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To the determination of non-washable speed in the channels bed consisting of disconnected soils

机译:在包括断开的土壤中的频道床中确定不可洗的速度

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This article analyzes the factors that influence the deformation process in the channel. When assessing the deformation process in channels consisting of disconnected soils, the method for determining nonwashable speed was analyzed, taking into account the trapezoidal shape of the channel, and, based on laboratory studies, a dependence was proposed for determining the non-washable speed. The values of the proposed dependencies are compared with the calculated values of the formulas of I.I. Levi, C.E. Mirtskhulava, V.A. Velikanova, B.I. Studenichnikov and A.M. Latyshenkov and obtained positive results. The proposed dependencies for the determination of non-washable speed are improved, taking into account turbulence and the laws of velocity distribution over the stream's depth. In the experimental researches, were used sand particles with different diameters d ≤ 0.315 mm ; 0.315 mm < d ≤ 0.63 mm ; 0.63 mm < d ≤1.25 mm 1.25 mm < d ≤ 2.5 mm 2.5 mm < d ≤ 5.0 mm . Based on the analysis of the experimental data, the coefficients are as follows: η_(1)= 1.41 for the bottom of the channel and η_(2)= 1.52 for side slopes. The reliability of the results is justified by comparing the proposed calculation method with a study of other authors. Based on the research, constructed a plot of the velocity distribution and the depth of the stream. In these diagrams, preservation of the change in velocity along the depth of the flow was observed under various modes of motion. In all experiments, a process was observed-the smallest value of the flow velocity at the bottom and the highest at a depth of (0.8–0.9) h from the water level.
机译:本文分析了影响信道中变形过程的因素。当评估由断开的土壤组成的通道中的变形过程时,分析了确定不可采用速度的方法,考虑到通道的梯形形状,并且基于实验室研究,提出了一种确定不可洗涤速度的依赖性。将所提出的依赖性的值与I.i的公式的计算值进行比较。 Levi,C.e. Mirtskhulava,V.A. Velikanova,B.I. Studenichnikov和A.M. Latatshenkov并获得了积极的结果。提高了用于确定不可清洗速度的所提出的依赖性,考虑到流深度的湍流和速度分布规律。在实验研究中,使用不同直径d≤0.315mm的砂颗粒; 0.315 mm

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