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工程科学与技术:2017,49(Z2):74-82
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三峡工程运用后上荆江枯水河槽调整及其对航道的影响
(武汉大学水资源与水电工程科学国家重点实验室)
Adjustments in low-water channel geometry and its effect on the navigation condition of the Upper Jingjiang Reach after the Three Gorges Project operation
(1.Whuhan university;2.State Key Laboratory of Water Resources and Hydrop)
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投稿时间:2016-08-24    修订日期:2016-12-27
中文摘要: 三峡工程运用后,上荆江河段河床冲刷较为剧烈,枯水(5000 m3/s流量下)河槽形态相应发生调整,对航运产生了较大影响。本文通过一维水动力学模型确定了各固定断面的枯水河槽形态参数。由于不同断面的河槽形态沿程存在显著差异,故采用基于对数转换的几何平均与断面间距加权平均相结合的河段平均方法,计算了2002-2015年上荆江河段尺度的枯水河槽形态参数。计算结果表明:受大范围护岸及护滩工程的影响,研究时段内上荆江枯水河槽宽度仅有小幅度增加,而相应的水深和面积增加约0.68 m及870 m2,增幅分别达12%及15%,航道条件总体上有所改善;枯水河槽宽深比呈持续减小趋势,由2002年的5.73减小至2015年的5.17,故近期上荆江枯水河槽形态趋于窄深;但在火箭洲、沙市及公安弯道等局部河段,江心洲或凸岸边滩的剧烈冲刷导致河槽展宽,宽深比明显增加,引起局部水深不足、航槽不稳定等现象。此外通过分析河槽形态调整对前期水沙条件的滞后响应,建立了河段尺度的枯水河槽形态参数与前6年平均的汛期水流冲刷强度之间的经验关系。结果表明:受人类活动干扰,上荆江河段尺度的枯水河槽宽度与前期水沙条件的相关程度较低,故建立的枯水河槽宽度公式不能反映水沙条件变化对河宽调整的影响;而上荆江河段尺度的枯水河槽水深、面积、宽深比与前6年平均的汛期水流冲刷强度的相关程度分别为0.92、0.95及0.85,故这三个参数均可较好地对由于三峡工程运用引起的水沙条件改变做出快速响应。
Abstract:Significant channel degradation has occurred along the Upper Jingjiang Reach (UJR) because of the operation of the Three Gorges Project (TGP), leading to the corresponding adjustments in low-water channel geometry. The section-scale low-water channel dimensions at each section in the UJR were first calculated by a one-dimensional hydrodynamic model. Due to the remarkable longitudinal variability in cross-sectional geometry, a reach-averaged method is adopted to calculate the reach-scale low-water channel dimensions in this reach annually from 2002 to 2015. Calculated results indicate that (i) the reach-scale low-water width changed slightly owing to the restriction of various river regulation engineering, and the corresponding depth and cross-sectional area respectively increased by 0.68 m and 870 m2, which led to a continuous decrease in the width-depth ratio from 5.73 in 2002 to 5.17 in 2015. Therefore, the low-water channel gradually developed into a narrow and deep shape in the UJR, with the low-water navigation condition being generally improved; (ii) however, the width-depth ratio at low water significantly increased in some subreaches such as the site of Huojianzhou, as well as the Shashi and Gongan bends. It is further explained that the central-bar and convex point-bar in these regions underwent dramatic degradation, which finally contributed to deteriorating the navigation condition. In addition, empirical relationships were developed between the reach-scale low-water channel dimensions and the previous flow and sediment regime. The results show that (i) the degree of correlation between the reach-scale low-water width and the previous flow and sediment regime was only 0.37, so the developed relationship cannot be applied to predict the variation in the low-water width; (ii) the reach-scale low-water depth, cross-sectional area and width-depth ratio correlated closely with the magnitude of the previous flow and sediment regime, with high correlation degrees of 0.92, 0.95 and 0.85 being obtained respectively. Therefore, these low-water channel dimensions can respond well to the altered flow and sediment regime caused by the TGP operation.
文章编号:201600844     中图分类号:    文献标志码:
基金项目:国家自然科学基金资助项目(51579186,51339001);国家重点研发计划课题(2016YFC0402303/05)
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引用文本:
周美蓉,夏军强,邓珊珊,林芬芬.三峡工程运用后上荆江枯水河槽调整及其对航道的影响[J].工程科学与技术,2017,49(Z2):74-82.
Zhou Meirong,Xia Junqiang,Deng Shanshan,Lin Fenfen.Adjustments in low-water channel geometry and its effect on the navigation condition of the Upper Jingjiang Reach after the Three Gorges Project operation[J].Advanced Engineering Sciences,2017,49(Z2):74-82.