Earth Surface Processes

Modern sedimentation rates and dry-humid change inferred from grain size records in Dianchi Lake, Yunnan Province

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  • 1. College of Geography Science, Nanjing Normal University, Nanjing 210046, China;
    2. Institute of Soil Science, CAS, Nanjing 210008, China

Received date: 2009-12-14

  Revised date: 2010-05-23

  Online published: 2011-01-20

Abstract

Based on radionuclide dating (210Pb and 137Cs) in the sediment core of the Dianchi Lake, Yunnan Province of China, we calculated the sedimentation rates in the past 159 years. The vertical profile of 137Cs has three obvious 137Cs peaks in the core corresponding to 1963, 1975 and 1986, since the onset of 137Cs fallout in 1954. Using the dating of the 137Cs peaks, the four time-averaged accumulation rates of the Dianchi Lake were 0.062, 0.051, 0.049 and 0.043 g/cm2·a-1, respectively. Four stages with different accumulation rates in core DC1 indicated a slower process since the onset of atmospheric nuclear weapons testing in the 1954. According to the result of 210Pb (CRS) dating in DC1, the sedimentation rate is 0.052 g/cm2·a-1, which is unstable in the past 129 years, which might be related to human activities during different historical periods of the past 100-150 years. As for dissimilar physical and chemical associations, diffusion characteristics for the two radionuclides (Pb and Cs), we interpreted the rationality of deviation by the two dating methods. The further precise result can be obtained by combining two or more dating methods, respectively. Compared with the local rainfall in the past 50 years with sediment grain size in the region of Dianchi Lake, it is found that there was an obvious variation trend in the sediment grain size with the fluctuations of rainfall. All these findings indicate that there is a positive correlation between grain size and the fluctuations of rainfall. This shows that sediment grain size could reflect the rainfall changes trend at a short time-scale and high resolution investigations, i.e. larger sediment grain size reflected more rainfall and wetter climate while smaller sediment grain size reflected less rainfall and drier climate.

Cite this article

WANG Xiao-lei, YANG Hao, ZHAO Qi-guo, CHEN Ye, CHEN Jing-song, WANG Lin-xian . Modern sedimentation rates and dry-humid change inferred from grain size records in Dianchi Lake, Yunnan Province[J]. GEOGRAPHICAL RESEARCH, 2011 , 30(1) : 161 -171 . DOI: 10.11821/yj2011010016

References

[1] 王苏民,窦鸿身. 中国湖泊志. 北京:科学出版社, 1998. 374~377.

[2] Evangeliou N, Florou H, Bokoros P, et al. Temporal and spatial distribution of 137Cs in Eastern Mediterranean Sea, horizontal and vertical dispersion in two regions. Journal of Environmental Radioactivity, 2009, 100:626~636.

[3] Putyrskaya V, Klemt E, Rǒllin S. Migration of 137Cs in tributaries, lake water and sediment of Lago Maggiore (Italy, Switzerland):Analysis and comparison with Lago di Lugano and other lakes. Journal of Environmental Radioactivity, 2009, 100:35~48.

[4] 王小雷,杨浩,赵其国,等. 利用210Pb、137Cs和241Am计年法研究云南抚仙湖现代沉积速率. 湖泊科学,2010, 22(1):136~142.

[5] Wu Y H, Wang S M,Hou X H. Chronology of Holocene lacustrine sediments in Co Ngoin, central Tibetan Plateau. Science in China Series D: Earth Sciences, 2006,49:991~1001.

[6] Simms A D, Woodroffe C, Jones B G, et al. Use of 210Pb and 137Cs to simultaneously constrain ages and sources of post-dam sediments in the Cordeaux reservoir, Sydney, Australia. Journal of Environmental Radioactivity, 2008, 99:1111~1120.

[7] 姚书春, 李世杰,刘吉峰, 等. 太湖 THS 孔现代沉积物137Cs和210Pb的分布及计年. 海洋地质与第四纪地质, 2006, 26(2):79~83.

[8] 刘志广, 王福, 裴艳东, 等. 天津三河岛潮间带137Cs与210Pb的分布及现代沉积过程.地质通报,2007, 26(7):864~868.

[9] 赵锁志,孔凡吉, 王喜宽. 内蒙古乌梁素海210Pb和137Cs测年与现代沉积速率. 现代地质, 2008,22(6):909~914.

[10] 张瑞,潘少明,汪亚平. 长江河口水下三角洲210Pb分布特征及其沉积速率. 沉积学报,2009,27(4):704~713.

[11] 刘广山,李冬梅,易勇. 胶州湾沉积物的放射性核素含量分布与沉积速率. 地球学报,2008,29(6):769~777.

[12] Street-Perrott F A,Holmes J A,Waller M P, et al. Drought and dust deposition in the west African Sabel: A 5500-year record from Kajemarum Oasis,Northeastern Nigeria. The Holocene,2000,10(2): 293~302.

[13] 强明瑞,陈发虎,周爱锋,等. 苏干湖沉积物粒度组成记录尘暴事件的初步研究. 第四纪研究,2006,26(6): 915~922.

[14] 王永波,刘兴起,张恩楼,等. 青藏高原北部可可西里地区近 4000年来尘暴事件初探——来自库赛湖沉积物粒度的证据. 沉积学报,2009,27(4): 691~696.

[15] Digerfeldt G. Studies on past lake-level fluctuations, In:Berglund B E. Hand-book of Holocene Palaeoecology and Palaeohydrology, Chichester: John Wiley, 1986. 127~143.

[16] Menking K M,Bischoff J L,Fitzpatrick J A,et al. Climatic/hydrologic oscillations since 155,000 yr B.P. at Owens Lake, California, reflected in abundance and stable isotope composition of sediment carbonate. Quaternary Research, 1997, 48: 58~68.

[17] Digerfeldt G,Olsson S,Sandgren P. Reconstruction of lake-level changes in lake Xinias, central Greece, during the last 40 000 years. Palaeogeography, Palaeoclimatology, Palaeoecology, 2000, 158: 65~82.

[18] Wang H, Liu H,Cui H,et al. Terminal Pleistocene/Holocene palaeoenvironmental changes revealed by mineral-magnetism measurements of lake sediments for Dali Nor area, southeastern Inner Mongolia Plateau, China. Palaeogeography, Palaeoclimatology, Palaeoecology, 2001, 170: 115~132.

[19] 王永波,刘兴起,羊向东,等. 可可西里库赛湖揭示的青藏高原北部近 4000年来的干湿变化. 湖泊科学,2008,20(5): 605~612.

[20] 万国江. 现代沉积的210Pb计年. 第四纪研究, 1997, 17(3): 230~239.

[21] 师长兴,尤联元,李炳元,等. 黄河三角洲沉积物的自然固结压实过程及其影响. 地理科学, 2003, 23 (2): 175~181.

[22] Cambray R S,Cawse P A,Garland J A,et al. Observations on radioactivity from the Chernoby accident. Nuclear Energy,1987, 26: 77~101.

[23] 张信宝. 有关湖泊沉积137Cs深度分布资料解释的探讨. 山地学报, 2005, 23(3): 294~299.

[24] Editorial Board of Science Yearbook. China Encyclopedia Yearbook. Beijing: Encyclopedia of China Publishing House, 1980. 645~653.

[25] Editorial board of science yearbook. Science yearbook. Shanghai: Shanghai translation publishing corporation, 1992. 2~37.

[26] 张燕,彭补拙,陈捷,等. 借助137Cs估算滇池沉积量. 地理学报, 2005, 60(1): 71~78.

[27] 项亮,吴瑞金,吉磊. 137Cs和241Am在滇池、剑湖沉积物孔柱中的蓄积分布及时标意义. 湖泊科学,1996, 8(1): 27~34.

[28] 万国江. 现代沉积年分辨率的137Cs计年——以云南洱海和贵州红枫湖为例. 第四纪研究, 1999, (1): 73~80.

[29] 胥思勤,万国江. 云南省程海现代沉积物中210Pb、137Cs的分布与计年研究. 地质地球化学, 2001, 29(4): 28~31.

[30] 姚远,张恩楼,沈吉,等. 云南属都湖流域人类活动的湖泊沉积响应. 海洋地质与第四纪地质, 2007, 27(5): 115~120.

[31] 项亮. 用γ分析方法研究滇池现代沉积年代. 核技术, 1997, 20(2): 100~104.

[32] 程致远,梁卓成,林瑞芬,等. 云南滇池现代沉积物210Pb法的CF模式年龄研究. 地球化学, 1990, (4) : 127~332.

[33] Wise S M. Caesium-137 and lead-210: a review of the techniques and some applications in geomorphology. In: Cullingford R A, Davidson D A, Lewin J. Timescales in Geomorphology.Chichester, U K: Wiley, 1980. 109~127.

[34] 于银亭,李培泉,吴润,等. 昆明滇池沉积速率的测定. 海洋与湖沼, 1996, 27(1): 41~45.

[35] 万国江. 现代沉积的210Pb计年. 第四纪研究,1997,17(3): 230~239.

[36] 徐经意,万国江,王长生,等. 云南省泸沽湖、洱海现代沉积物中210Pb,137Cs的垂直分布及其计年. 湖泊科学, 1999, 11(2): 110~116.

[37] 卢少勇,金相灿,张烨,等. 滇池内湖滨带底泥的有机质分布规律. 湿地科学, 2009, 7(2): 135~141.

[38] 彭丹,金峰,吕俊杰,等. 滇池底泥中有机质的分布状况研究. 土壤, 2004, 36(5): 568~572.

[39] 项亮. 137Cs湖泊沉积年代学方法应用的局限——以Crawford湖为例. 湖泊科学, 1995, 7(4): 307~313.

[40] 昆明环境科学研究所. 滇池富营养化调查研究. 昆明:云南科技出版社, 1992. 156~159.

[41] 阎自申. 前置库在滇池流域运用研究. 云南环境科学, 1996, 15 (2): 33~35.

[42] 李仁英,杨浩,王丽,等. 滇池沉积物中重金属的形态分布特征. 土壤, 2008, 40(2): 264~268.
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