Please use this identifier to cite or link to this item: http://hdl.handle.net/20.500.12136/667
Item metadata
Title: Dose response curve of the ESR signal of the Aluminum center in quartz grains extracted from sediment
Authors: Duval, Mathieu
Issue Date: Dec-2012
Publisher: East Carolina University, Luminescence Dosimetry Laboratory
Citation: Ancient TL, 2012, 30 (2), 41-49
Abstract: A single saturating exponential (SSE) function is classically used in ESR dating to fit the experimental ESR data points derived from the aluminum (Al) center in quartz. However, this function has some obvious limits as it does not accurately fit the data points of the dose response curve. This results in unreliable equivalent dose (DE) values which are highly dependent on the maximum irradiation dose. Dose response curves of Al center in quartz show that the dose response data contain at least two components: a first one dominating at low dose (usually < 5 kGy) and saturating quite quickly and a second one dominating at higher doses with an almost linear behavior. These data are more appropriately fitted with a function combining an exponential with a linear term (EXP+LIN). Two variations of the EXP+LIN function were studied, each one corresponding to distinct physical assumptions. Since it is still unclear which one should be preferred, the mean DE value extracted from the fitting of the two equations may be reasonably considered as the most reliable estimate of the true DE value. In addition, to ensure accurate fitting of the linear part, it is important to have at least three data points at high doses (>10 kGy). It is also suggested to pool all the ESR intensities derived from repeated ESR measurements of each aliquot in the fitting process, in order to reduce the error in the DE value.
URI: http://hdl.handle.net/20.500.12136/667
ISSN: 0735-1348
metadata.dc.relation.publisherversion: http://www.ecu.edu/cs-cas/physics/ancient-timeline/ATL30.cfm
Type: Article
Appears in Collections:Geocronología y Geología



Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.