QUANTITIVELY PARTITION OF EOLIAN AND HYDROMORPHIC COMPONENTS IN LACUSTRINE SEDIMENTS: AN EXAMPLE FROM LAKE QINGHAI

DONG Jibao; AN Zhisheng; LU Fengyan

Volume 16 Issue 4

Dec. 2010

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Article Navigation > Journal of Geomechanics > 2010 > 16(4): 402-411

DONG Jibao, AN Zhisheng, LU Fengyan, 2010. QUANTITIVELY PARTITION OF EOLIAN AND HYDROMORPHIC COMPONENTS IN LACUSTRINE SEDIMENTS: AN EXAMPLE FROM LAKE QINGHAI. Journal of Geomechanics, 16 (4): 402-411.

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QUANTITIVELY PARTITION OF EOLIAN AND HYDROMORPHIC COMPONENTS IN LACUSTRINE SEDIMENTS: AN EXAMPLE FROM LAKE QINGHAI

DONG Jibao^{1, 2},
AN Zhisheng¹,
LU Fengyan^{1, 2}

1.
State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, The Chinese Academy of Sciences, Xi'an 710075, P. R. China
2.
Graduate School of The Chinese Academy of Sciences, Beijing 100049, P. R. China

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Abstract

Abstract

This paper reports a cluster analysis on sources of Lake Qinghai sediments, and a grainsize analysis on the surface sediments of Lake Qinghai and its adjacent typical aeolian loess Based on the results, we have fitted the typical grain size distributions of the lake sediments and evaluated the proportions of eolian and fluvial components by using the grain size distributions of given end members, i. e., taking the aeolian loess sediments around the lake as eolian end-member and the surface lake sediments as fluvial end-member. The fitting result shows that the grain size distributions of Lake Qinghai sediments can be grouped into three types:1) dominated by fluvial components; 2) dominated by eolian components (aeolian loess); 3) mixture of both with different proportions. It is hopeful that this method will provide a new way for quantitively partition of different components in lake sediments and for understanding of paleoenvironment. in the future researches.
- Lake Qinghai,
- Grain size,
- Eolian component,
- Quantitively partition,
- Cluster analysis

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References

[1]	Doeglas J. D. Grain-size indices, classification and environment[J] Sedimentlogy, 1968, 10:83~100. doi: 10.1111/sed.1968.10.issue-2
[2]	Visher G S. Grain size distributions and depositional processes[J]. Journal of Sedimentary Petrology. 1969, 39 (3): 1074~1106. http://d.old.wanfangdata.com.cn/NSTLQK/NSTL_QKJJ0226056781/
[3]	鹿化煜, 安芷生.黄土高原红粘土与黄土古土壤粒度特征对比-红粘土风成成因的新证据[J].沉积学报, 1999, 17 (2):226~232. doi: 10.3969/j.issn.1000-0550.1999.02.011 LU Huayu, AN Zhisheng. Comparison of Grainsize distribution of red clay and loess-paleosol deposits in Chinese Loess Plateau[J]. Acta Sedimentology Sinica, 1999, 17 (2):226~232. doi: 10.3969/j.issn.1000-0550.1999.02.011
[4]	Lu H Y, Vandenberghe J, An Z. S. Aeolian origin and palaeoclimatic implications of the 'red clay'(north China) as evidence by grain-size distribution[J]. Journal of Quaternary Science, 2001, 16 (1):89~97. doi: 10.1002/(ISSN)1099-1417
[5]	Solohub J. T., Klovan J. E. Evaluation of grain-size parameters in lacustrine environments[J]. Journal of Sedimentary Petrology, 1970, 40 (1):81~101. http://www.researchgate.net/publication/285864115_Evaluation_of_grain-size_parameters_in_lacustrine_environments
[6]	Friedman M. G. Address of the retiring president of the international association of sedimentologists:differences in size distributions of populations of particles among sands of various origins[J]. Sedimentology, 1979, 26:3~32. doi: 10.1111/sed.1979.26.issue-1
[7]	Sahu B K. Depositonal mechanisms from the size analysis of clastic sediments[J]. Journal of Sedimentary Petrology, 1964, 34 (1):73~83. http://www.researchgate.net/publication/250081317_Depositional_Mechanisms_from_the_Size_Analysis_of_Clastic_Sediments
[8]	Passega R. Grain size representation by CM patterns as a geological tool[J]. Journal of Sedimentary Petrology. 1964, 34 (4):830~847. doi: 10.1306/74D711A4-2B21-11D7-8648000102C1865D
[9]	Klovan E. J. the use of factor analysis in determining depositional environments from grain-size distribution[J]. Journal of Sedimentary Petrology. 1966, 36 (1):115~125. https://www.researchgate.net/publication/240778442_The_Use_of_Factor_Analysis_in_Determining_Depositional_Environments_from_Grain-Size_Distributions
[10]	曲政.沉积物粒度数据表征方法的研究[J].中国粉体技术, 2001, 7 (4):24~31. doi: 10.3969/j.issn.1008-5548.2001.04.008 QU Zheng. Research on grainsize presentation method of sediments[J]. China Powder Science and Technology, 2001, 7 (4):24~31. doi: 10.3969/j.issn.1008-5548.2001.04.008
[11]	方志江, 曲政. BP网络在沉积环境自动识别中的应用[J].煤田地质与勘探, 2000, 28 (2):13~15. doi: 10.3969/j.issn.1001-1986.2000.02.004 FANG Zhijiang, QU Zheng. Application of BP neutral network in environmental recognition model[J]. Coal Geology & Exploration, 2000, 28 (2):13~15. doi: 10.3969/j.issn.1001-1986.2000.02.004
[12]	柏春广, 穆桂金, 王建.艾比湖湖相沉积物粒度的分维特征及环境意义[J].干旱区地理, 2002, 25 (4):336~ 341. doi: 10.3321/j.issn:1000-6060.2002.04.009 BO Chunguang, MU Guijin, WANG Jian. Grain-size fractal dimensions characteritics of lacustrine sediments of Aiby Lake and the environmental significance[J]. Arid Land Geography, 2002, 25 (4):336~341. doi: 10.3321/j.issn:1000-6060.2002.04.009
[13]	柏春广, 王建.一种新的粒度指标:沉积物粒度分维值及其环境意义[J].沉积学报, 2003, 21 (2):234~239. doi: 10.3969/j.issn.1000-0550.2003.02.007 BO Chunguang, WANG Jian. A new grainsize index:grain-size fractal dimension of sediment and its environmental significance[J]. Acta Sedimentology Sinica, 2003, 21 (2):234~239. doi: 10.3969/j.issn.1000-0550.2003.02.007
[14]	陈冬梅, 穆桂金.不同沉积环境下沉积物的粒度分形特征的对比研究[J].干旱区地理, 2004, 27 (1):47~51. doi: 10.3321/j.issn:1000-6060.2004.01.009 CHEN Dong mei, MU Guijin. Comparising study of grain-size fractal dimensions characteristics between several sediments with different forming environments[J]. Arid Land Geography, 2004, 27 (1):47~51. doi: 10.3321/j.issn:1000-6060.2004.01.009
[15]	McLaren P. An interpretation of trends in grain size measures[J]. Journal of Sedimentary Petrology 1981, 51 (2), 611~ 624. http://www.researchgate.net/publication/250081957_An_Interpretation_of_Trends_in_Grain_Size_Measures
[16]	McLaren P. Donald Bowles. The effects of sediment transport on grain-size distributions[J]. Journal of Sedimentary Petrology 1985, 55 (4), 457~470. http://www.researchgate.net/publication/236628463_The_Effects_Of_Sediment_Transport_On_Grain-Size_Distributions
[17]	李敬卫, 乔彦松, 王燕, 等.江西九江红土堆积的粒度特征及成因研究[J].地质力学学报, 2009, 15 (1):95 ~104. doi: 10.3969/j.issn.1006-6616.2009.01.009 LI Jingwei, QIAO Yansong, WANG Yan, et al. Aeolian origin of the red earth formation in Jiujiang City of Jiangxi Province, China:Evidence from grain-size analysis[J]. Journal of Geomechanics, 2009, 15 (1):95~104. doi: 10.3969/j.issn.1006-6616.2009.01.009
[18]	于学峰, 周卫健, 刘晓清, 等.青藏高原东部全新世泥炭灰分的粒度特征及其古气候意义[J].沉积学报, 2006, 24 (6):864~869. doi: 10.3969/j.issn.1000-0550.2006.06.012 YU Xuefeng, ZHOU Weijian, LIU Xiaoqing, et al. Grain size characteristics of the Holocene peat sediment in eastern Tibetan Plateau and its paleoclimatic significance[J]. Acta Sedimentology Sinica, 2006, 24 (6):864~869. doi: 10.3969/j.issn.1000-0550.2006.06.012
[19]	乔彦松, 郭正堂, 郝青振, 等.中新世黄土-古土壤序列的粒度特征及其对成因的指示意义[J].中国科学D辑地球科学, 2006, 36 (7):646~653. http://d.old.wanfangdata.com.cn/Periodical/zgkx-cd200607005 QIAO Yansong, GUO Zhengtang, HAO Qingzhen, et al. Grain-size features of the Miocene loess-soil sequence at Qinan: Inplications on its origin[J]. Science in China Ser. D Earth Sciences, 2006, 36 (7):646~653. http://d.old.wanfangdata.com.cn/Periodical/zgkx-cd200607005
[20]	张平, 宋春晖, 杨用彪, 等.稳定湖相沉积物和风成黄土粒度判别函数的建立及其意义[J].沉积学报, 2008, 26 (3):501~507. http://d.old.wanfangdata.com.cn/Periodical/cjxb200803018 ZHANG Ping, SONG Chunhui, YANG Yongbiao, et al. The significance and establishment of discriminant function with grain size of stable lacustrine sediment and eolian loess[J], Acta Sedimentology Sinica, 2008, 26 (3):501~507. http://d.old.wanfangdata.com.cn/Periodical/cjxb200803018
[21]	孙东怀, 鹿化煜, Rea D. K.中国黄土粒度的双峰分布及其古气候意义[J].沉积学报, 2000, 18 (3):337~ 335. http://d.old.wanfangdata.com.cn/Periodical/cjxb200003001 SUN Donghuai, LU Huayu, Rea D. K Bimode grain-size distribution of Chinese loess and its paleoclimate implication [J]. Acta Sedimentology Sinica, 2000, 18 (3):337~335. http://d.old.wanfangdata.com.cn/Periodical/cjxb200003001
[22]	孙东怀, 安芷生, 苏瑞侠, 等.古环境中沉积物粒度组分分离的数学方法及其应用[J].自然科学进展, 2001, 11 (3):269~276. doi: 10.3321/j.issn:1002-008X.2001.03.008 SUN Donghuai, AN Zhisheng, SU Ruixia, et al. Mathematical approach to sedimentary component partitioning of polymodal sediments and its applications[J]. Progress in Natural Science, 2001, 11 (3):269~276. doi: 10.3321/j.issn:1002-008X.2001.03.008
[23]	孙东怀.黄土粒度分布中的超细粒组分及其成因[J].第四纪研究, 2006, 26 (6):928~936. doi: 10.3321/j.issn:1001-7410.2006.06.007 SUN Donghuai. Supper-fine grain size compositions in Chinese loess and their palaeoclimatic implication[J]. Quaternary Sciences, 2006, 26 (6):928~936. doi: 10.3321/j.issn:1001-7410.2006.06.007
[24]	Sun Donghuai, Bloemendal J, Rea D. K, et al. Grain-size distribution function of polymodal sediments in hydraulic and aeolian environments, and numerical partitioning of the sedimentary components[J]. Sedimentary Geology, 2002, 152: 263~277. doi: 10.1016/S0037-0738(02)00082-9
[25]	Sun Donghuai, Bloemendal J, Rea D. K, et al. Bimodal grain-size distribution of Chinese loess, and its palaeoclimatic implications[J]. Catena, 2004, 55:325~340. doi: 10.1016/S0341-8162(03)00109-7
[26]	Sun Donghuai. Monsoon and westerly circulation changes recorded in the late Cenozoic aeolian sequences of Northern China [J]. Global and Planetary Change, 2004, 41:63~80. doi: 10.1016/j.gloplacha.2003.11.001
[27]	殷志强, 秦小光, 吴金水, 等.中国北方部分地区黄土、沙漠沙、湖泊、河流细粒沉积物粒度多组分分布特征研究[J].沉积学报, 2009, 27 (2):343~351. http://d.wanfangdata.com.cn/Periodical/cjxb200902019 YIN Zhiqiang, QIN Xiaoguang, WU Jinshui, et al. The multimodal grain-size distribution characteristics of loess, desert, lake and river sediments in some areas of northern China[J]. Acta Sedimentology Sinica, 2009, 27 (2):343~351. http://d.wanfangdata.com.cn/Periodical/cjxb200902019
[28]	Xiao Jule, Chang Zhigang, Si Bin et al. partitioning of the grain-size components of Dali Lake core sediments:evidence for lake-level changes during the Holocene[J]. Journal of Paleolimnology, 2009, 42:249~260. doi: 10.1007/s10933-008-9274-7
[29]	Weltje J. G. End-member modeling of compositional data Numerical-statistical algorithms for solving the explicit mixing problem[J]. Mathmatical Geology, 1997, 29 (4):503~549. doi: 10.1007/BF02775085
[30]	Weltje J. G., Prins A. M. muddled or mixed? inferring palaeoclimate from size distributions of deep sea clastics[J]. sedimentary geology, 2002, 162:39~62. doi: 10.1016-S0037-0738(03)00235-5/
[31]	Prins M A, Vriend M, Nugteren G, et al. Late Quaternary aeolian dust input variability on the Chinese Loess Plateau: inferences from unmixing of loess grain-size records[J]. Quaternary Science Reviews, 2007, 26:230~242. doi: 10.1016/j.quascirev.2006.07.002
[32]	Weltje J. G., Prins A. M. Genetically meaningful decomposition of grain-size distributions[J]. sedimentary geology, 2007, 202:409~424. doi: 10.1016/j.sedgeo.2007.03.007
[33]	Prins A. M, Zheng Hongbo, Beets K, et al. Dust supply from river floodplains:the case of the lower Huang He (Yellow River) recorded in a loess-palaeosol sequence from the Mangshan Plateau[J]. Journal of Quaternary Science, 2008, 24: 75~84. http://cn.bing.com/academic/profile?id=39a237709ef2243c04d1c9e94a034656&encoded=0&v=paper_preview&mkt=zh-cn
[34]	Xu, H., Liu, X., An, Z. S. et al. Spatial pattern of modern sedimentation rate of Qinghai Lake and a preliminary estimate of the sediment flux. Chinese Science Bulletin. 2010, 55 (7):621~627. doi: 10.1007/s11434-009-0580-x
[35]	Jin, Z. D., You, C. F., Yu, J. M. Toward a geochemical mass balance of major elements in Lake Qinghai, NE Tibetan Plateau:A significant role of atmospheric deposition[J]. Applied Geochemistry. 2009, 24:1901~1907. doi: 10.1016/j.apgeochem.2009.07.003
[36]	中国科学院兰州分院, 中国科学院西部资源环境研究所.青海湖近代环境的演化和预测[M].北京:科学出版社, 1~10.1994. Lanzhou Branch of Chinese Academy of Sciences, West Center of Resource and Environment, Chinese Academy of Sciences. Evolution of Recent Environment in Qinghai Lake and Its Prediction. Science Press, Beijing, 1~10 1994.
[37]	陈发虎, 汪世兰, 张维信, 等.青海湖南岸全新世黄土剖面、气候信息及湖南升降探讨[J].地理科学, 1991, 11 (1):76~85. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK000005715624 CHEN Fahu, WANG Shilan, ZHANG Weixi, et al. THE Loess profile at south bank, climatic information and lake-level fluctuation of Qinghai lake during the Holocene[J]. Sinica Geographica Sinica, 1991, 11 (1):76~85. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK000005715624
[38]	师永民, 王新民, 宋春晖.青海湖湖区风成沙堆积[J].沉积学报, 1996, 14 (增刊):235~240. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199600006153 SHI Yongmin, WANG Xinmin, SONG Chunhui. Aeolian Deposition in Qinghai Lake Area[J]. Acta Sedimentology Sinica, 1996, 14 (Supp.):235~240. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199600006153
[39]	宋春晖, 方小敏, 师永民, 等.青海湖西岸风成沙丘特征及成因[J].中国沙漠, 2000, 20 (4):443~446. doi: 10.3321/j.issn:1000-694X.2000.04.021 SONG Chunhui, FANG Xiaomin, SHI Yongmin, et al. Characteristics and formation of aeolian dune on western shore of the Qinghai lake[J]. Journal of Desert Research, 2000, 20 (4):443~446. doi: 10.3321/j.issn:1000-694X.2000.04.021
[40]	周笃琚, 马海州, 高东林, 等.青海湖南岸全新世黄土地球化学特征及气候环境意义[J].中国沙漠, 2004, 24 (2):144~148. doi: 10.3321/j.issn:1000-694X.2004.02.005 ZHOU Dujun, MA Haizhou, GAO Donglin, et al. Geochemical Characteristics and Climatic Environmental Significance of Holocene Loess on South Qinghai Lake Shore[J]. Journal of Desert Research, 2004, 24 (2):144~148. doi: 10.3321/j.issn:1000-694X.2004.02.005
[41]	赵存法, 鹿化煜, 周亚利, 等.青海湖地区冰消期以来气候变化的黄土记录[J].高校地质学报, 2009, 15 (1): 135~140. doi: 10.3969/j.issn.1006-7493.2009.01.014 ZHAO Cunfa, LU Huayu, ZHOU Yali, et al. Palaeoclimate Changes Recorded by Loess Deposit around Qinghai Lake (Northeastern Qinghai-Tibetan Plateau) since Last Deglaciation[J]. Geological Journal of China Universities, 2009, 15 (1):135~140. doi: 10.3969/j.issn.1006-7493.2009.01.014