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Determination of friction factor for rivers with non-submerged vegetation in banks and floodplains

机译:岸滩漫滩非淹没河流摩擦系数的确定

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Due to vegetation flexibility, friction factor varies in flood plains and river banks and is a function of vegetation characteristics and flow conditions. Study of river behavior and effect of vegetation on river systems are very important for water intake in pumping stations, water treatment plans and wastewater and construction of structures such as bridges and diversion channels. Purpose of this research is to develop a relationship for estimation of non-submerged vegetation roughness in the flood plains and river banks. Number of 182 experiments was conducted on a laboratory flume and effect of parameters on the roughness coefficient was evaluated.Results show a nonlinear decrease of roughness coefficient with increasing of flow rate. Increase of velocity from 0.2 to 2 m/s make Manning’s coefficient reduces to about 30% of the first case. Decrease of roughness coefficient with decrease of submergence ratio and density was low compared to the velocity effect.
机译:由于植被的柔韧性,摩擦系数在洪泛区和河岸中变化,并且是植被特征和流量条件的函数。研究河流行为和植被对河流系统的影响对于泵站的取水,水处理计划和废水以及桥梁和引水渠等结构的建设非常重要。这项研究的目的是建立一种估算洪泛平原和河岸非淹没植被粗糙度的关系。在实验室水槽上进行了182次实验,评估了参数对粗糙度系数的影响。结果表明,随着流速的增加,粗糙度系数呈非线性下降。速度从0.2 m / s增加到2 m / s使曼宁系数降低到第一种情况的约30%。与速度效应相比,随着浸没率和密度的降低,粗糙度系数的降低幅度很小。

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