

FOLLOWUS
1. Key Lab of Marine Geology and Environment Institute of Oceanology Chinese Academy of Sciences
2. Key Lab of Marine Hydrocarbon Resources and Environmental Geology Ministry of Land and Resources
3. University of Chinese Academy of Sciences
网络首发:2014-07-11,
纸质出版:2014
Scan QR Code
High resolution records of flood deposition in the mud area off the Changjiang River mouth during the past century[J]. 海洋湖沼学报(英文), 2014,32(4):909-920.
Hu, G., Li, A., Liu, J. et al. High resolution records of flood deposition in the mud area off the Changjiang River mouth during the past century., Chin. J. Ocean. Limnol. 32, 909–920 (2014). https://doi.org/10.1007/s00343-014-3244-x
High resolution records of flood deposition in the mud area off the Changjiang River mouth during the past century[J]. 海洋湖沼学报(英文), 2014,32(4):909-920. DOI: 10.1007/s00343-014-3244-x.
Hu, G., Li, A., Liu, J. et al. High resolution records of flood deposition in the mud area off the Changjiang River mouth during the past century., Chin. J. Ocean. Limnol. 32, 909–920 (2014). https://doi.org/10.1007/s00343-014-3244-x DOI:
This paper presents a paleoflood study to determine the flood frequency of the Changjiang River
based on core cj0702
taken from the Changjiang River subaqueous delta. We identified flood deposits by means of high-resolution grain-size variation
sensitive population
geochemical indexes and magnetic susceptibility. The core covers a time span of 120 years by 210Pb dating and was sampled at 1–2 cm intervals. Grain size
geochemical elements
and physical parameters were analyzed. The results indicate that the sediment of the core is mainly composed of silt and clay
as well as groups of interbedded silt
clay silt
and clay. Vertically
the grain size pattern was controlled by seasonal variations in water discharge and by the sediment input in winter from the abandoned Huanghe River delta. River flooding caused extreme values in all our measured parameters. We identified more than 20 flood events that occurred since 1887 using the physical parameter analysis method. The environmentally sensitive component of sediment grain size (14.32–96.39 μm) contribution>30%
Zr/Rb ratio>1.5
and magnetic susceptibility>16 were selected as the criteria for flood identification generally. We also found that floods that had taken place in the upstream
midstream
or downstream parts of the river were clearly identified by these indexes while the large-scale floods that covered the whole drainage area did not leave clear indications in the sediment record. This study for identification of flood events is of great significance for understanding hyperpycnal current sedimentation as well as for forecasting of floods.
Allison M A, Kineke G C, Gordon E S. 2000. Development and reworking of a seasonal flood deposit on the inner continental shelf off the Atchafalaya River. Continental Shelf Research, 20: 2 267–2 294.
Bai J J, Zou H X, Zhu C. 2008. Archaeological discovery and research on the remains of the paleoflood of the Yuxi site. Chinese Science Bulletin, 53(Supple I): 18–27. (in Chinese with English abstract)
Bentley S J, Nittrouer C A. 2003. Emplacement, modification, and reservation of event strata on a flood-dominated continental shelf: Eel shelf, northern California. Continental Shelf Research, 23: 1 465–1 493.
Borgeld J C, Hughes-Clarke J E, Goff J A, Mayer L A, Curtis J A. 1999. Acoustic backscatter of the flood 1995 deposit on the eel shelf. Marine Geology, 154: 197–210.
Bourgeois J, Hansen T A, Wiberg P L, Kauffman E G. 1988. A tsunami deposit at the Cretaceous-Tertiary boundary in Texas. Science, 241: 567–570.
Chen J Y, Shen H T, Yun C X. 1988. Dynamic Processes and Morphological Evolution of the Changjiang Estuary. Shanghai Science and Technology Press, Shanghai. 452p. (in Chinese with English abstract)
Chen Z Y, Song B P, Wang Z H, Cai Y L. 2000. Late Quaternary evolution of the sub-aqueous Yangtze Delta, China: sedimentation, stratigraphy, palynology, and deformation. Marine Geology, 162: 423–441.
DeMaster D J, Mckee B A, Nittrouer C A, Qian J C, Cheng G D. 1985. Rates of sediment accumulation and particle reworking based on radiochemical measurements from continental shelf deposits in the East China Sea. Cont inental Shelf Res earch, 4: 143–158.
Dott R H. 1983. 1982 EPM presidential address: episodic sedimentation, how normal is average? How rare is rare? Does it matter? Journal of Sedimentary Petrology, 53: 5–23.
Drake D E. 1999. Temporal and spatial variability of the sediment grain-size distribution on the Eel shelf: the flood layer of 1995. Marine Geology, 154: 169–182.
Fan D J, Qi H Y, Sun X X, Guo Z G, Yang Z S. 2011. Annual lamination and its sedimentary implications in the Yangtze River delta inferred from High-resolution biogenic silica and sensitive grain-size records. Continental Shelf Research, 31: 129–137.
Guan B X. 1983. Sketch of the current structure and eddy characteristics in the East China Sea. Proceedings of the International Symposium Sedimentation on the Continental Shelf, With Special Reference to the East China Sea. China Ocean Press, Beijing. p.56–79. (in Chinese)
Hayes M O. 1967. Hurricanes as geological agents, south Texas coast. American Association of Petroleum Geology Bulletin, 51: 937–942.
Heezen B C, Ewing M. 1952. Turbidity currents and submarine slumps and the 1929 Grand Banks earthquake. American Journal of Science, 250: 849–878.
Hori K, Saito Y, Zhao Q H, Wang P X. 2002. Architecture and evolution of the tidal-dominated Changjiang River delta, China. Sedimentary Geology, 146: 249–264.
Hori K, Saito Y. 2007. An early Holocene sea-level jump and delta initiation. Geophysical Research Letters, 34(18): L18401.
Hu G, Shen H T, Zhuang K L, Zhou L Y, Liu J. 2007. Evolution pattern of coastal erosion in the Yangtze River Estuary. Marine Geology and Quaternary Geology, 27(1): 13–21. (in Chinese with English abstract)
Huang Z S. 2003. The historical flood and drought in Yangtze River basin. Yangtze River, 34: 1–3. (in Chinese with English abstract)
Huh C A, Su C C. 1999. Sedimentation dynamics in the East China Sea elucidated from 210P b, 137Cs, and 239, 240Pu. Mar ine Geol olgy, 160: 183–196.
Kortekaas S, Dawson A. 2007. Distinguishing tsunami and storm deposits: an example from Martinhal, SW Portugal. Sedimentary Geology, 200: 208–221.
Kuehl S A, DeMaster D J, Nittrouer C A. 1986. Nature of sediment accumulation on the Amazon continental shelf. Continental Shelf Research, 6: 209–225.
Kuehl S A, Pacioni T D, Rine J M. 1995. Seabed dynamics of the inner Amazon continental shelf: temporal and spatial variability of surficial strata. Marine Geology, 125: 283–302.
Li C A, Zhang Y F. 2004. Flood sedimental characteristic and its mark on the middle reaches of Yangtze River. Advances in Water Science, 15(4): 485–488. (in Chinese with English abstract)
Li C X, Li P. 1983. The characteristics and distribution of Holocene sand bodies in the Changjiang delta area. Acta Oceanologica Sinica, 5(2): 54–66.
Li G X, Yang Z G, Liu Y. 2005. Sediment Distribution Map of the East China Seas. Science Press, Beijing China. 65p. (in Chinese)
Liu J P, Li A C, Xu K H, Veolzzi D M, Yang Z S, Milliman J D, DeMaster D J. 2006. Sedimentary features of the Yangtze River-derived along-shelf clinoform deposit in the East China Sea. Continental Shelf Research, 26: 2 141–2 156.
Liu J, Saito Y, Kong X H, Wang H, Xiang L H, Wen C. 2010. Sedimentary record of environmental evolution off the Yangtze River estuary, East China Sea, during the last ∼13,000 years, with special reference to the influence of the Yellow River on the Yangtze River delta during the last 600 years. Quaternary Science Reviews, 29: 2 424–2 438.
McKee B A, DeMaster D J, Nittrouer C A. 1984. The use of 234Th/238U disequilibrium to examine the fate of particlereactive species on the Yangtze continental shelf. Earth and Planetary Science Letters, 68: 431–442.
McKee B A, Nittrouer C A, DeMaster D J. 1983. Concepts of sediment deposition and accumulation applied to the continental shelf near the mouth of the Yangtze River. Geology, 11: 631–633.
Milliman J D, Shen H T, Yang Z S, Mead R H. 1985. Transport and deposition of river sediment in the Changjiang estuary and adjacent continental shelf. Continental Shelf Research, 4: 37–45.
Oldfield F, Appleby P G, Battarbee R W. 1978. Alternative 210Pb dating: results from the New Guinea Highlands and Lough Erne. Nature, 271: 339–342.
Palinkas C M, Nittrouer C A, Walsh J P. 2006. Inner-shelf sedimentation in the Gulf of Papua, New Guinea: a mudrich shallow shelf setting. Journal of Coastal Research, 22(4): 760–772.
Pfitzner J, Brunskill G, Zgorskis I. 2004. 137Cs and excess 210Pb deposition patterns in estuarine and marine sediment in the central region of the Great Barrier Reef Lagoon, North-eastern Australia. Journal of Environmental Radioactivity, 76: 81–102.
Saito Y, Yang Z S, Hori K. 2001. The Huanghe (Yellow River) and Changjiang (Yangtze River) deltas: a review on their characteristics, evolution and sediment discharge during the Holocene. Geomorphology, 41: 219–231.
San Miguel E G, Bolívar J P, García-Tenorio R. 2004. Vertical distribution of Th-isotope ratios, 210Pb, 226Ra and 137Cs in sediment cores from an estuary affected by anthropogenic releases. Science of the Total Environment, 318: 143–157.
Shen H T. 2001. The Material Flux in the Yangtze River Estuary. China Ocean Press, Beijing, China. p.60–80. (in Chinese with English abstract)
Shen H T, Li J F. 2011. Water and Sediment Transport in the Changjiang Estuary. China Ocean Press, Beijing, China. p.1–7. (in Chinese with English abstract)
Sherwood C R, Butman B, Cacchione D A, Drake D E, Gross T F, Sternberg R W, Wiberg P L, Williams A J. 1994. Sediment-transport events on the northern California continental shelf during the 1990–1991 STRESS experiment. Continental Shelf Research, 14: 1 063–1 099.
Shi Y F, Jiang T, Su B D, Chen J Q, Qin N X. 2004. Preliminary analysis on the relation between the evolution of heavy flood in the Yangtze River catchment and the climate changes since 1840. Journal of Lake Sciences, 16(4): 289–297. (in Chinese with English abstract)
Sternberg R W. 1986. Transport and accumulation of riverderived sediment on the Washington continental shelf, USA. Journal of the Geological Society, 143: 945–956.
Su Y S. 1986. A survey of geographic environment, circulation system and the central fishing grounds in the Huanghai Sea and East China Sea. Journal of Shandong College of Oceanology, 16(1): 12–28. (in Chinese with English abstract)
Summerfield C K, Nittrouer C A, Alexander C R. 1999. 7Be as a tracer of flood sedimentation on the northern California continental margin. Continental Shelf Research, 19: 335–361.
Wang K, Feng S Z, Shi X H. 2001. A 3D baroclinic model of summer circulation in the Bohai, Yellow and East China Seas. Oceanologia et Limnologia Sinica, 32(5): 551–560. (in Chinese with English abstract)
Wang M J, Zheng H B, Xie X, Fan D D, Yang S Y, Zhao Q H, Wang K. 2011. A 600-year flood history in the Yangtze River drainage: comparison between a subaqueous delta and historical records. Chinese Science Bulletin, 56(2): 188–195.
Wang X. 2011. Post-Glacial Sediment Environment Evolution of the Subaqueous Yangtze delta. Ph.D Thesis, Institute of oceanology, Chinses Academy of Sciences. (in Chinese with English abstract)
Wheatcroft R A, Borgeld J C. 2000. Oceanic flood deposits on the northern California shelf: large-scale distribution and small-scale physical properties. Continental Shelf Research, 20: 2 163–2 190.
Wheatcroft R A, Sommerfield C K, Drake D E, Borgeld J C, Nittrouer C A. 1997. Rapid and widespread dispersal of flood sediment on the northern California margin. Geology, 25: 163–166.
Xia N, Zhang Q, Yao D, Li G H. 2008. Geochemical analysis of marine sediments using fused glass disc by X-ray fluorescence spectrometry. Chinese Journal of Oceanology and Limnology, 26(4): 475–479.
Xia P, Meng X W, Yin P, Cao Z M, Wang X Q. 2011. Eightyyear sedimentary record of heavy metal inputs in the intertidal sediments from the Nanliu River estuary, Beibu Gulf of South China Sea. Environmental P ollution, 159: 92–99.
Xiang R, Yang Z L, Saito Y, Guo Z G, Fan D J, Li Y H, Xiao S B, Shi X F, Chen M H. 2006. East Asia Winter Monsoon changes inferred from environmentally sensitive grainsize component records during the last 2300 years in mud area southwest off Cheju Island ECS. Science in China Series D, 49(6): 604–614.
Xiao S B, Li A C. 2005. A study on environmentally sensitive grain size population in inner shelf of the East China Sea. Acta Sedimentologica Sinica, 23(1): 122–129. (in Chinese with English abstract)
Xiao S B, Li R, Chen M H. 2013. Detecting sedimentary cycles using autocorrelation of grain size. Scienctific Report, 3: 1–8.
Yang D Y, Xie Y B. 1997. Paleoflood lack-water deposits. Acta Sedimentol ogica Sin ica, 15(3): 29–32. (in Chinese with English abstract)
Yang Z S, Chen X H. 2007. Centurial high resolution records of sediment grain-size variation in the mud area off the Changjiang (the Yangtze River) estuary and its influential factors. Quaternary Sciences, 27(5): 690–699.
Yang Z S, Wang H J, Saito Y, Milliman J D, Xu K H, Qiao S Q. 2006. Dam impacts on the Changjiang (Yangtze River) sediment discharge to the sea: the past55 years and after the Three Gorges dam. Water Resources Research, 42(4): 1–10.
Yang Z S. 1988. Mineralogical assemblages and chemical characteristics of clays from sediments of the Huanghe, Changjiang, Zhujiang Rivers and their relationship to the climate environment in their sediment source areas. Oceanologia et Limnologia Sinica, 19(4): 336–346.
Yuan S Y, Zhao X A, Li C A. 2006. Identification marks of Paleoflood. Geological Science and Technology Information, 25(4): 55–58. (in Chinese with English abstract)
Zhang Y F, Li C A, Chen L, Wang H. 2009. Magnetic fabric of Holocene palaeo-floods events in Jianghan Plain. Earth Science (Journal of China University of Geosciences), 34(6): 985–992. (in Chinese with English abstract)
Zhang Y F, Li C A, Yan G L, Dong X H. 2004. A comparison study of magnetic fabric characters between flooded sediments and normal river sediments. Chinese Journal of Geophysics, 47(4): 639–645. (in Chinese with English abstract)
Zhao J B, Zhou X H, Sun G Z. 2007. Research on flood change indicated by deposit in high valley flat profile of Weihe River in Xianyang. Acta Sedimentol ogica Sinica, 25(4): 597–602. (in Chinese with English abstract)
Zhu C, Zheng C G, Ma C M, Sun Z B, Zhu G Y, Wang H L. 2005. The study on ancient flood sediment at central dam ruins in the reservoir area of Three Gorges of the Yangtze River. Chinese Science Bulletin, 50(20): 2 240–2 250. (in Chinese with English abstract)
0
浏览量
0
Downloads
7
CSCD
关联资源
相关文章
相关作者
相关机构

京公网安备11010802024621