溃坝洪水在下游水库的演进及坝前爬高
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TV122.4

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国家自然科学基金(51409123)


Dam-break flood evolution in downstream reservoir and runup in front of dam
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    摘要:

    基于物理模型试验,探讨上游坝体溃决时间T1上游坝前水深H1上游水库面积S1下游坝前水深H2及下游水库面积S2等因素对溃坝洪水在下游水库演进初始波高及下游坝前初始波浪爬高的影响结果表明:溃坝洪水在下游水库的演进过程可分为洪水波洪水涌浪反射叠加振荡衰减4个阶段下游坝前初始波浪爬高随T1、H2、S2的增大而减小H1的增加而增大与上游水库面积S1无明显相关关系拟合出下游坝前初始波浪爬高值经验公式并得出各因素对波浪初始爬高影响程度从大到小的次序为:T1、S2、H1、H2

    Abstract:

    Factors including the upstream dam breaking time T1, water depths in front of the upstream dam H1 and downstream dam H2, upstream reservoir area S1 and downstream reservoir area S2 that can influence the dam-break flood evolution in the downstream reservoir, the initial flood wave height and the initial runup height in front of the downstream dam, are discussed based on physical model tests. The results show that, the evolution process of a dam break flood in the downstream reservoir can be divided into four stages: flood wave forming, flood surging, reflection superposition and oscillation attenuation. The initial runup height of the flood wave in front of the downstream dam decreases with the increase of T1, H2, and S2, while increases with H1, but it has no obvious correlation with the upstream reservoir area S1. In addition, the empirical formula of the initial wave height in front of the downstream dam is proposed, and the influence degree of each factor on the initial wave runup height from high to low is obtained in the following order: T1, S2, H1, and H2.

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谭箐,王晓刚,刘火箭,等.溃坝洪水在下游水库的演进及坝前爬高[J].水利水电科技进展,2019,39(2):26-30.(TAN Qing, WANG Xiaogang, LIU Huojian, et al. Dam-break flood evolution in downstream reservoir and runup in front of dam[J]. Advances in Science and Technology of Water Resources,2019,39(2):26-30.(in Chinese))

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  • 在线发布日期: 2019-03-21