samples measured with the post-IR IRSL protocol

  • 1. Geographical Institute, Geomorphology, University of Bayreuth, 95440 Bayreuth (Germany)
  • 2. Department of Geography, Justus-Liebig-University Giessen, 35390 Giessen (Germany)
  • 3. IRAMAT-CRP2A, Université Bordeaux Montaigne, Maison de l'Archéologie, Esplanade des Antilles, 33607 Pessac Cedex (France)
  • 4. Institute for Geography, University of Cologne, 50923 Cologne (Germany)
  • 5. Department of Physics, East Carolina University, NC 27858 Greenville (United States)

Description

Recent post-IR IRSL (pIRIR) dating studies using polymineral fine grains assumed that the a-values obtained for the IRSL signal at 50 °C and the pIRIR signal at higher temperatures (e.g. 225 °C) are identical. However, the a-value of a sample depends on the stimulation method, and the assumption mentioned above remains to be tested. Using five polymineral fine grain samples, this study investigates whether a common a-value can be used for both the IR and the pIRIR signals. Applying the pIRIR protocol, the a-values were measured with three different methods of signal resetting (optical bleaching, end of SAR cycle, heating). In addition, uncorrected α- and β-irradiation induced growth curves were determined for three samples and fitted with single saturating exponential functions. For the investigated samples we found significant mean differences, 0.023 ± 0.012 and higher, in the a-values determined for the IR50 and pIRIR225 signals. Synthetic a-values deduced from uncorrected multiple-aliquot dose response curves seem to confirm this observation. Although, in summary, our results indicate that the practice of using a common a-value should be carefully re-considered, the physical reasons remain to be determined. - Highlights: • Measurement of the a-value on polymineral fine grain using the pIRIR protocol. • Mean a-value differs for the IR50 and pIRIR225 signal. • We observe a dependency of the a-value on the method of signal resetting. • a-values appear to be dose dependent. • It seems not appropriate to use identical a-values for IR50 and pIRIR225

Availability note (English)

Available from http://dx.doi.org/10.1016/j.radmeas.2014.04.027

Additional details

Identifiers

DOI
10.1016/j.radmeas.2014.04.027;
PII
S1350-4487(14)00184-X;

Publishing Information

Journal Title
Radiation Measurements
Journal Volume
68
Journal Page Range
p. 18-29
ISSN
1350-4487
CODEN
RMEAEP

INIS

Country of Publication
United Kingdom
Country of Input or Organization
International Atomic Energy Agency (IAEA)
INIS RN
46127881
Subject category
S37: INORGANIC, ORGANIC, PHYSICAL AND ANALYTICAL CHEMISTRY; S61: RADIATION PROTECTION AND DOSIMETRY;
Descriptors DEI
AGE ESTIMATION; BLEACHING; EFFICIENCY; IRRADIATION; LUMINESCENCE; MINERALS; TEMPERATURE RANGE 0400-1000 K
Descriptors DEC
EMISSION; PHOTON EMISSION; TEMPERATURE RANGE

Optional Information

Copyright
Copyright (c) 2014 Elsevier Science B.V., Amsterdam, The Netherlands, All rights reserved.