长江上游龙门水道河床演变及碍航原因分析
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River evolution and navigation obstacle property in Longmen waterway in the upper Yangtze River
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    摘要:

    龙门水道为长江上游重点碍航河段,兼具浅险滩和急流滩的特点。采取实测资料研究该河段近期水沙特性,以及岸线、深泓和典型断面等变化,分析龙门水道碍航原因。结果表明,龙门水道平面形态稳定,岸线和深槽位置变化很小,年际间冲淤交替。在上游水库蓄水等的影响下,来沙量减少,枯水河槽小幅冲刷。弯道段洪、枯河宽差距较大,汛期易在凸岸形成碍航浅滩;中、枯水流量下,大河村丁顺坝束水形成急流滩,弯顶右岸石梁头部的复杂流态与左岸漫滩斜流综合作用形成险滩。

    Abstract:

    Longmen waterway is the key impeding navigation channel due to its shallow,chaos and rapids flow.Based on recent field investigation data,the flow-sediment property,variation of depth contour,thalweg and typical cross sections were studied,navigation obstruction was analyzed.Results show in 2007—2015,plane form of Longmen waterway was steady;shoal lines changed a little,river bed scoured and silt alternatively.Affected by upstream reservoir,decreased incoming sediment led to slight erosion in low channel.Large difference between flood and dry river width resulted in siltation in bend convex bank,in middle and low water flow,rapids flow appeared neighbouring Dahe spur dike,and chaos flow formed nearby the head of Longmen rock spur.

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闫 涛,张 明,普晓刚,等.长江上游龙门水道河床演变及碍航原因分析[J].水运工程,2017(3):110-115.

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  • 在线发布日期: 2017-03-16
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