Show simple item record M. en_US G. A. T. en_US A. G. en_US 2011-05-31T10:28:55Z 2011-05-31T10:28:55Z 2007-09 en_US
dc.identifier en_US
dc.identifier.citation Jain , M , Duller , G A T & Wintle , A G 2007 , ' Dose response, thermal stability and optical bleaching of the 310 degrees C isothermal TL signal in quartz ' Radiation Measurements , vol 42 , no. 8 , pp. 1285-1293 . , 10.1016/j.radmeas.2007.08.008 en_US
dc.identifier.other PURE: 162161 en_US
dc.identifier.other dspace: 2160/6820 en_US
dc.description.abstract Several characteristics of the isothermal thermoluminescence (ITL) signal from quartz grains held at 310 degrees C are investigated. The effect oil the TL signal of holding the quartz at this temperature for different periods of time is recorded. It is shown that the TL and ITL data cannot be explained by a single trap obeying non-first order kinetics. The pattern of TL signal loss implies that probably two TL peaks are removed, one by holding for similar to 5 s at 310 degrees C and the other by holding for 500 s. The ITL decay curves that result from holding the sample at 310 degrees C is analysed using the Sum of three first order decay functions, and these are termed fast, medium and slow ITL. Two signal integrals, 0-5 and 50-100s, are considered to be representative of the fast and medium ITL components. These are investigated with regard to their response to laboratory irradiation, thermal stability and the effects of optical bleaching. The (0-5s) signal shows all order of magnitude higher for saturation level with laboratory dose than the optically stimulated luminescence (OSL) signal, and has a thermal stability that is very sintilar to published values for the OSL or the 325 degrees C TL peak. Bleaching with a solar simulator reduces both parts of the ITL signal to a low, but non-zero level in a few thousand seconds. This result is supported by an equivalent dose estimate oil a modern river sample from Zambia of 11 +/- 2 Gy. This combination of low residual dose and high saturation level appears to be Suitable for dating samples that are demonstrated to be beyond the range of OSL dating. (c) 2007 Elsevier Ltd. All rights reserved. en_US
dc.format.extent 9 en_US
dc.relation.ispartof Radiation Measurements en_US
dc.subject BLUE en_US
dc.subject dosimetry en_US
dc.subject isothermal TL en_US
dc.subject RELEVANCE en_US
dc.subject thermoluminescence en_US
dc.subject OSL en_US
dc.subject RED TL en_US
dc.subject PEAK en_US
dc.subject quartz en_US
dc.subject optical sensitivity en_US
dc.subject PROTOCOL en_US
dc.subject kinetics en_US
dc.title Dose response, thermal stability and optical bleaching of the 310 degrees C isothermal TL signal in quartz en_US
dc.contributor.pbl Institute of Geography & Earth Sciences en_US
dc.contributor.pbl Quaternary Environmental Change Group en_US

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