床质泥沙非均质性对生长床形态长度、高度和移动速度影响的实验研究

N. Ikramov, T. Majidov
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引用次数: 4

摘要

在自然水流中,河床的生长运动导致水库体积和渠道断面面积减小,泵站前湾和水电站压力池淤积泥沙。这会导致泵、水轮机和压力管道的磨损,以及其他负面后果。在许多国家,河流携带着大量的沉积物和巨大的成本。在确定输沙量时,床脊高度和运动速度是重要的数值。这些数值的确定是基于实验研究,没有考虑到不同组分沉积物的非均质性。因此,根据所得公式计算出的数值与现场数据存在较大差异。为了消除这些差异,实验研究使用六种类型的分数具有相同的加权平均直径。在实验室数据的基础上,根据泥沙的水力尺寸和几何尺寸,得到了山脊长度、高度和移动速度的关系图。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Experimental Research of the Influence of Bedload Sediment Heterogeneity on Length, Height and Shifting Velocity of Growing Bed Configuration
In the natural current of water, the growing bed movement leads to a reduction of reservoir volume and canal cross-section area, filling by forebay of pump station and hydroelectric station pressure basins with sediment. This leads to abrasive wear of pumps, water turbines, and pressure pipelines, as well as other negative consequences. In many countries, rivers come laden with a large amount of sediment and enormous costs. At determining of sediment discharge it is important values of height and movement velocity of bed ridges. The determination of these values is based on experimental studies was not taken into account the heterogeneity of sediment with different fractions. For this reason, the calculated values according to obtained formulas have large discrepancies with field data. To eliminate these discrepancies, experimental studies were conducted using six types of fractions with the same weighted average diameter. Based on of laboratory data diagrams and interrelation were obtained for ridge length, height and movement velocity from sediment hydraulic and geometric sizes.
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