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三峡建库后洞庭湖入汇对下荆江顶托特征的变化分析OA

Changes in the backwater effect of Dongting Lake inflows on the Lower Jingjiang River after the impoundment of the Three Gorges Reservoir

中文摘要英文摘要

厘清三峡建库后洞庭湖对下荆江顶托的新特征是当前的重要问题.针对江湖交汇点上游的监利至城陵矶河段,引入Copula函数研究不同时期的江湖汇流遭遇特征;基于冲积河流水流运动规律提出平衡态下的江湖流量搭配关系,构建干流受顶托强度的评估指标,在此基础上定量分析了三峡建库前后下荆江受顶托事件的发生几率、出现时机以及年内不同时期的顶托强度变化.研究表明,平衡态下的江湖流量搭配为非线性函数关系,该关系与江湖流量之间的多年平均拟合线相近,可用于判别干流的顶托或消落状态.三峡建库后,监利流量处于中枯水量级的历时增长,导致干流与湖泊汇流均为中枯水的遭遇概率增幅为 44.6%,干流中水与湖泊汇流为洪水(大于30 000m3/s)的遭遇概率增幅为5.4%.受其影响,江湖汇流点的侵蚀基准面降低,并且年尺度上湖区对干流的平均顶托强度减弱,但干流处于顶托态的时机由平滩以上流量级向中水流量级转移,4-7月份出现远大于历史同期顶托强度的极端情况增多,需引起长期关注.

Clarifying the new characteristics of Dongting Lake's backwater effect on the lower Jingjiang River after the impoundment of the Three Gorges Reservoir is a critical issue at present.Focusing on the river section from Jianli to Chenglingji upstream of the confluence between the river and the lake,Copula functions were employed to investi-gate the characteristics of flow coincidences between the river and the lake in different periods.Based on the flow dynamics of alluvial rivers,a balanced-state flow pairing relationship was proposed,and an index for assessing the backwater intensity of the mainstream was developed.On this basis,the occurrence probability and timing of backwa-ter events as well as the variation of backwater intensity during different periods within a year for the lower Jingjiang River before and after the impoundment of the Three Gorges Reservoir were quantitatively analyzed.The results indi-cate that,under the balanced state,the flow pairing between the river and the lake follows a nonlinear functional rela-tionship.This relationship is close to the long-term mean fitted line of river-lake discharges and can be used to deter-mine whether the mainstream is in a backwater or drawdown state.After the impoundment of the Three Gorges Reser-voir,the duration of Jianli discharges at the medium-low flow level increased,resulting in a 44.6%rise in the coinci-dence probability of both the mainstream and lake inflows being at medium-low flow.The coincidence probability of the mainstream at medium flow and lake inflows at flood level(exceeding 30,000 m³/s)increased by 5.4%.As a result,the erosional base level at the river-lake confluence decreased,and on an annual scale,the mean backwater intensity of the lake on the mainstream weakened.However,the timing of the mainstream being in a backwater state shifted from above-bankfull flow levels to medium flow levels.The occurrence of extreme backwater intensity far exceeding the historical values during April-July has increased,warranting long-term attention.

李芷晴;孙昭华;陈立;安姗姗;周炜兴

武汉大学 水资源工程与调度全国重点实验室,湖北 武汉 430072||长江勘测规划设计研究有限责任公司,湖北 武汉 430010||流域水安全保障湖北省重点实验室,湖北 武汉 430010武汉大学 水资源工程与调度全国重点实验室,湖北 武汉 430072武汉大学 水资源工程与调度全国重点实验室,湖北 武汉 430072武汉大学 水资源工程与调度全国重点实验室,湖北 武汉 430072武汉大学 水资源工程与调度全国重点实验室,湖北 武汉 430072

建筑与水利

三峡水库下荆江洞庭湖流量遭遇回水顶托

Three Gorges Reservoirlower Jingjiang RiverDongting Lakeflow encounterbackwater effect

《水利学报》 2026 (5)

767-781,15

国家自然科学基金项目(52479074)水利部三峡后续研究项目(12630100100020J005)

10.3724/j.slxb.20250601

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