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Transport and Deposition of River Sediment in the Changjiang Estuary and Adjacent Continental Shelf

机译：长江口及邻近大陆架河流沉积物的迁移与沉积

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Hydrographic observations, suspended-sediment measurements, and historical data indicate transport paths and sinks for sediment within the Changjiang estuary and adjacent shelf. Most of the sediment transported by the Changjiang to the ocean is carried through the North Channel of the South Branch. Sediment transport is directly related to river stage, but tidal phase (spring vs neap tides) also plays an important role. An estimated 40% of the sediment load in the river is deposited in the estuary, mostly in and seaward of the South Channel. The remaining sediment is deposited directly offshore during flood seasons, but much is resuspended and carried southward by subsequent winter storms. (Author)

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Milliman, J. D.; Chen, H. T.; Yang, Z. S.; Meade, R. H.;
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年度 1985
页码 p.1-13
总页数 13
原文格式 PDF
正文语种 eng
中图分类工业技术;
关键词
Sediment transport; Sedimentation; China; Rivers; Estuaries; East china sea; Floods; Seasons; Channels; North(Direction); Sediments; Paths; Transport; Deposition; Hydrography; Observation; Oceans; Tides; Winter; Continental shelves; Storms; Reprints;

机译：泥沙运输;沉积;中国;河流;河口;东海;洪水;季节;渠道;北（方向）;沉积物;路径;运输;沉积;水文;观测;海洋;潮汐;冬季;大陆架;风暴;重印;

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Transport and Deposition of River Sediment in the Changjiang Estuary and Adjacent Continental Shelf

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