推移质翻越低坝输移特性的试验研究

TV142.2; 对于山区河流低坝而言,平时淤积在坝前的推移质粗沙可能会在洪水期集中翻越坝顶,形成高强度输沙.本文开展水槽试验,研究推移质粗沙自上游起动、推进、再翻越坝顶后向下游输移的过程,分析了输沙参数的变化特性及数理规律,描述了翻坝输沙模式及运动特征,揭示了输沙规律与河床形态之间的自然联系.取得如下认识:①输沙量随时间大致以幂函数规律增长.②低坝附近区域河床形态终将趋于稳定,上游和下游均形成相对稳定的曲面斜坡淤积体.③在不同的水流强度下推移质翻坝输移模式存在差异.对于一般水流强度工况,上游淤积体曲面斜坡表面泥沙颗粒以滚动或滑动模式起动,推移至接近坝顶位置时再跃移翻坝,后向下游输移;对于更高...

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Published in水科学进展 Vol. 31; no. 3; pp. 356 - 365
Main Authors 晏自立, 徐元, 李丹勋
Format Journal Article
LanguageChinese
Published 清华大学水沙科学与水利水电工程国家重点实验室,北京,100084 30.05.2020
Subjects
Online AccessGet full text
ISSN1001-6791
DOI10.14042/j.cnki.32.1309.2020.03.005

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Abstract TV142.2; 对于山区河流低坝而言,平时淤积在坝前的推移质粗沙可能会在洪水期集中翻越坝顶,形成高强度输沙.本文开展水槽试验,研究推移质粗沙自上游起动、推进、再翻越坝顶后向下游输移的过程,分析了输沙参数的变化特性及数理规律,描述了翻坝输沙模式及运动特征,揭示了输沙规律与河床形态之间的自然联系.取得如下认识:①输沙量随时间大致以幂函数规律增长.②低坝附近区域河床形态终将趋于稳定,上游和下游均形成相对稳定的曲面斜坡淤积体.③在不同的水流强度下推移质翻坝输移模式存在差异.对于一般水流强度工况,上游淤积体曲面斜坡表面泥沙颗粒以滚动或滑动模式起动,推移至接近坝顶位置时再跃移翻坝,后向下游输移;对于更高水流强度工况,后期的翻坝输沙模式可能发生显著转变,周期性边壁漩涡成为翻坝输沙的主要动力来源.
AbstractList TV142.2; 对于山区河流低坝而言,平时淤积在坝前的推移质粗沙可能会在洪水期集中翻越坝顶,形成高强度输沙.本文开展水槽试验,研究推移质粗沙自上游起动、推进、再翻越坝顶后向下游输移的过程,分析了输沙参数的变化特性及数理规律,描述了翻坝输沙模式及运动特征,揭示了输沙规律与河床形态之间的自然联系.取得如下认识:①输沙量随时间大致以幂函数规律增长.②低坝附近区域河床形态终将趋于稳定,上游和下游均形成相对稳定的曲面斜坡淤积体.③在不同的水流强度下推移质翻坝输移模式存在差异.对于一般水流强度工况,上游淤积体曲面斜坡表面泥沙颗粒以滚动或滑动模式起动,推移至接近坝顶位置时再跃移翻坝,后向下游输移;对于更高水流强度工况,后期的翻坝输沙模式可能发生显著转变,周期性边壁漩涡成为翻坝输沙的主要动力来源.
Author 晏自立
徐元
李丹勋
AuthorAffiliation 清华大学水沙科学与水利水电工程国家重点实验室,北京,100084
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YAN Zili
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Keywords 推移质
挟沙力
输沙率
输移特性
径流式低坝
河床形态
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Snippet TV142.2; 对于山区河流低坝而言,平时淤积在坝前的推移质粗沙可能会在洪水期集中翻越坝顶,形成高强度输沙.本文开展水槽试验,研究推移质粗沙自上游起动、推进、再翻越坝顶后向...
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Title 推移质翻越低坝输移特性的试验研究
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