基于二维水动力模型的溃坝洪水模拟研究OA
Simulation of dam-break flooding based on a two-dimensional hydrodynamic model:a case study of Huoshishan Reservoir in Biyang County,Zhumadian City,Henan Province
针对水库大坝溃决后洪水突发性强、破坏力大的特点,探明溃坝洪水的传播与淹没规律,是防灾减灾和编制避险预案的重要基础.本文以河南省驻马店市泌阳县火石山水库为研究对象,构建GPU加速的二维水动力模型,与逐渐溃坝计算模型耦合模拟溃口逐步扩展过程,并将溃坝出流与溢洪道泄流叠加作为入流边界.选取设计洪水、校核洪水、超坝顶高程洪水3种工况,模拟下游平原区溃坝洪水演进过程,量化分析淹没范围、水深分布与洪峰传播特征.结果表明:超坝顶高程洪水工况下,溃坝洪水呈"急涨—单峰—缓退"的态势,淹没水深呈"浅水漫滩—水深增大—深水主导—浅水滞退"的动态演化过程,溢洪道预泄与土石坝逐渐溃决模式可削减溃坝洪峰.洪水向下游传播时起涨与峰现时刻依次推迟,洪峰沿程衰减,淹没历时缩短,距坝最近的春水镇九里岗村淹没水深最大、受淹时间最长、风险最高.随上游来水条件从设计洪水升级至超坝顶洪水,下游淹没面积由2.86 km2增至7.76 km2,最大淹没水深由6.67 m升至10.65 m,水深大于3.0 m的深水区面积占比由6.3%升至30.9%,致灾程度逐步加剧.
In view of the abrupt onset and high destructive power of floods following dam failure,clarifying the propagation and inundation patterns of dam-break floods is an important basis for disaster prevention and mitigation and for formulating emergency evacuation plans.Taking the Huoshishan Reservoir in Biyang County,Zhumadian City,Henan Province,as the study object,a GPU-accelerated two-dimensional hydrodynamic model was constructed and coupled with a gradual dam-break calculation model to simulate the progressive expansion of the breach.The dam-break outflow was superimposed on the spillway discharge to form the inflow boundary.Three scenarios—the design flood,the check flood,and the flood exceeding the dam crest elevation—were selected to simulate the routing of dam-break floods in the downstream plain area,and the inundation extent,water depth distribution,and flood-peak propagation characteristics were quantitatively analyzed.The results show that under the scenario of the flood exceeding the dam crest elevation,the dam-break flood exhibits a pattern of"rapid rise—single peak—gradual recession",and the inundation depth undergoes a dynamic evolution of"shallow-water overbank spreading—increasing water depth—deep-water dominance—slow recession of shallow water".The spillway pre-release and the gradual breaching mode of the earth-rockfill dam can reduce the dam-break flood peak.As the flood propagates downstream,the onset of rise and peak occurrence are successively delayed,the peak attenuates along the routing path,and the inundation duration shortens.Jiuligang Village in Chunshui Town,located closest to the dam,experiences the greatest inundation depth and the longest inundation duration,and thus has the highest risk.As the upstream inflow condition escalates from the design flood to the flood exceeding the dam crest,the downstream inundation area increases from 2.86 to 7.76 km2,the maximum inundation depth rises from 6.67 to 10.65 m,and the proportion of deep-water areas with water depths greater than 3.0 m increases from 6.3%to 30.9%,indicating progressively increasing hazard severity.
王韫策;冷艳杰;臧文斌;孙伊博;刘世昆;阚光远
中国水利水电科学研究院,100038,北京||北京中水科工程集团有限公司,100048,北京中国水利水电科学研究院,100038,北京中国水利水电科学研究院,100038,北京||水利部防洪抗旱减灾技术创新中心(水旱灾害防御中心),100038,北京黄河水文勘察测绘局,450040,郑州中国水利水电科学研究院,100038,北京||水利部防洪抗旱减灾技术创新中心(水旱灾害防御中心),100038,北京中国水利水电科学研究院,100038,北京
建筑与水利
溃坝洪水模拟逐渐溃坝计算模型二维水动力模型洪水模拟淹没分析火石山水库
dam-break flood simulationgradual dam-break calculation modeltwo-dimensional hydrodynamic modelflood simulationinundation analysisHuoshishan Reservoir
《中国水利》 2026 (18)
61-70,10
国家重点研发计划项目(2023YFC3209202).
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