Process_Description:
Infrared luminescence dating - A fully referenced description of this method appears in the supplement to Bender et al. (2022). All analyses performed at the Utah State University (USU) Luminescence Lab, North Logan, Utah. Samples are opened and processed under dim amber safelight conditions. Sample processing for feldspar infrared stimulated luminescence (IRSL) dating followed standard procedures involving sieving, HCl and bleach treatments, heavy liquid mineral density separation at 2.58 g per cubic cm with no HF pre-treatment to isolate the potassium-rich feldspar component of a narrow grain-size range, 75-250 microns. The lab follows the latest single-aliquot regenerative-dose (SAR) procedures for potassium feldspar dating in which the IRSL signal is measured at 50 degrees Celsius. SAR protocol includes tests for sensitivity correction and brackets the equivalent dose (DE) the sample received during burial by irradiating the sample at five different doses (below, at, and above the DE, plus a zero dose and a repeated dose to check for recuperation of the signal and sensitivity correction). The resultant DE data are fit with a saturating exponential curve. The IRSL age is calculated by correcting for fading (loss of signal with time) using the fading method of Auclair and others (2003) and the age correction model of Huntley and Lamothe (2001). The cumulative DE and age data are reported at 2-sigma error and were determined using the Central Age Model (CAM) or the Minimum Age Model (MAM), depending on the distribution of DE results and evidence for partial bleaching. For cases in which the samples have significant positive skew and overdispersion, ages are calculated based on the MAM. Dose-rate calculations were determined by chemical analysis of of the U, Th, K, and Rb content using ICP-MS and ICP-AES techniques by ALS Chemex in Elko, NV, using conversion factors from Guerin and others (2011). Internal grain beta dose rate was determined assuming 12.5%K and 400 ppm Rb attenuated to grain size (Mejdahl, 1979). Alpha contribution to dose rate determined using an efficiency factor, 'a-value', of 0.086 +/- 0.0009. The contribution of cosmic radiation to the dose rate was calculated using sample depth, elevation, and latitude and longitude. Dose rates are calculated based on water content, sediment chemistry, and cosmic contribution.
Process_Date: Unknown