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《Scientia Geographica Sinica》 2005-05
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Grain-size Characteristics and Their Environmental Significance of Hongze Lake Sediments

HE Hua-Chun,DING Hai-Yan,ZHANG Zhen-Ke,SHI Xiao-Dong,LI Shu-Heng,MAO Long-Jiang(The Key Laboratory of Coast & Island Development of Ministry of Education,Nanjing University,Nanjing,Jiangshu 210093)  
As a main lodging of surface substances,lake sediments continuously and sensitively record information of regional climate and environment with annual to decadal resolution.The sediment core of HLC with a length of 112 cm was taken from deep water location in Hongze Lake in 2003,the sediment were cut at interval of 2 cm and were measured for grain sizes by the particle-size analyzer "Mastersizer 2000"made in England.Based on accurate dating by ~(210)Pb,the authors reconstruct the dry-humid transformation history of the regional climate according to the vertical profile of sediment particle sizes,which provides a new effective way for recovering the century-scale climatic changes,the following conclusions are drawn: (1) By the analyses of the grain-size parameters of the Hongze lake sediments,three stages of environmental changes since 300 years ago have been distinguished.They are:Ca.1720-1795A.D.,the amount of rainfall was less and weather was drought;Ca.1795A.D.-1890A.D.,as a whole,the average grain-size was decrease,the weather was drought in this stage but Ca.1886 A.D.the flux of water into Hongze Lake was increased;Ca.1890 to current,the changes of grain-size parameter was acute and frequent and this changing phenomenon perhaps instead of the environment fluctuate in shorter periods. (2) During long time-scale studies,lake level is the most important factor domination sediment grain size.Sediments are finer during the humid period of high water level because coarse particles cannot be transported to the lake's deepwater part.On the contrary,during short time-scale studies within a given climate period,rainfall change becomes the key factor determining sediment grain size because the level is basically constant.When rainfall is heavy,runoff flow is strong enough to bring coarse terrestrial particles to the sampling location,resulting in large grain sizes. (3) Grain-size parameters changes is relate not only with the natural environment changes but also with the human activities such as Huanghe(Yellow) River changing channel and some brakes were built up around the lake.
【Fund】: 国家自然科学基金“河海交互作用与苏北平原成因研究(40271004)”资助项目
【CateGory Index】: X832;
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6 DAI Xue rong 1 LI Ji jun 2 YU Li zhong 1 SHI Yu xin 3 WANG Jia cheng 4 1(Department of Geography,East China Normal University,Shanghai 200062) 2(Department of Geography,Lanzhou University,Lanzhou 730000) 3(Lanzhou Institute of Geology;Model of Grain-size Distribution of the Eolian Deposits in Lanzhou Area and its Paleoclimatic Significances[J];ACTA SEDIMENTOLOGICA SINICA;2000-01
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8 Sun Jianzhong (Institute of Geological Sciences, Jilin Province);QUATERNARY PERIGLACIAL STAGES OF THE SONGLIAO PLAIN[J];Scientia Geographica Sinica;1981-02
9 Chen Jiaqi (Nanjing Institute of Geography and Limnology,Academia Sinica);A PRELIMINARY RESEARCH ON THE REGULARITY AND FACTORS OF CHANGES OF FLOOD AND DROUGHT IN TAIHU LAKE BASIN SINCE THE SOUTHERN SONG DYNASTY[J];Scientia Geographica Sinica;1989-01
10 Zhang Shufu Xiao Jiayi (Nanjing Normal University) Yu Lizhong (Liverpool University, U.K.) Wu Yushuc (Institute of Botany, Academia Sinica, Beijing);MINERAL MAGNETIC MEASUREMENT OF LAKE SEDIMENTS AND ITS ENVIRONMENTAL IMPLICATION[J];Scientia Geographica Sinica;1991-02
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