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Application of modified Manning formula in the determination of vertical profile velocity in natural rivers

机译:改进的曼宁公式在确定天然河流垂直剖面速度中的应用

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Seldom studied before, the vertical profile velocity is indicative of the flood process and nutrient transportation process. In this paper, a substitution of cross section hydraulic radius with vertical depth was made to the Manning formula, which was then applied in the vertical profile velocity determination, simultaneously, the determination accuracy and its relationship with hydraulic conditions were discussed, based on the 1050 vertical profiles sampled from 140 cross sections in flood and moderate level seasons. The observations show the following. (1) The modified Manning formula provides a simplified approach for vertical profile velocity determination with acceptable accuracy. (2) The fitting quality of the profile velocity from the middle region of the cross section and the flood season were higher than that from near the bank or the moderate level season. The coefficient of determination (ft2) of the regression for the moderate level season and the flood season were 0.55 and 0.58, while the Nash-Sutcliffe coefficients were 0.64 and 0.82, respectively. (3) Analysis of the determination error and the coefficient of variation showed a positive correlation with the river aspect ratio. This seems to suggest that the modified Manning formula tends to be more applicable in narrow and deep rivers. More measurements from rivers or channels with a high aspect ratio would be meaningful for future research.
机译:以前很少研究,垂直剖面速度指示洪水过程和养分输送过程。本文将截面水力半径用垂直深度替换为曼宁公式,然后将其应用于垂直剖面速度确定中,同时基于1050讨论了确定精度及其与水力条件的关系。在洪水和中等水平季节中,从140个断面取样的垂直剖面。观察结果如下。 (1)修改后的曼宁公式为垂直剖面速度确定提供了简化的方法,并且具有可接受的精度。 (2)断面中部和洪水季节剖面速度的拟合质量均高于河岸附近或中等水平季节的剖面速度拟合质量。中等水平季节和洪水季节的回归的确定系数(ft2)为0.55和0.58,而纳什-萨特克利夫系数的分别为0.64和0.82。 (3)对确定误差和变异系数的分析与河流纵横比呈正相关。这似乎表明,修改后的曼宁公式更倾向于在狭窄和深水河流中使用。高纵横比的河流或河道的更多测量对于将来的研究将是有意义的。

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