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    黄土丘陵区坝系拓扑结构对极端洪水级联风险的调控机制

    Regulation mechanism of dam system topology on extreme flood cascade risk in the Loess Hilly Region

    • 摘要: 在极端暴雨频发的背景下,黄土丘陵区大量老旧淤地坝因溢洪设施缺失与坝体老化,面临极高的溃坝风险。然而,现有研究多聚焦单坝失稳过程,对坝系尺度洪水级联传播机制及“拦沙效益—防洪安全”库容竞争关系关注不足。以宁夏西吉县车路沟典型并联坝系为研究对象,基于MIKE11、MIKE21耦合模型模拟300年一遇极端暴雨条件下坝系洪水传播与溃决演化过程,解析并联拓扑结构对级联风险的调控机制;结合层次分析法(AHP)与淤积预测模型,系统评估坝系布局合理性及长期防洪能力演化特征。结果表明:①300年一遇极端暴雨条件下,流域内4座骨干坝发生漫顶溃决,但受并联拓扑结构与沟道地形共同作用,溃坝洪水主要沿支沟纵向传播,未形成跨单元级联放大;洪峰过程呈现明显错峰特征,主沟最大淹没水深为7.25 m。坝体局部失稳虽导致单元内洪水风险增加,但未诱发全流域连锁溃决,表明并联坝系具有较强的风险阻断能力。②坝系布局综合评价得分为0.84,总体处于“合理”等级,其中安全性达0.96,而效益性仅为0.29,表明坝系整体具备较强的洪水风险阻断能力,但坝地资源开发利用程度较低,仍处于“拦沙—成地”效益转化滞后阶段。③随着泥沙持续淤积与库区蓄水占用,坝系有效防洪库容将持续衰减,拦沙淤地过程与防洪调蓄功能之间存在显著的库容竞争关系,该竞争效应将导致坝系长期防洪安全裕度逐步降低。研究可为黄土高原老旧坝系风险防控、库容管理与布局优化提供理论依据。

       

      Abstract: Under the increasing occurrence of extreme rainstorms, numerous aging check dams in the Loess Hilly Region are facing substantial failure risks due to the absence of spillway facilities and long-term structural aging. However, previous studies have primarily focused on the instability of individual dams, while insufficient attention has been paid to flood cascade propagation mechanisms at the dam-system scale and the storage-capacity trade-off between sediment retention benefits and flood-control safety. Taking the typical parallel dam system in Chelugou Watershed, Xiji County, Ningxia, China, as a case study, this research employed a coupled MIKE11/21 hydrodynamic model to simulate flood propagation and dam-breach evolution under a 300-year return-period extreme rainfall event, analyzing the regulatory mechanism of parallel topology structure on cascade risk. In addition, the Analytic Hierarchy Process (AHP) and a sedimentation prediction model were integrated to evaluate the rationality of dam-system layout and the long-term evolution of flood-control capacity. The results indicate that: ① four key check dams experienced overtopping failures under the 300-year return-period rainfall scenario. Nevertheless, constrained by the combined effects of parallel topology and gully geomorphology, breach floods propagated mainly along individual tributaries without triggering cross-unit cascade amplification. Flood peaks exhibited pronounced temporal staggering, and the maximum inundation depth in the main channel reached 7.25 m. Although local dam failures increased flood hazards within individual sub-units, no basin-wide chain failure occurred, demonstrating the strong risk-blocking capability of the parallel dam system. ② The comprehensive layout evaluation score of the dam system was 0.84, overall at a "reasonable" level. The safety score reached 0.96, whereas the benefit score was only 0.29, indicating that the degree of development and utilization of dam resources is relatively low, and it is still in the stage of lagging behind in the transformation of benefits from "sand interception to land formation". ③ Continuous sediment deposition and reservoir occupation progressively reduce the effective flood-control storage capacity. A significant storage-capacity competition exists between sediment retention and flood regulation functions, which may gradually diminish the long-term flood-safety margin of the dam system.The findings provide scientific support for risk management, storage-capacity regulation, and layout optimization of aging check-dam systems on the Loess Plateau.

       

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