异化水沙条件下汉江游荡段航道整治研究
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Channel regulation in wandering reach of Hanjiang River under altered flow-sediment regimes
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    摘要:

    自丹江口水库蓄水后,汉江中下游游荡河段水沙条件发生显著异化,导致航道条件稳定性变差。基于多年水库蓄水数据及碾盘山(沿山头坝址)—郑金庙河段全长110 km的实测地形资料,系统分析该河段水沙特性变化规律、滩险碍航特点及演变趋势。结果表明,1988—2012年该河段狮子口滩段累积冲刷量达1 272.35万m3,伴随平滩河槽持续展宽、主河槽最大刷深约10 m,且边滩与心滩冲淤频繁,撇弯切滩、汊道交替演变现象突出,洲滩变化剧烈。受此影响,航道条件极不稳定,航槽易变且碍航问题严峻。针对性提出固滩护岸与中低水整治协同的治理原则和整治参数确定方法,明确445 m3/s作为碾盘山枢纽下游设计最低通航流量。

    Abstract:

    Since the Danjiangkou Reservoir impoundment,flow and sediment conditions in the wandering reach of the Hanjiang River’s middle and lower reaches have changed significantly,weakening waterway stability.On the basis of long-term reservoir impoundment data and measured topographic data of the 110 km reach from Nianpanshan (Yanshantou Dam site) to Zhengjinmiao,we systematically analyze the variation patterns of flow-sediment characteristics,evolution trends of shoals,and navigation obstruction features in this reach.The results show that from 1988 to 2012,the Shizikou shoal section has a cumulative scouring volume of 12.7235 million m3,with the bank-full channel widening,the main channel scouring up to 10 m deep.Meanwhile,the side bars and mid-channel bars experiences frequent erosion and deposition;the phenomena of cutoff and alternating evolution of branched channels are prominent,leading to drastic changes in the shoals and bars.This makes waterway conditions extremely unstable,with frequent navigation channel shifts and severe hindrances.Accordingly,governance principles combining bar stabilization-bank protection with medium-low flow regulation are proposed,with a method to determine regulation parameters.The minimum designed navigable discharge downstream of the Nianpanshan Hydro-junction is determined as 445 m3/s.

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漆炼勇,李求生,杨宇平.异化水沙条件下汉江游荡段航道整治研究[J].水运工程,2026(3):191-198.

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  • 在线发布日期: 2026-03-24
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