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      长江中游周天河段河床演变与航道条件变化分析

      Analysis of Shoal-Channel Evolution and Navigation Conditions in Zhou-Tian Reach of the Middle Yangtze River

      • 摘要: 以长江中游周天河段为研究对象,基于实测水文与地形数据,分析了荆江一期整治工程实施后的滩槽演变特征与航道条件变化。结果表明:2022年3月至2024年5月期间,九华寺边滩头部略有上提,对岸侧戚家台边滩相对稳定;周公堤心滩和蛟子渊边滩的右缘冲淤交替变化,蛟子渊边滩尾部右缘略有后退;新厂边滩的形态基本稳定,天兴洲头部左缘冲刷后退。周天河段进口九华寺边滩区域的水深4.5 m的河槽槽贯通,航槽形态相对稳定;颜家台区域水深4.5 m河槽平面形态存在一定的变化;覃家洲至草房关区域左岸侧存在水深不足4.5 m的沙舌深入河槽,蛟子渊边滩尾部区域也存在4.5 m的沙舌深入河槽,形成了交错形式的水深4.5 m河槽;天星洲水道水深4.5 m河槽贯通,胡汾沟区域的小型沙舌进入河道,陀阳树边滩区域的航道边界存在一定幅度的摆动,不利于航道边界条件的稳定。

         

        Abstract: Taking the Zhou-Tian reach in the middle Yangtze River as the study object, this research analyzes the evolution characteristics of shoals and channels along with navigation conditions changes after the first-phase Jingjiang regulation project, based on measured hydrological and topographic data. Key findings from March 2022 to May 2024 include: The Jiuhuasi fluvial bar showed slight upstream advancement at its head and variations at its tail, while the Qijiatai bar on the opposite bank remained stable.The Zhougongdi central bar and Jiaoziyuan bar exhibited alternating erosion-deposition patterns along their right margins, with minor retreat observed at the tail of Jiaoziyuan bar.The Xinchang bar maintained morphological stability, while the left margin of Tianxingzhou head experienced erosion.Navigation channel observations revealed: A continuous 4.5-meter-deep channel formed at the entrance (Jiuhuasi area) with stable morphology.The Yanjiatai area showed planar morphological variations in its 4.5m channel.Sand tongues (<4.5m depth) intruded into main channels near Tanjiazhou-Caofangguan (left bank) and Jiaoziyuan bar tail, creating interlaced 4.5m channels.While Tianxingzhou waterway maintained continuous 4.5m channels, small sand tongues near Hufengou and boundary fluctuations at Tuoyangshu bar adversely affected navigation stability.

         

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