Dose evaluation using multiple-aliquot quartz OSL: test of methods and a new protocol for improved accuracy and precision

被引:69
作者
Jain, M [1 ]
Botter-Jensen, L
Singhvi, AK
机构
[1] Univ Delhi, Dept Geol, Delhi 110007, India
[2] Riso Natl Lab, Dept NUK 201, DK-4000 Roskilde, Denmark
[3] Phys Res Lab, Ahmedabad 380009, Gujarat, India
关键词
quartz OSL; scatter; normalisation; equivalent dose;
D O I
10.1016/S1350-4487(02)00165-8
中图分类号
TL [原子能技术]; O571 [原子核物理学];
学科分类号
0827 ; 082701 ;
摘要
Multiple-aliquot quartz OSL dose-response curves often suffer from substantial variability in the luminescence output from identically treated aliquots (scatter) that leads to large uncertainties in the equivalent-dose estimates. In this study, normalisation and its bearing on the accuracy and precision of the equivalent-dose estimates is investigated. We conclude that the most commonly used procedure employing the natural OSL (natural normalisation), leads to both poor accuracy and poor precision in the equivalent-dose estimates as it is insensitive to possible dose-dependent and non-dose-dependent sensitivity changes during the pre-heat, and fundamental variability in the shapes of quartz OSL (blue-green or blue-light stimulated luminescence) decay forms. A new protocol using a combination of 'elevated temperature IR cleaning' (ETIR) and 'component-specific dose normalisation' (CSDN) has been developed. CSDN accounts for variability in the OSL decay forms and absorbs such sensitivity changes. A combination of ETIR and CSDN protocol increased palaeodose precision from +/-100% to +/-4% in quartz separates from the fluvially transported sands in the Thar desert. A comparison with palaeodose estimates from the single-aliquot-regeneration protocol (SAR) gave similar accuracy and precision, (C) 2002 Elsevier Science Ltd. All rights reserved.
引用
收藏
页码:67 / 80
页数:14
相关论文
共 35 条
[1]   OPTICAL DATING - RECUPERATION AFTER BLEACHING [J].
AITKEN, MJ ;
SMITH, BW .
QUATERNARY SCIENCE REVIEWS, 1988, 7 (3-4) :387-393
[2]   Partial bleaching and the decay form characteristics of quartz OSL [J].
Bailey, RM ;
Smith, BW ;
Rhodes, EJ .
RADIATION MEASUREMENTS, 1997, 27 (02) :123-136
[3]   Quartz thermoluminescence: Dose and dose-rate effects and their implications [J].
Chawla, S ;
Rao, TKG ;
Singhvi, AK .
RADIATION MEASUREMENTS, 1998, 29 (01) :53-63
[4]  
Dear W.A., 1992, INTRO ROCK FORMING M
[5]   Optical dating of single sand-sized grains of quartz: sources of variability [J].
Duller, GAT ;
Botter-Jensen, L ;
Murray, AS .
RADIATION MEASUREMENTS, 2000, 32 (5-6) :453-457
[6]   Lake Lewis basin, central Australia: environmental evolution and OSL chronology [J].
English, P ;
Spooner, NA ;
Chappell, J ;
Questiaux, DG ;
Hill, NG .
QUATERNARY INTERNATIONAL, 2001, 83-5 :81-101
[7]   Study of non-linear luminescence-dose growth curves for the estimation of paleodose in luminescence dating: Results of Monte Carlo simulations [J].
Felix, C ;
Singhvi, AK .
RADIATION MEASUREMENTS, 1997, 27 (04) :599-609
[8]   THE MECHANISM OF THERMOLUMINESCENCE IN AN AUSTRALIAN SEDIMENTARY QUARTZ [J].
FRANKLIN, AD ;
PRESCOTT, JR ;
SCHOLEFIELD, RB .
JOURNAL OF LUMINESCENCE, 1995, 63 (5-6) :317-326
[9]  
Galloway R., 1996, ANCIENT TL, V14, P1
[10]   Deep traps in quartz and their use for optical dating [J].
Huntley, DJ ;
Short, MA ;
Dunphy, K .
CANADIAN JOURNAL OF PHYSICS, 1996, 74 (3-4) :81-91