首页|1997-2019年长江口北槽地形演化特征及驱动机制

1997-2019年长江口北槽地形演化特征及驱动机制

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河口拦门沙位于河流和海洋的交界,具有弱动力、易沉积、水深浅的环境特征。打通拦门沙,建设深水航道一直是海洋学和工程学的一个难题,目前深水航道工程已经深刻地改变了拦门沙河槽的演化格局。本文根据北槽三期航道工程建设时间节点,收集了1997年、2002年、2007年和2019年北槽航道水下地形数据分析工程前后的地形演变特征,并结合航道工程建设、人为疏浚和外部环境变化等因素对北槽地形演变的驱动效应进行分析。结果表明:深水航道建设后长江口北槽主要出现了"槽冲滩淤"的河槽地形演化特征;空间上,北槽上段主要发生了北侧滩涂淤积,南侧航道侵蚀,而下段主要发生了南侧滩涂淤积,北侧航道侵蚀的演变格局。导堤和丁坝的建设是引起河槽"槽冲滩淤"的主要因素,而科氏力引起的涨、落潮流路变化也增加了河槽上下段的差异演化;深水航道工程建设是引起1997-2007年北槽淤积的主要驱动因素,而人为疏浚则是2007-2019年北槽侵蚀的主要影响因素;尽管人类活动已经成为北槽河槽演化的主要原因,但周围环境变化如流域来沙减少和海平面上升也加剧了近期的北槽侵蚀。
Characteristics and Driving Mechanisms of Terrain Evolution in the North Passage of the Yangtze River Estuary from 1997 to 2019
The estuarine sandbar is located at the junction of rivers and oceans,characterized by weak dynamics,easy sedimentation,and shallow water depth.Opening up sandbars and constructing deep-water channels have always been a challenge in oceanography and engineering.Currently,deep-water channel engineering has profoundly changed the evolutionary pattern of sandbar channels.This article collects underwater terrain data from 1997,2002.2007 and 2019 to analyze the characteristics of terrain evolution before and after the construction of the North Passage Phase Ⅲ waterway project.It also analyzes the driving effects of terrain evolution in the North Passage by combining factors such as waterway engineering construction,human dredging,and external environmental changes.The results show that after the construction of deep-water waterways,the North Passage of the Yangtze River Estuary mainly exhibits the characteristics of channel topography evolution,such as channel erosion,beach deposition,and sedimentation;In space,the upper section of the North Passage is mainly silted by the north mudflat and eroded by the south channel,while the lower section is mainly silted by the south mudflat and eroded by the North Passage.The construction of guide embankments and spur dikes is the main factor causing channel erosion and sedimentation,and the changes in the rising and falling tide paths caused by Coriolis forces also increase the differential evolution of the upper and lower sections of the channel;The construction of deep-water waterways was the main driving factor for sedimentation in the North Passage from 1997 to 2007,while human dredging was the main influencing factor for erosion in the North Passage from 2007 to 2019;Although human activities have become the main cause of the evolution of the North Passage,changes in the surrounding environment,such as reduced sediment from the basin and rising sea levels,have also intensified recent erosion in the North Passage.

north passage of the Yangtze River Estuarydeep water waterwayshuman activitiesdriving effect

黄小秋、陈晓红、徐健、李宇涵

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上海市地质调查研究院,上海 200072

长江上海航道处,上海 200010

上海市水务规划设计研究院/上海市海洋规划设计研究院,上海 200233

上海海洋大学海洋科学学院,上海 201306

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长江口北槽 深水航道 人类活动 驱动效应

上海市科委科研基金资助项目

21DZ1201700

2024

海洋技术学报
国家海洋技术中心

海洋技术学报

CSTPCD
影响因子:0.327
ISSN:1003-2029
年,卷(期):2024.43(3)