中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Sedimentary records of water environment in lake Chaohu in the Yangtze delta region, China

文献类型:期刊论文

作者Du, L.1; Yi, C. L.1; Pan, S. M.1; Xie, P.2
刊名JOURNAL OF COASTAL RESEARCH
出版日期2006-12-01
卷号1页码:242-245
ISSN号0749-0208
关键词grain-size parameters (137)Cs dating sedimentation rate sedimentary environment Chaohu lake
通讯作者Du, L, Nanjing Univ, Dept Geog, Key Lab Coast & Isl Dev, Nanjing 210093, Peoples R China
中文摘要Three lacustrine core samples were collected from Chaohu lake in December 2002 in the Yangtze delta region. The grain sizes were analyzed using a Laser Analyzer to obtain grain-size parameters. Sediment geochronology was determined in radioisotopes Cs-137 and the average sedimentary rates are 0.29cm.a(-1), 0.35 cm.a(-1) and 0.24cm-a(-1) in Cores C 1, C2 and C3, respectively. The grain-size parameters of the deposits vary regularly with the fluctuation of hydrodynamics. From 1950s to the beginning of 20th century, coarse-grained sediment was deposited, suggesting strong hydraulic conditions and high water-level periods with much precipitation; from the start of 20(th) century to latter half of 18(th) century, fine-grained sediment was deposited, indicating that weak hydraulic conditions and low water-level periods with less precipitation; before the first half of 18(th) century, coarse-grained sediment was deposited, suggesting great velocity of flow and high water-level periods of more precipitation.
英文摘要Three lacustrine core samples were collected from Chaohu lake in December 2002 in the Yangtze delta region. The grain sizes were analyzed using a Laser Analyzer to obtain grain-size parameters. Sediment geochronology was determined in radioisotopes (137)Cs and the average sedimentary rates are 0.29cm.a(-1), 0.35 cm.a(-1) and 0.24cm-a(-1) in Cores C 1, C2 and C3, respectively. The grain-size parameters of the deposits vary regularly with the fluctuation of hydrodynamics. From 1950s to the beginning of 20th century, coarse-grained sediment was deposited, suggesting strong hydraulic conditions and high water-level periods with much precipitation; from the start of 20(th) century to latter half of 18(th) century, fine-grained sediment was deposited, indicating that weak hydraulic conditions and low water-level periods with less precipitation; before the first half of 18(th) century, coarse-grained sediment was deposited, suggesting great velocity of flow and high water-level periods of more precipitation.
学科主题Environmental Sciences; Geography, Physical; Geosciences, Multidisciplinary
WOS标题词Science & Technology ; Life Sciences & Biomedicine ; Physical Sciences
类目[WOS]Environmental Sciences ; Geography, Physical ; Geosciences, Multidisciplinary
研究领域[WOS]Environmental Sciences & Ecology ; Physical Geography ; Geology
收录类别SCI
语种英语
WOS记录号WOS:000202961300045
公开日期2010-10-13
源URL[http://ir.ihb.ac.cn/handle/152342/8754]  
专题水生生物研究所_中科院水生所知识产出(2009年前)_期刊论文
作者单位1.Nanjing Univ, Dept Geog, Key Lab Coast & Isl Dev, Nanjing 210093, Peoples R China
2.Chinese Acad Sci, Inst Hydrobiol, State Key Lab Freshwater Ecol & Biotechnol China, Donghua Expt Stn Lake Ecosyst, Wuhan, Peoples R China
推荐引用方式
GB/T 7714
Du, L.,Yi, C. L.,Pan, S. M.,et al. Sedimentary records of water environment in lake Chaohu in the Yangtze delta region, China[J]. JOURNAL OF COASTAL RESEARCH,2006,1:242-245.
APA Du, L.,Yi, C. L.,Pan, S. M.,&Xie, P..(2006).Sedimentary records of water environment in lake Chaohu in the Yangtze delta region, China.JOURNAL OF COASTAL RESEARCH,1,242-245.
MLA Du, L.,et al."Sedimentary records of water environment in lake Chaohu in the Yangtze delta region, China".JOURNAL OF COASTAL RESEARCH 1(2006):242-245.

入库方式: OAI收割

来源:水生生物研究所

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