Dam-break flood evolution in downstream reservoir and runup in front of dam
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TV122.4

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    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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  • Online: March 21,2019
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