2021 Vol. 41, No. 1
Article Contents

LI Dongxue, LIU Nannan, YANG Shengli, LIU Weiming, CHENG Ting, LIU Li, LUO Yuanlong. Application of quartz OSL standardized growth curve for De determination in loess on the eastern Tibetan Plateau[J]. Quaternary Sciences, 2021, 41(1): 111-122. doi: 10.11928/j.issn.1001-7410.2021.01.10
Citation: LI Dongxue, LIU Nannan, YANG Shengli, LIU Weiming, CHENG Ting, LIU Li, LUO Yuanlong. Application of quartz OSL standardized growth curve for De determination in loess on the eastern Tibetan Plateau[J]. Quaternary Sciences, 2021, 41(1): 111-122. doi: 10.11928/j.issn.1001-7410.2021.01.10

Application of quartz OSL standardized growth curve for De determination in loess on the eastern Tibetan Plateau

  • Fund Project:

    国家自然科学基金项目(批准号:41877447和41472147)和科技部第二次青藏高原综合考察研究项目(批准号:2019QZKK0602)共同资助

More Information
  • The quartz OSL standardized growth curve(SGC) method has the potential to greatly save laboratory time in high-resolution dating for loess sequences. However, there is still controversial about its applicability on different temporal and spatial scales. In this study, we selected two typical loess sections at Maerkang(31°54'40.84″N, 102°11'44.34″E; 2666 m a.s.l.) and Zhouqü(33°46'44. 4″N, 104°23'56. 4″E; 2047 m a.s.l.) in the eastern Tibetan Plateau. The thicknesses of the two loess profiles are 5.1 m and 12 m, respectively. 5 OSL dating samples were collected from each location. The characteristics of quartz OSL growth curve were systematically analyzed to examine the applicability of the SGC method and least square normalized growth curve(LS-SGC) method for determining the equivalent dose(De) of quartz grains from the loess in the study region.

    Our results show that: (1)The quartz OSL signals of the loess at the eastern Tibetan Plateau are dominated by the fast component, which are suitable for De measurement by single aliquot regenerative dose(SAR) method. The growth curve shapes of different samples and different aliquots indicated that a common quartz OSL growth curve exists in the study region. The quartz growth curves of different samples from Zhouqü and Markang were consistent within 100 Gy, and distinct deviations in the SGC curves were observed over 100 Gy for different sections. The SGC fitting curves of Zhouqü, Markang and total samples showed different growing trends; (2)The comparison of the Des determined by SGC, LS-SGC and SAR protocol showed that the LS-SGC method could get better results than the SGC method, with smaller residual sum of squares and less errors. The Des obtained by the two methods for the same sample was in good agreement with the SAR De values. The De values obtained by the central age model and the minimum age model indicated that the Des determined by SGC, LS-SGC and SAR methods for each sample were consistent within the 10%error; (3)For all loess samples, the De determined by SGC and LS-SGC agreed well with the SAR De value within 0~100 Gy, and both methods can be used to estimate the equivalent dose. Beyond this range, there is a large deviation for SGC results. Whereas, LS-SGC method resulted in better De estimations than the SGC method for loess samples with 100~200 Gy.

    This study would not only facilitate the applications of quartz OSL dating of loess deposits and better investigating aeolian processes in the eastern Tibetan Plateau, but also deepen our understanding of quartz OSL SGC method.

  • 加载中
  • [1]

    赖忠平.基于光释光测年的中国黄土中氧同位素阶段2/1和3/2界限位置及年代的确定[J].第四纪研究, 2008, 28(5):883-891. doi: 10.3321/j.issn:1001-7410.2008.05.011

    Lai Zhongping. Locating and dating the boundaries of MIS2/1 and 3/2 in Chinese loess using luminescence techniques[J]. Quaternary Sciences, 2008, 28(5):883-891. doi: 10.3321/j.issn:1001-7410.2008.05.011

    [2]

    Buylaert J P, Murray A S, Thomsen K J, et al. Testing the potential of an elevated temperature IRSL signal from K-feldspar[J]. Radiation Measurements, 2009, 44(5-6):560-565. doi: 10.1016/j.radmeas.2009.02.007

    [3]

    Li B, Li S H. Luminescence dating of Chinese loess beyond 130 ka using the non-fading signal from K-feldspar[J]. Quaternary Geochronology, 2012, 10(7):24-31. doi: 10.1016/j.quageo.2011.12.005

    [4]

    Kang S G. A high-resolution quartz OSL chronology of the Talede loess over the past 30 ka and its implications for dust accumulation in the Ili Basin, Central Asia[J]. Quaternary Geochronology, 2015, 30:181-187. https://doi.org/10.1016/j.quageo.2015.04.006. doi: 10.1016/j.quageo.2015.04.006

    [5]

    Wintle A G, Adamiec G. Optically stimulated luminescence signals from quartz:A review[J]. Radiation Measurements, 2017, 98:10-33. https://doi.org/10.1016/j.radmeas.2017.02.003. doi: 10.1016/j.radmeas.2017.02.003

    [6]

    Perić Z, Adolphi E L, Stevens T, et al. Quartz OSL dating of Late Quaternary Chinese and Serbian loess:A cross Eurasian comparison of dust mass accumulation rates[J]. Quaternary International, 2018, 502:30-44. https://doi.org/10.1016/j.quaint.2018.01.010. doi: 10.1016/j.quaint.2018.01.010

    [7]

    Duller G A T. Equivalent dose determination using single aliquots[J]. International Journal of Radiation Applications & Instrumentation Part D:Nuclear Tracks & Radiation Measurements, 1991, 18(91):371-378. doi: 10.1016/1359-0189(91)90002-Y

    [8]

    Murray A S, Roberts R G. Measurement of equivalent dose in quartz using a regenerative-dose single-aliquot protocol[J]. Radiation Measurements, 1998, 29(5):503-515. doi: 10.1016/S1350-4487(98)00044-4

    [9]

    Murray A S, Wintle A G. Luminescence dating of quartz using an improved single-aliquot regenerative-dose protocol[J]. Radiation Measurements, 2000, 32(1):57-73. doi: 10.1016/S1350-4487(99)00253-X

    [10]

    鹿化煜, 周亚利, Mason J, 等.中国北方晚第四纪气候变化的沙漠与黄土记录-以光释光年代为基础的直接对比[J].第四纪研究, 2006, 26(6):888-894. doi: 10.3321/j.issn:1001-7410.2006.06.002

    Lu Huayu, Zhou Yali, Mason J, et al. Late Quaternary climatic changes in Northern China-New evidence from sand dune and loess records based on optically stimulated luminescence dating[J]. Quaternary Sciences, 2006, 26(6):888-894. doi: 10.3321/j.issn:1001-7410.2006.06.002

    [11]

    Lu Y C, Wang X L, Wintle A G. A new OSL chronology for dust accumulation in the last 130, 000 yr for the Chinese Loess Plateau[J]. Quaternary Research, 2007, 67(1):152-160. doi: 10.1016/j.yqres.2006.08.003

    [12]

    李国强, 陶淑娴, 佘琳琳, 等.阿拉善高原古湖岸堤释光测年与晚第四纪湖面变化[J].第四纪研究, 2019, 39(4):803-811.

    Li Guoqiang, Tao Shuxian, She Linlin, et al. Optically stimulated luminescence dating of paleoshorelines revealed Late Quaternary lake evolution in Alxa Plateau[J]. Quaternary Sciences, 2019, 39(4):803-811.

    [13]

    楚纯洁, 赵景波, 周金风.毛乌素沙地中部黄土-古土壤剖面沉积特征与地层划分[J].第四纪研究, 2018, 38(3):623-635.

    Chu Chunjie, Zhao Jingbo, Zhou Jinfeng. Sedimentary characteristics and stratigraphic division of the loess-paleosol section in Wushen County, the central Mu Us dune field in North China[J]. Quaternary Sciences, 2018, 38(3):623-635.

    [14]

    Ou X J, Xu L B, Lai Z P, et al. Potential of quartz OSL dating on moraine deposits from eastern Tibetan Plateau using SAR protocol[J]. Quaternary Geochronology, 2010, 5(2-3):257-262. doi: 10.1016/j.quageo.2009.02.004

    [15]

    Lai Z P, Zhang W G, Chen X, et al. OSL chronology of loess deposits in East China and its implications for East Asian monsoon history[J]. Quaternary Geochronology, 2010, 5(2-3):154-158. doi: 10.1016/j.quageo.2009.02.006

    [16]

    Kang S G, Wang X L, Lu Y C. Quartz OSL chronology and dust accumulation rate changes since the last glacial at Weinan on the southeastern Chinese Loess Plateau[J]. Boreas, 2013, 42(4):815-829. doi: 10.1111/bor.12005

    [17]

    Thomsen K J, Murray A S, Buylaert J P, et al. Testing single-grain quartz OSL methods using sediment samples with independent age control from the Bordes-Fitte rockshelter (Roches d'Abilly site, Central France)[J]. Quaternary Geochronology, 2016, 31:77-96. https://doi.org/10.1016/j.quageo.2015.11.002. doi: 10.1016/j.quageo.2015.11.002

    [18]

    Li B, Jacobs Z, Roberts R G. Investigation of the applicability of standardised growth curves for OSL dating of quartz from Haua Fteah Cave, Libya[J]. Quaternary Geochronology, 2016, 35:1-15. https://doi.org/10.1016/j.quageo.2016.05.001. doi: 10.1016/j.quageo.2016.05.001

    [19]

    刘向军, 赖忠平, Madsen David B, 等.晚第四纪青海湖高湖面研究[J].第四纪研究, 2018, 38(5):1166-1178.

    Liu Xiangjun, Lai Zhongping, Madsen David B, et al. Late Quaternary highstands of Qinghai Lake, Qinghai-Tibetan Plateau[J]. Quaternary Sciences, 2018, 38(5):1166-1178.

    [20]

    年小美, 张卫国.光释光技术在我国海岸晚第四纪沉积测年中的应用[J].第四纪研究, 2018, 38(3):573-586.

    Nian Xiaomei, Zhang Weiguo. Application of optically stimulated luminescence dating to Late Quaternary coastal deposits in China[J]. Quaternary Sciences, 2018, 38(3):573-586.

    [21]

    颜燕燕, 张家富, 胡钢, 等.晋陕峡谷基座阶地沉积物释光测年方法的比较研究[J].第四纪研究, 2018, 38(3):594-610.

    Yan Yanyan, Zhang Jiafu, Hu Gang, et al. Comparison of various luminescence dating procedures on sediments from one of the strath terraces of the Yellow River in the Jinshaan Canyon[J]. Quaternary Sciences, 2018, 38(3):594-610.

    [22]

    张博譞, 陈杰, 覃金堂, 等.帕米尔高原瓦恰盆地黄土的石英光释光测年[J].第四纪研究, 2018, 38(3):636-645.

    Zhang Boxuan, Chen Jie, Qin Jintang, et al. Quartz optically stimulated luminescence dating of loess from Waqia Basin in the Pamir Plateau[J]. Quaternary Sciences, 2018, 38(3):636-645.

    [23]

    Murray A S, Wintle A G. The single aliquot regenerative dose protocol:Potential for improvements in reliability[J]. Radiation Measurements, 2003, 37(4-5):377-381. doi: 10.1016/S1350-4487(03)00053-2

    [24]

    Wintle A G, Murray A S. A review of quartz optically stimulated luminescence characteristics and their relevance in single-aliquot regeneration dating protocols[J]. Radiation Measurements, 2006, 41(4):369-391. doi: 10.1016/j.radmeas.2005.11.001

    [25]

    Roberts H M, Duller G A T. Standardised growth curves for optical dating of sediment using multiple-grain aliquots[J]. Radiation Measuremnts, 2004, 38(2):241-252. doi: 10.1016/j.radmeas.2003.10.001

    [26]

    Burbidge C I, Duller G A T, Roberts H M. De determination for young samples using the standardised OSL response of coarse-grain quartz[J]. Radiation Measurements, 2006, 41(3):278-288. doi: 10.1016/j.radmeas.2005.06.038

    [27]

    Lai Z P. Testing the use of an OSL standardised growth curve (SGC) for De determination on quartz from the Chinese Loess Plateau[J]. Radiation Measurements, 2006, 41(1):9-16. doi: 10.1016/j.radmeas.2005.06.031

    [28]

    Lai Z P, Brückner H, Zöller L, et al. Existence of a common growth curve for silt-sized quartz OSL of loess from different contents[J]. Radiation Measurements, 2007, 42(9):1432-1440. doi: 10.1016/j.radmeas.2007.08.006

    [29]

    杨传成, 陈杰, 张克旗, 等.水成相沉积物细颗粒石英光释光综合生长曲线的建立与应用[J].地震地质, 2007, 29(2):402-411. doi: 10.3969/j.issn.0253-4967.2007.02.018

    Yang Chuancheng, Chen Jie, Zhang Keqi, et al. Standardized growth curve (SGC) for optically dating of fine-grain quartz from water-land sediments[J]. Seismology and Geology, 2007, 29(2):402-411. doi: 10.3969/j.issn.0253-4967.2007.02.018

    [30]

    Long H, Lai Z P, Fan Q S, et al. Applicability of a quartz OSL standardised growth curve for De determination up to 400 Gy for lacustrine sediments from the Qaidam Basin of the Qinghai-Tibetan Plateau[J]. Quaternary Geochronology, 2010, 5(2-3):212-217. doi: 10.1016/j.quageo.2009.05.005

    [31]

    Kang S G, Wang X L, Lu Y C. The estimation of basic experimental parameters in the fine-grained quartz multiple-aliquot regenerative-dose OSL dating of Chinese loess[J]. Radiation Measurements, 2012, 47(9):674-681. doi: 10.1016/j.radmeas.2012.01.009

    [32]

    Shen Z, Mauz B. Estimating the equivalent dose of Late Pleistocene fine silt quartz from the lower Mississippi Valley using a standardized OSL growth curve[J]. Radiation Measurements, 2011, 46(8):649-654. doi: 10.1016/j.radmeas.2011.05.060

    [33]

    Chen G Q, Yi L, Xu X Y, et al. Testing the standardized growth curve (SGC) to OSL dating:Coastal sediments from the south Bohai Sea, China[J]. Geochronometria, 2013, 40(2):101-112. doi: 10.2478/s13386-013-0103-z

    [34]

    Yang L H, Lai Z P, Long H et al. Construction of a quartz OSL standardised growth curve (SGC) for aeolian samples from the Horqin dune field in Northeastern China[J]. Geochronometria, 2013, 38(4):391-396. doi: 10.2478/s13386-011-0045-2

    [35]

    Stevens T, Simon J A, Lu H Y, et al. Examining the potential of high sampling resolution OSL dating of Chinese loess[J]. Quaternary Geochronology, 2007, 2(1-4):15-22. doi: 10.1016/j.quageo.2006.03.004

    [36]

    Telfer M W, Bateman M D, Carr A S, et al. Testing the applicability of a standardized growth curve (SGC) for quartz OSL dating:Kalahari dunes, South African coastal dunes and Florida dune cordons[J]. Quaternary Geochronology, 2008, 3(1/2):137-142. doi: 10.1016/j.quageo.2007.08.001

    [37]

    赖忠平, 欧先交.光释光测年基本流程[J].地理科学进展, 2013, 32(5):683-693.

    Lai Zhongping, Ou Xianjiao. Basic procedures of optically stimulated luminescence (OSL) dating[J]. Progress in Geography, 2013, 32(5):683-693.

    [38]

    E C Y, Lai Z P, Sun Y J, et al. A luminescence dating study of loess deposits from the Yili River basin in Western China[J]. Quaternary Geochronology, 2012, 10(3):50-55. doi: 10.1016/j.quageo.2012.04.022

    [39]

    Jia Y L, Lai Z P, Zhang J R, et al. Chronology and provenance of aeolian sediments from Poyang Lake area in the middle reaches of the Yangtze River in China[J]. Quaternary Geochronology, 2012, 10(3):44-49. doi: 10.1016/j.quageo.2012.01.011

    [40]

    Liu X J, Lai Z P, Madsen D, et al. Lake level variations of Qinghai Lake in northeastern Qinghai-Tibetan Plateau since 3.7 ka based on OSL dating[J]. Quaternary International, 2012, 236(1-2):57-64. doi: 10.1016/j.quaint.2010.08.009

    [41]

    Lai Z P, Bruckner H. Effects of feldspar contamination on equivalent dose and the shape of growth curve for OSL of silt-sized quartz extracted from Chinese loess[J]. Geochronometria, 2008, 30(1):49-53. doi: 10.2478/v10003-008-0010-0

    [42]

    Lai Z P, Bruckner H, Fulling A, et al. Effects of thermal treatment on the growth curve shape for OSL of quartz extracted from Chinese loess[J]. Radiation Measurements, 2008, 43(2-6):763-766. doi: 10.1016/j.radmeas.2008.01.023

    [43]

    刘瑞元.光释光测年中应用标准曲线法(SGC)求等效剂量(De)计算方法的一种改进研究[D].北京: 中国科学院大学硕士学位论文, 2013: 1-65.

    Liu Ruiyuan. Improvement Mathematics for Equivalent dose (De) Calculation Use the Standardized Growth Curve (SGC) in Optically Stimulated Luminescence Dating[D]. Beijing: The Master's Dissertation of University of Chinese Academy of Sciences, 2013: 1-65.

    [44]

    Li B, Roberts R G, Jacobs Z, et al. Potential of establishing a'global standardised growth curve'(gSGC) for optical dating of quartz from sediments[J]. Quaternary Geochronology, 2015, 27:94-104. https://doi.org/10.1016/j.quageo.2015.02.011. doi: 10.1016/j.quageo.2015.02.011

    [45]

    罗来兴, 杨逸畴.川西滇北地貌形成的探讨[J].地理集刊, 1963, 5:1-23.

    Luo Laixing, Yang Yichou. Discussion of formation of the landform in the in western Sichuan and northern Yunnan[J]. Collected Works of Geography, 1963, 5:1-23.

    [46]

    柴宗新.川西高原的黄土[C]//中国第四纪研究委员会.第三届全国第四纪学术会议论文集.北京: 科学出版社, 1982: 273-274.

    Chai Zongxin. Loess in west Sichuan Plateau[C]//Chinese Society of Quaternary Sciences. The Collection of Third Academic Session Papers. Beijing: Science Press, 1982: 273-274.

    [47]

    陈富斌, 高生淮, 陈继良, 等.甘孜黄土剖面磁性地层初步研究[J].科学通报, 1990, 35(20):1600.

    Chen Fubin, Gao Shenghuai, Chen Jiliang, et al. Preliminary study on magnetic stratigraphy in the Ganzi Loess section[J]. Chinese Science Bulletin, 1990, 35(20):1600.

    [48]

    方小敏, 陈富斌, 施雅风, 等.甘孜黄土与青藏高原冰冻圈演化[J].科学通报, 1996, 41(20):1865-1867. doi: 10.3321/j.issn:0023-074X.1996.20.013

    Fang Xiaomin, Chen Fubin, Shi Yafeng, et al. Evolution of the Ganzi loess and the cryosphere of the Tibetan Plateau[J]. Chinese Science Bulletin, 1996, 41(20):1865-1867. doi: 10.3321/j.issn:0023-074X.1996.20.013

    [49]

    郭飞, 王婷, 刘宇明, 等.临夏黄土记录的26万年来季风快速变化[J].第四纪研究, 2019, 39(3):557-564.

    Guo Fei, Wang Ting, Liu Yuming, et al. Rapid Asian monsoon changes recorded by loess depositions in Linxia since 260 ka B.P.[J]. Quaternary Sciences, 2019, 39(3):557-564.

    [50]

    马兴悦, 吕镔, 赵国永, 等.川西高原理县黄土磁学特征及其影响因素[J].第四纪研究, 2019, 39(5):1307-1319.

    Ma Xingyue, Lü Bin, Zhao Guoyong, et al. Magnetic properties and their influence factors of Lixian loess in western Sichuan Plateau[J]. Quaternary Sciences, 2019, 39(5):1307-1319.

    [51]

    任少芳, 郑祥民, 周立旻, 等.基于光释光测年的东海嵊山岛风尘黄土环境敏感粒度组分研究[J].第四纪研究, 2018, 38(3):646-658.

    Ren Shaofang, Zheng Xiangmin, Zhou Limin, et al. Analysis of environmentally sensitive grain-size component of loess on the Shengshan Island in East China Sea based on optically stimulated luminescence dating[J]. Quaternary Sciences, 2018, 38(3):646-658.

    [52]

    蒋凯, 王喜生, 盛美.浑善达克沙地南缘晚更新世黄土-古土壤序列的高分辨率磁性气候记录[J].第四纪研究, 2019, 39(3):565-578.

    Jiang Kai, Wang Xisheng, Sheng Mei. Magnetoclimatological patterns of a Late Pleistocene loess-paleosol sequence in the southern Hunshandake Sandy Land[J]. Quaternary Sciences, 2019, 39(3):565-578.

    [53]

    张克旗.甘孜黄土细颗粒石英光释光测年初步研究[J].核技术, 2012, 35(12):916-922.

    Zhang Keqi. A preliminary discussion on measurements of SMAR equivalent dose of fine-grain quartz extracted from Ganzi loess[J]. Radiation Measurements, 2012, 35(12):916-922.

    [54]

    刘楠楠, 杨胜利, 刘维明, 等.青藏高原东缘黄土石英光释光信号积分区间选择[J].地球环境学报, 2018, 9(6):569-579.

    Liu Nannan, Yang Shengli, Liu Weiming, et al. Selection of integration time intervals for quartz optically stimulated luminescene (OSL) of loess in the eastern Tibetan Plateau[J]. Journal of Earth Environment, 2018, 9(6):569-579.

    [55]

    Lehmkuhl F, Schulte P, Zhao H, et al. Timing and spatial distribution of loess and loess-like sediments in the mountain areas of the northeastern Tibetan Plateau[J]. Catena, 2014, 117:23-33. https://doi.org/10.1016/j.catena.2013.06.008. doi: 10.1016/j.catena.2013.06.008

    [56]

    Duller G A T. Distinguishing quartz and feldspar in single grain luminescence measurements[J]. Radiation Measurements, 2003, 37(2):161-165. doi: 10.1016/S1350-4487(02)00170-1

    [57]

    Peng J, Li B. Single-aliquot regenerative-dose (SAR) and standardized growth curve (SGC) equivalent dose determination in a batch model using the R Package 'numOSL'[J]. Ancient TL, 2017, 35(2):32-53.

    [58]

    邹乐强.最小二乘法原理及其简单应用[J].科技信息, 2010, (23):282-283.

    Zou Leqiang. The principle of least square method and its simple application[J]. Science & Technology Information, 2010, (23):282-283.

    [59]

    田生昌.最小二乘法的统计学原理及在农业试验分析中的应用[J].数学的实践与认识, 2015, 45(4):124-133.

    Tian Shengchang. The least squares method of statistical principles and applications in agricultural pilot study[J]. Journal of Mathematics in Practice and Theory, 2015, 45(4):124-133.

    [60]

    Galbraith R F, Roberts R G, Laslett G M, et al. Optical dating of single and multiple grains of quartz from jinmium rock shelter, Northern Australia, part 1, Experimental design and statistical models[J]. Archaeometry, 2010, 41(2):339-364. doi: 10.1111/j.1475-4754.1999.tb00987.x

  • 加载中
通讯作者: 陈斌, bchen63@163.com
  • 1. 

    沈阳化工大学材料科学与工程学院 沈阳 110142

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索

Figures(9)

Article Metrics

Article views(396) PDF downloads(65) Cited by(0)

Access History

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint