长江口及邻近海域现代沉积速率及其对长江入海泥沙去向的指示意义

王昕; 石学法; 王国庆; 乔淑卿; 刘涛

doi:10.3799/dqkx.2013.074

Volume 38 Issue 4

Jul. 2013

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Article Navigation > Earth Science > 2013 > 38(4): 763-775

WANG Xin, SHI Xue-fa, WANG Guo-qing, QIAO Shu-qing, LIU Tao, 2013. Sedimentation Rates and Its Indication to Distribution of Yangtze Sediment Supply around the Yangtze (Changjiang) River Estuary and Its Adjacent Area, China. Earth Science, 38(4): 763-775. doi: 10.3799/dqkx.2013.074

Citation:

WANG Xin, SHI Xue-fa, WANG Guo-qing, QIAO Shu-qing, LIU Tao, 2013. Sedimentation Rates and Its Indication to Distribution of Yangtze Sediment Supply around the Yangtze (Changjiang) River Estuary and Its Adjacent Area, China. Earth Science, 38(4): 763-775. doi: 10.3799/dqkx.2013.074

Citation:

WANG Xin, SHI Xue-fa, WANG Guo-qing, QIAO Shu-qing, LIU Tao, 2013. Sedimentation Rates and Its Indication to Distribution of Yangtze Sediment Supply around the Yangtze (Changjiang) River Estuary and Its Adjacent Area, China. Earth Science, 38(4): 763-775. doi: 10.3799/dqkx.2013.074

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Sedimentation Rates and Its Indication to Distribution of Yangtze Sediment Supply around the Yangtze (Changjiang) River Estuary and Its Adjacent Area, China

doi: 10.3799/dqkx.2013.074

1.
Ludong University, Institute of Geography & Planning, Yantai 264025, China
2.
Key laboratory of State Oceanic Administration for Marine Sedimentology & Environmental Geology, First Institute of Oceanography, State Oceanic Administration, Qingdao 266061, China
3.
Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China

Received Date: 2012-12-20
Publish Date: 2013-07-01

Abstract

Abstract

Based on ²¹⁰Pb data of 16 gravity core samples and from the previous study, the spatial pattern of sedimentation rates and its indication to distribution of Yangtze sediment supply in the Yangtze River estuary and its adjacent area were examined. The high accumulation rates were observed at the subaqueous delta off the south branch with the maximum value of 6.3cm/a, generally above 3cm/a. The second highest values distribute on the Hangzhou bay, about 1.7-3.0cm/a in north and much lower in south (0.4-1.0cm/a). Relative higher sedimentation rates, about 2.58cm/a, appear in the northwest of study area. The radial sand ridges along the north Jiangsu coastal line, delta-shelf transitional zone and continental shelf were characterized by low sedimentation rates (< 1cm/a), due to the strong hydrodynamic setting and lack of modern Changjiang material supply. As revealed by this study, a large amount of Yangtze sediment load is deposited around the subaqueous delta and the north Hangzhou Bay. The dispersion of modern Yangtze sediment to East China Sea is constrained to the west of 123°E. The relatively high sedimentation rate in north continental area is mainly contributed by sediment eroded from the abandoned Yellow delta and suspended materials transported by Yellow Sea longshore currents.
- Yangtze Estuary,
- ²¹⁰Pb,
- sedimentation rate,
- sediment supply,
- oceanography

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References(109)

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Sedimentation Rates and Its Indication to Distribution of Yangtze Sediment Supply around the Yangtze (Changjiang) River Estuary and Its Adjacent Area, China

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