首页|小浪底水库运用后黄河下游游荡段游荡程度变化特点及机理

小浪底水库运用后黄河下游游荡段游荡程度变化特点及机理

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为实现黄河下游游荡段游荡程度变化的定量评价,提出了游荡指数的计算方法;本文结合Landsat影像,分析了小浪底水库运用后游荡段游荡程度的变化特点及机理.研究表明,2000-2022年黄河下游游荡段整体游荡程度降低,游荡指数由0.918减至0.674,且游荡程度降低速率先快后慢.其中铁谢—伊洛河口河段和花园口—夹河滩河段游荡程度显著降低,伊洛河口—花园口河段游荡程度基本不变,夹河滩—高村河段游荡程度有所增加.此外,游荡段游荡特性演变与水沙、河床边界条件变化以及局部河势调整密切相关.从水沙条件来看,小浪底水库运用后黄河下游输沙锐减、洪峰调平,使得河道全线冲刷、流路集中,以致游荡段游荡特性减弱,且丰水年较枯水年更有利于河势归顺;从河床边界条件来看,沿程河岸约束性强的河段游荡特性趋于减弱,且河床纵向稳定性增加是游荡段游荡程度降低及降低速率减慢的因素之一;从局部河势调整的影响来看,朱寨—东坝头河段河势变化是夹河滩—高村河段后期切滩频发的重要原因.
Characteristics and mechanism of wandering intensity adjustments in a wandering reach of the Lower Yellow River after the operation of the Xiaolangdi Reservoir
To quantitatively explore the adjustments in the wandering intensity in a wandering reach of the Lower Yellow River(LYR)since the operation of the Xiaolangdi(XLD)Reservoir,the calculation method of a new wandering index(WI)was proposed.In addition,Landsat images were collected to perform an analysis of the spatio-temporal variations in the wandering intensity and their response to major influencing factors.The results indicate that the wandering intensity in the wandering reach integrally presented a decreasing trend during the period from 2000 to 2022,with the value of WI decreasing from 0.918 to 0.674 and changing rate being fast to slow.Specifically,the wandering intensity in the Tiexie-Yiluohekou reach and Huayuankou-Jiahetan reach has decreased,while the Yiluohekou-Huayuankou reach maintained and the Jiahetan-Gaocun reach increased.Furthermore,the wandering intensity adjustments had close relations to the flow-sediment regime,riverbed boundary conditions and local river regime evolution.For flow and sediment regime,the decrease of wandering intensity in the wandering reach was significantly attributed to the sharp reduction in the incoming sediment volume and rising-recession rate of floods in the LYR owing to the operation of XLD Reservoir,which resulted in the riverbed erosion and flow concentration in the downstream channel.Regarding riverbed boundary conditions,the wandering intensity in the sub-reaches with strong lateral restrict caused by banks or channel regulation works tended to decrease.Also,the increase in the longitudinal stability of the riverbed was one of the reasons why the wandering intensity in the wandering reach declined with a slower changing rate in the later stage.Concerning about propagation of river regime adjustments,the frequent occurrence of avulsion in the Jiahetan-Gaocun reach during the later period was mainly attributed to the river regime evolution in the inlet reach between Zhuzhai to Dongbatou.

wandering intensityspatio-temporal variationsevolution mechanismwandering indexLandsat imageLower Yellow River

刘雨晨、夏军强、周美蓉、程亦菲

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武汉大学水资源工程与调度全国重点实验室,武汉 430072

游荡程度 时空变化 演变机理 游荡指数 Landsat影像 黄河下游

国家自然科学基金国家自然科学基金

U2243238U2243237

2024

地理学报
中国地理学会 中国科学院地理科学与资源研究所

地理学报

CSTPCDCSSCICHSSCD北大核心
影响因子:3.3
ISSN:0375-5444
年,卷(期):2024.79(5)
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