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Investigating the contribution of recuperated TL to post-IR IRSL signals in a perthitic feldspar
Affiliation:1. Illinois State Geological Survey, Prairie Research Institute, University of Illinois at Champaign-Urbana, Champaign, IL 61820, USA;2. School of Natural Resources, University of Nebraska-Lincoln, Lincoln, NE 68583, USA;3. Department of Geography, University of Wisconsin-Madison, Madison, WI 53706, USA;4. State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi''an 710075, China
Abstract:Using a museum specimen of perthitic feldspar, the characteristics of post-IR IRSL production at 200 °C after different prior IR bleaching at 100 °C were investigated. It was found that the post-IR IRSL signal had an isothermal TL contribution that was unexpected following a previous preheat at 320 °C; this is the result of isothermal decay of recuperated TL peaks resulting from photo-transfer that occurred when the previous IRSL signal was measured at a lower temperature. The isothermal TL contribution to the post-IR IRSL signal depends on prior IR bleaching conditions. Since the recuperated TL signal comes from photo-transfer during IRSL production, this signal should also suffer from anomalous fading. Thus, it is suggested that this isothermal TL contribution to the measured post-IR IRSL is removed by the inclusion of an additional step, a cut-heat to 300 °C, in the post-IR IRSL dating protocol.
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