Hostname: page-component-8448b6f56d-c47g7 Total loading time: 0 Render date: 2024-04-24T00:39:10.960Z Has data issue: false hasContentIssue false
  • English
  • Français

Measurement of 10Be Concentration of Modern Falling Dust in Northern China

Published online by Cambridge University Press:  18 July 2016

Feng Xian ,
Weijian Zhou ,
Xianghui Kong ,
Jun Jiang ,
Zhenkun Wu ,
Ning Chen  and
Guoqing Zhao
Feng Xian*
Affiliation:
State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, No. 10 Fenghui South Road, Hi-Tech Zone, Xi'an 710075, China Xi'an AMS Center, No. 99 Yanxiang Road, Yanta District, Xi'an 710052, China
Weijian Zhou
Affiliation:
State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, No. 10 Fenghui South Road, Hi-Tech Zone, Xi'an 710075, China Xi'an AMS Center, No. 99 Yanxiang Road, Yanta District, Xi'an 710052, China School of Human Settlements and Civil Engineering, Xi'an Jiaotong University, No. 26 Xianning West Road, Beilin District, Xi'an 710049, China
Xianghui Kong
Affiliation:
State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, No. 10 Fenghui South Road, Hi-Tech Zone, Xi'an 710075, China Xi'an AMS Center, No. 99 Yanxiang Road, Yanta District, Xi'an 710052, China
Jun Jiang
Affiliation:
Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, No. 26 Xinong Road, Yang Ling 712100, China
Zhenkun Wu
Affiliation:
State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, No. 10 Fenghui South Road, Hi-Tech Zone, Xi'an 710075, China Xi'an AMS Center, No. 99 Yanxiang Road, Yanta District, Xi'an 710052, China
Ning Chen
Affiliation:
State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, No. 10 Fenghui South Road, Hi-Tech Zone, Xi'an 710075, China Xi'an AMS Center, No. 99 Yanxiang Road, Yanta District, Xi'an 710052, China
Guoqing Zhao
Affiliation:
State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, No. 10 Fenghui South Road, Hi-Tech Zone, Xi'an 710075, China Xi'an AMS Center, No. 99 Yanxiang Road, Yanta District, Xi'an 710052, China
*
Corresponding author. Email: xianf@ieecas.cn.
Rights & Permissions [Opens in a new window]

Abstract

Core share and HTML view are not available for this content. However, as you have access to this content, a full PDF is available via the ‘Save PDF’ action button.

Paleoenvironmental and paleogeomagnetic tracing studies from Chinese loess 10Be have progressed in recent years (Zhou et al. 2007a,b, 2010). In this approach, 10Be flux determined from sediment concentration and accumulation rate may be used to recover information about paleomonsoon rainfall rates as well as past variations in the geomagnetic field strength. However, these methods require that a correction be made for residual undecayed 10Be in remobilized dust. To better understand the feature of the 10Be signals related to the remobilized dust, we report the first observational study on 10Be concentration of modern falling dust using the 3MV multi-element accelerator mass spectrometer (AMS) in the Xi'an AMS Center. Ten samples collected at Ansai observation station (109°19′E, 36°51′N) in northern China from May 2008 to June 2009 are measured along with 3 chemical blanks. The results clearly show that the 10Be content of modern falling dust is relatively uniform, with a mean value of 1.21 x 108 atoms/g, a measurement similar to that of Chinese loess (Zhou et al. 2007a) and to the value found in the study by Shen et al. (2009) on dust 10Be falling near Dingbian, China (1.25 ± 0.06 x 108 atoms/g). Despite the fact that modern dust flux is much higher in spring relative to summer in northern China, 10Be concentration in falling dust remains fairly constant. In addition, we find that dust 10Be concentration is roughly independent of the local precipitation changes. This feature might be considered as an analogue to improve our understanding on the fundamental information of the source component contained in loess 10Be records and its spatial/temporal distribution features.

Type
Articles
Information
Radiocarbon , Volume 54 , Issue 1 , 2012 , pp. 37 - 43
Copyright
Copyright © 2012 by the Arizona Board of Regents on behalf of the University of Arizona 

References

An, ZS, Liu, TS, Lu, YC, Porter, SC, Kukla, G, Wu, XH, Hua, YM. 1990. The long-term paleomonsoon variation recorded by the loess-paleosol sequence in Central China. Quaternary International 7–8:91–5.Google Scholar
An, ZS, Kukla, GJ, Porter, SC, Xiao, JL. 1991. Magnetic susceptibility evidence of monsoon variation on the Loess Plateau of central China during the last 130,000 years. Quaternary Research 36(1):29–36.CrossRefGoogle Scholar
Baumgartner, S, Beer, J, Wagner, G, Kubik, P, Suter, M, Raisbeck, GM, Yiou, F. 1997. 10Be and dust. Nuclear Instruments and Methods in Physics Research B 123(1–4):296–301.CrossRefGoogle Scholar
Beer, J, Shen, CD, Heller, F, Liu, TS, Bonani, G, Beate, D, Suter, M, Kubik, PW. 1993. 10Be and magnetic susceptibility in Chinese loess. Geophysical Research Letters 20(1):57–60.CrossRefGoogle Scholar
Frank, M. 2000. Comparison of cosmogenic radionuclide production and geomagnetic field intensity over the last 200,000 years. Philosophical Transactions of the Royal Society of London Series A 358(1768):1089–107.CrossRefGoogle Scholar
Gu, ZY, Lal, D, Southon, J, Caffee, MW, Guo, ZT, Chen, MY. 1996. Five million year 10Be record in Chinese loess and red-clay: climate and weathering relationships. Earth and Planetary Science Letters 144(1–2):273–87.CrossRefGoogle Scholar
Heller, F, Shen, CD, Beer, J, Liu, XM, Liu, TS, Bronger, A, Suter, M, Bonani, G. 1993. Quantitative estimates of pedogenic ferromagnetic mineral formation in Chinese loess and palaeoclimatic implications. Earth and Planetary Science Letters 114(2–3):385–90.CrossRefGoogle Scholar
Korschinek, G, Bergmaier, A, Faestermann, T, Gerstmann, UC, Knie, K, Rugel, G, Wallner, A, Dillmann, I, Dollinger, G, Lierse von Gostomskie, C, Kossert, K, Maiti, M, Poutivtsev, M, Remmert, A. 2010. A new value for the half-life of 10Be by heavy-ion elastic recoil detection and liquid scintillation counting. Nuclear Instruments and Methods in Physics Research B 268(2):187–91.CrossRefGoogle Scholar
Lal, D, Peters, B. 1967. Cosmic ray produced radioactivity on earth. In: Sittle, K, editor. Handbook of Physics. Volume 46/2. Berlin: Springer. p 551–612.Google Scholar
Liu, XD, Yin, ZY, Zhang, XY, Yang, XC. 2004. Analyses of the spring dust storm frequency of northern China in relation to antecedent and concurrent wind, precipitation, vegetation, and soil moisture conditions. Journal of Geophysical Research 109(D16):D16210, doi:10.1029/2004JD004615.CrossRefGoogle Scholar
McHargue, LR, Damon, PE. 1991. The global beryllium-10 cycle. Reviews of Geophysics 29(2):141–58.CrossRefGoogle Scholar
Shen, CD, Beer, J, Liu, TS, Oeschger, H, Bonani, G, Suter, M, Wölfli, W. 1992. 10Be in Chinese loess. Earth and Planetary Science Letters 109(1–2):169–77.Google Scholar
Shen, CD, Beer, J, Heller, F, Kubik, PW, Suter, M, Liu, TS. 2000. 10Be-susceptibility model and quantitative estimates of pedogenic ferromagnetic material flux in Chinese loess. Nuclear Instruments and Methods in Physics Research B 172(1–4):551–4.CrossRefGoogle Scholar
Shen, CD, Beer, J, Kubik, PW, Sun, WD, Liu, TS, Liu, KX. 2009. 10Be in desert sands, falling dust and loess in China. Nuclear Instruments and Methods in Physics Research B 268(7–8):1050–3.Google Scholar
Xian, F. 2007. The study of the data analysis for the past 80ka paleo-geomagnetic field tracing and paleoprecipitation reconstruction from 10Be in loess of China [PhD dissertation]. Beijing: Graduate University of Chinese Academy of Sciences.Google Scholar
Xian, F, An, ZS, Wu, ZK, Beck, JW, Yu, HG, Kang, ZH, Cheng, P. 2008. A simple model for reconstructing geomagnetic field intensity with 10Be production rate and its application in loess studies. Science in China Series D 51(6):855–61.CrossRefGoogle Scholar
Zhang, XY, Gong, SL, Zhao, TL, Arimoto, R, Wang, YQ, Zhou, ZJ. 2003. Sources of Asian dust and role of climate change versus desertification in Asian dust emission. Geophysical Research Letters 30(24):2272, doi:10.1029/2003GL018206.CrossRefGoogle Scholar
Zhou, WJ, Zhao, X, Lu, XF, Lin, L, Zhengkun, W, Peng, C, Wengnian, Z, Chunhai, H. 2006. The 3MV multi-element AMS in Xian, China: unique features and preliminary tests. Radiocarbon 48(2):285–93.CrossRefGoogle Scholar
Zhou, WJ, Priller, A, Beck, WJ, Wu, ZK, Chen, MB, An, ZS, Kutschera, W, Xian, F, Yu, HG, Liu, L. 2007a. Disentangling geomagnetic and precipitation signals in an 80-kyr Chinese loess record of 10Be. Radiocarbon 49(1):139–60.CrossRefGoogle Scholar
Zhou, WJ, Chen, MB, Xian, F, Song, SH, Wu, ZK, Jull, AJT, Liu, WG. 2007b. The mean value concept in mono-linear regression of multi-variables and its application to trace studies in geosciences. Science in China Series D 50(12):1828–34.CrossRefGoogle Scholar
Zhou, WJ, Lu, XF, Wu, ZK, Zhao, WN, Huang, CH, Li, LL, Cheng, P. 2007c. New results on Xi'an-AMS and sample preparation systems at Xi'an-AMS center. Nuclear Instruments and Methods in Physics Research B 262(1):135–42.CrossRefGoogle Scholar
Zhou, WJ, Xian, F, Beck, JW, Jull, AJT, An, ZS, Wu, ZK, Liu, M, Chen, MB, Priller, A, Kutschera, W, Burr, GS, Yu, HG, Song, SH, Cheng, P, Kong, XH. 2010. Reconstruction of 130-kyr relative geomagnetic intensities from 10Be in two Chinese loess sections. Radiocarbon 52(1):129–47.CrossRefGoogle Scholar