| 特大洪水期间长江口浑浊带分粒级输沙特征 |
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| 引用本文： | 朱春燕,董坚,谢卫明,郭磊城,何青.特大洪水期间长江口浑浊带分粒级输沙特征[J].海洋通报,2024(3). |
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| 作者姓名： | 朱春燕 董坚 谢卫明 郭磊城 何青 |
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| 作者单位： | 华东师范大学河口海岸学国家重点实验室，上海 200241 |
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| 基金项目： | 国家自然科学基金（U2040216, 42206169）；中国博士后科学基金项目（2022M721165, 2023T160219）；上海市科委重点项目（20DZ1204701, 21230750600）；上海市浦江人才计划（22PJD020） |
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| 摘 要： | 基于2020年7月特大洪水期间长江口浑浊带南槽、北槽和北港多站位同步实测水沙动力数据，研究了河口浑浊带分粒级输沙时空特征及其对泥沙来源响应的指示意义，结果表明：1）北港和北槽是流域泥沙净向口外输移的主要输沙通道，南槽是海域泥沙净向口内输移的主要输沙通道，主槽内粉砂是主要输沙组分，占比63.2%，口外粉砂和黏土是主要输沙组分，分别占43.2%、40.9%；2）大潮粉砂输运占比高于小潮，黏土输运占比低于小潮，口外测站砂组分在大小潮期间在横沙浅滩和九段沙间沿岸输移，横沙浅滩附近大、小潮离岸输沙分别是北港口外的1.7倍和8倍，不利于横沙浅滩淤涨；3）当前流域减沙高达70%，此次特大洪水期间黏土、粉砂和砂三组分近底净向口内输移为减沙背景下的口外供沙提供了有力的佐证。
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| 关 键 词： | 长江口 浑浊带 特大洪水 分粒级输沙 泥沙来源 流域减沙 |
| 收稿时间： | 2023/8/8 0:00:00 |
| 修稿时间： | 2023/9/12 0:00:00 |
Multi-fraction sediment transport in the turbidity maximum of the Yangtze Estuary during the extreme flood |
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| ZHU Chunyan,Dong Jian,XIE Weiming,GUO Leicheng,HE Qing.Multi-fraction sediment transport in the turbidity maximum of the Yangtze Estuary during the extreme flood[J].Marine Science Bulletin,2024(3). |
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| Authors: | ZHU Chunyan Dong Jian XIE Weiming GUO Leicheng HE Qing |
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| Institution: | State Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai 200241, China |
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| Abstract: | The multi-fraction sediment transport in the turbidity maximum of the Yangtze Estuary was studied based on the data collected under the extreme flood in July 2020. It aims to exhibit the spatial and temporal changes in the multi-fraction sediment transport over a spring-neap tide and identify the effect of the changes in sediment supply. The results show that: 1) the North Channel and North Passage are the main channels for net seaward sediment transport delivering fluvial sediment whereas the South Passage is the main channel for net-transporting offshore sediment. The main channel transports 63.2% silt fraction whereas offshore sediment transport indicates 43.2% and 40.9% of the fractions silt and clay, respectively. 2) Silt fraction transport is higher at spring tide than that at neap tide whereas clay fraction transport is lower at spring tide than that at neap tide. The location of sand accumulation moves between seaward of Hengsha flat and Jiuduan shoal over a spring-neap tidal cycle. Moreover, offshore sediment transport is 1.7 and 8 times larger than alongshore sediment transport at spring and neap tides, respectively at Hengsha flat which suppress the accretion of the tidal flat. 3) As fluvial sediment supply has reduced by 70%, the net landward sediment transport in the South Passage implies that offshore sediment supply plays an important role, which needs to be considered in the future study. |
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| Keywords: | Yangtze Estuary turbidity maximum extreme flood multi-fraction sediment transport sediment source reduced fluvial sediment supply |
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