Effects of feldspar contamination on equivalent dose and the shape of growth curve for OSL of silt-sized quartz extracted from Chinese loess

被引:110
作者
Lai, Zhongping [1 ,2 ]
Brueckner, Helmut [2 ]
机构
[1] Chinese Acad Sci, Qinghai Inst Salt Lakes, Luminescence Dating Lab, Xining 810008, Peoples R China
[2] Univ Marburg, Fac Geog, D-35032 Marburg, Germany
来源
GEOCHRONOMETRIA | 2008年 / 30卷
关键词
BLSL; IRSL; equivalent dose; Chinese loess; quartz luminescence; feldspar luminescence;
D O I
10.2478/v10003-008-0010-0
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
This study examines the effects of feldspar contamination of different extent (by fluorosilicic acid etching for different time periods and mixing pure quartz with different percentage of un-etched grains) on blue-light stimulated luminescence (BLSL) of quartz (38-63 mu m) for Chinese loess. In particular, the D-e values and the shape of growth curves will be examined. The results show that: (1) The D-e determined using feldspar in Chinese loess is obviously underestimated, and infra-red stimulated luminescence (IRSL) has a greater underestimation than BLSL. For aliquots with no fluorosilicic acid etching, an IRSL D-e underestimation of similar to 30% is observed for a sample with an expected age of similar to 22 ka, similar to 19% underestimation for BLSL, and similar to 10% for post-IR BLSL. For quartz BLSL, the contamination of feldspar, which has not dissolved by fluorosilicic acid etching, will inevitably lead to age underestimation. We suggest that the IR-checking should be performed for every single aliquot. An aliquot should be excluded from the final D-e calculation if obvious IRSL signal was observed. (2) For the sample under examination blue LED stimulation can reset both IRSL and BLSL signals of feldspars, while IR stimulation cannot reset the BLSL of feldspars. (3) For multiple-mineral aliquot the growth curve shape of the post-IR BLSL is different from that of the IRSL, and within 25 Gy it is identical to that of the pure quartz BLSL. The contamination of feldspars in quartz will change the shape of a growth curve for quartz BLSL.
引用
收藏
页码:49 / 53
页数:5
相关论文
共 20 条
[1]   Equivalent dose estimation using a single aliquot of polymineral fine grains [J].
Banerjee, D ;
Murray, AS ;
Botter-Jensen, L ;
Lang, A .
RADIATION MEASUREMENTS, 2001, 33 (01) :73-94
[2]   Experiences with single-aliquot OSL procedures using coarse-grain feldspars [J].
Blair, MW ;
Yukihara, EG ;
McKeever, SWS .
RADIATION MEASUREMENTS, 2005, 39 (04) :361-374
[3]   Luminescence dating of old (>70 ka) Chinese loess:: A comparison of single-aliquot OSL and IRSL techniques [J].
Buylaert, J. P. ;
Vandenberghe, D. ;
Murray, A. S. ;
Huot, S. ;
De Corte, F. ;
Van den Haute, P. .
QUATERNARY GEOCHRONOLOGY, 2007, 2 (1-4) :9-14
[4]  
DULLER GAT, 1993, RADIAT PROT DOSIM, V47, P683
[5]   COMPARISON OF THE GREEN-STIMULATED AND INFRARED-STIMULATED LUMINESCENCE OF FELDSPAR [J].
GALLOWAY, RB .
RADIATION MEASUREMENTS, 1994, 23 (2-3) :617-620
[6]   Limits to depletion of blue-green light stimulated luminescence in feldspars: implications for quartz dating [J].
Jain, M ;
Singhvi, AK .
RADIATION MEASUREMENTS, 2001, 33 (06) :883-892
[7]   Spectral information from minerals relevant for luminescence dating [J].
Krbetschek, MR ;
Gotze, J ;
Dietrich, A ;
Trautmann, T .
RADIATION MEASUREMENTS, 1997, 27 (5-6) :695-748
[8]   Existence of a common growth curve for silt-sized quartz OSL of loess from different continents [J].
Lai, Zhong-Ping ;
Brueckner, Helmut ;
Zoeller, Ludwig ;
Fuelling, Alexander .
RADIATION MEASUREMENTS, 2007, 42 (09) :1432-1440
[9]   Locating the boundary between the Pleistocene and the Holocene in Chinese loess using luminescence [J].
Lai, Zhong-Ping ;
Wintle, Ann G. .
HOLOCENE, 2006, 16 (06) :893-899
[10]   Effects of thermal treatment on the growth curve shape for OSL of quartz extracted from Chinese loess [J].
Lai, ZhongPing ;
Brueckner, Helmut ;
Fuelling, Alexander ;
Zoeller, Ludwig .
RADIATION MEASUREMENTS, 2008, 43 (2-6) :763-766