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Study on the roughness coefficient of mountain gravel-bed rivers

机译:山区砾石河道糙率系数研究

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The bed slope of mountain river is relatively large, and the relationship between water depth and discharge is complex. Roughness coefficient is an important parameter in hydraulic calculations, how to choose the roughness coefficient is very important both in theoretical research and engineering calculations. Through flume experiments, we analyse the effects of hydraulic radius, water depth and discharge on the law of roughness coefficient. It is found that roughness coefficient is not a constant but changes with the water depth, we derive a new mountain gravel-bed river roughness coefficient formula according to the experiment results.
机译:山区河流床坡较大,水深与流量关系复杂。粗糙度系数是水力计算中的一个重要参数,如何选择粗糙度系数在理论研究和工程计算中都非常重要。通过水槽试验,我们分析了水力半径,水深和流量对粗糙度系数定律的影响。结果表明,粗糙度系数不是恒定的,而是随水深的变化而变化的,根据实验结果推导了新的山砾石床河流粗糙度系数公式。

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