长江口2002—2019年滩涂演变分析
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Tidal flat evolution in Yangtze River Estuary from 2002 to 2019
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    摘要:

    在长江流域输沙量大幅度减少的背景下,基于实测地形资料分析三峡工程运行前后长江口滩涂的总体变化,其存在高滩增加,中、低滩均减小的趋势。对长江口滩涂与涉水工程的关系归纳为4类,其中基本圈围成陆的滩涂,高、中、低滩面积均大幅减小;建有工程的滩涂,总体表现为高滩增加,中滩减小多,低滩减小少的现象;受周边工程影响的滩涂,滩涂演变与工程的相对位置及滩涂所处的河势与水文泥沙条件等有关;而基本处于自然演变的滩涂,则表现为高滩增加、中滩和低滩减小的演变特征。结果表明,流域来沙减少是长江口滩涂演变的驱动因素,具有范围大、周期长、变化缓慢的特征;而人类活动是长江口滩涂演变的触发因素,具有局部、周期短、变化剧烈的特征。

    Abstract:

    Since the sediment runoff in the Yangtze River Basin has greatly decreased,this study analyzes the general changes in tidal flats in Yangtze River Estuary before and after the operation of the Three Gorges project based on the measured topographic data and finds that the high tidal flats increase,while the medium and low tidal flats decrease.The relationship between tidal flats in Yangtze River Estuary and wading engineering can be divided into four categories.Specifically,in terms of tidal flats that have been enclosed,the areas of high,medium,and low tidal flats are greatly reduced.In terms of tidal flats with built projects,the high tidal flats increase.The medium tidal flats decrease greatly,and the low tidal flats decrease slightly.In terms of tidal flats affected by surrounding projects,the evolution of the tidal flats is related to the relative position of the projects,the river regime of the tidal flats,and hydrologic and sediment conditions.In terms of tidal flats undergoing natural evolution,the high tidal flats increase,and the medium and low tidal flats decrease.The results show that the reduction of sediment inflow in the basin is the driving factor of the tidal flat evolution in Yangtze River Estuary,which has the characteristics of large range,long period,and slow change.However,human activities are the factors triggering the evolution of the tidal flats in Yangtze River Estuary,which have the characteristics of local range,short period,and drastic change.

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张东来,宋 磊.长江口2002—2019年滩涂演变分析[J].水运工程,2023(6):137-143.

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  • 在线发布日期: 2023-06-13
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