| In-Situ Observation of Fluid Mud in the North Passage of Yangtze Estuary, China |
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| 引用本文： | 李九发 万新宁 何青 应铭 时连强 S.M.Hutchinson. In-Situ Observation of Fluid Mud in the North Passage of Yangtze Estuary, China[J]. 中国海洋工程, 2004, 18(1): 149-156 |
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| 作者姓名： | 李九发 万新宁 何青 应铭 时连强 S.M.Hutchinson |
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| 作者单位： | [1]StateKeyLaboratoryforEstuarineandCoastalResearch,EastChinaNormalUniversity,Shanghai200062,China [2]TelfordInstituteofEnvironmentalSystems,SchoolofEnvironmentandlifeSciences,UniversityofSalford,Salford,Gt.Manchester,M66PU,U.K. |
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| 基金项目： | ThisworkwassupportedbytheNationalNaturalScienceFoundationofChina (GrantNo .5 0 1790 12 ) |
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| 摘 要： | Observations of fluid mud were made in the lower North Passage of the Yangtze Estuary in February 2000, on 10 -11 August 2000, on 30 - 31 August 2000 (after two strong typhoons), on 21 - 24 August 2000 (neap tide) and on 3 -6 September 2000 (mean tide) respectively. In situ data show that the fluid mud in this area consists of fine cohesive sediment (median size 7.23 μm). The formation and movement of fluid mud varied during the neap-spring and flood-ebb tidal cycle. Observations suggest that fluid mud phenomena in this area may be categorised in a three-fold manner as slack water, storm and saltwedge features. The thickness of the fluid mud layer of slack water during the neap tide ranged from 0.2 to 0.96 m, whereas during the mean tide, the thickness ranged from 0.17 to 0.73 m, and the thickness of the fluid mud layer was larger during slack water than at the flood peak. Shoals cover an area of 800 km^2 with a water depth smaller than 5 m. Erosion of these extensive intertidal mudflats due to storm action provides an abundant sediment source. This is particularly significant in this estuary when the tidal level is lower than 5 m. The lower North Passage is a typical zone of saltwater wedging, so the saltwedge fluid mud has the most extensive spatial range in the estuary.
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| 关 键 词： | 流动性泥浆 扬子江 河口 沉积物 观测资料 |
In-Situ Observation of Fluid Mud in the North Passage of Yangtze Estuary, China |
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| LI Jiu-fa a,,WAN Xin-ning a,HE Qing a YING Ming a,SHI Lian-qiang a and S. M. Hutchinsonb a State Key Laboratory for Estuarine and Coastal Research,East China Normal University,Shanghai ,China b Telford Institute of Environmental Systems,School of Environment and Life Sciences,University of Salford,Salford,Gt. Manchester,M PU,U.K.. In-Situ Observation of Fluid Mud in the North Passage of Yangtze Estuary, China[J]. China Ocean Engineering, 2004, 18(1): 149-156 |
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| Authors: | LI Jiu-fa a WAN Xin-ning a HE Qing a YING Ming a SHI Lian-qiang a S. M. Hutchinsonb a State Key Laboratory for Estuarine Coastal Research East China Normal University Shanghai China b Telford Institute of Environmental Systems School of Environment Life Sciences University of Salford Salford Gt. Manchester M PU U.K. |
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| Affiliation: | LI Jiu-fa a,1,WAN Xin-ning a,HE Qing a YING Ming a,SHI Lian-qiang a and S. M. Hutchinsonb a State Key Laboratory for Estuarine and Coastal Research,East China Normal University,Shanghai 200062,China b Telford Institute of Environmental Systems,School of Environment and Life Sciences,University of Salford,Salford,Gt. Manchester,M6 6PU,U.K. |
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| Abstract: | |
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| Keywords: | fluid mud in situ observations north passage Yangtze Estuary China |
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