用数值模拟方法分析低地河流水力参数的变化

Szymon Wojak, A. Strużyński, Maciej Wyrębek
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引用次数: 0

摘要

研究目的:河道是一种动态结构,其中河流作用导致水流能量与河床物质稳定性之间的平衡状态。利用监测工具很难捕捉到河流形态的变化,但可以使用物理或数值模拟来反映这些自然过程。本研究的目的是利用数值模拟的方法分析奈达河调节段水力参数的变异性及其对形态变化的影响。材料与方法:在野外实测的基础上,建立了该河流的数值模型。在本节中,通道得到了加强,从而使其恢复过程成为可能。数值模拟了从低流到上岸流的范围。采用Riley法测定河岸流量。基于模型参数的计算使得分析它们对床层动力学的影响成为可能。结果与结论:利用数值模拟结果(平均流速、剪应力和水深)计算剪切速度、雷诺数、颗粒雷诺数和沉降速度。单个参数随流量增加的变化趋势不明显,证明了水流与河床之间存在不规则联系。河流流量的变化不仅影响河流过程的强度,而且影响河流过程的位置。在低流量时形成的底部形态在高流量时完全改变了,正如对奈达河检查段的测量和模拟所表明的那样。
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ANALYSIS OF CHANGES IN HYDRAULIC PARAMETERS IN A LOWLAND RIVER USING NUMERICAL MODELING
Aim of the study: River channels are dynamic structures in which fluvial processes leading to equilibrium state between energy of flowing water and the stability of the bed material. The changes of river morphology is difficult to capture using the monitoring tools, however, physical or numerical modeling can be used instead to reflect these natural processes. Objective of the study is to analyze the variability of hydraulic parameters and their impact on morphological changes using numerical modeling of a regulated section of the Nida River. Material and methods: On the basis of field measurements, numerical model of the river was built. In this section, the channel has been strengthened, which enables the process of its restoration. Numerical modeling was carried out for a range of flows from low to an overbank one. Bankfull discharge was determined using the Riley method. Calculations based of modeled parameters made it possible to analyze their impact on the bed dynamics. Results and conclusions: The numerical modeling resutls (average velocity, shear stresses, and water depth) was used to calculate shear velocity, Reynolds Number, Grain Reynolds Number and settling velocity. The lack of clear trends of changes in individual parameters with increasing flows proves the existence of irregular connections between flowing water and riverbed. Changing discharge in the river affects not only the intensity of fluvial processes, but also their location. The bottom morphology created during low flows is completely changed at the passage of high water, as indicated by measurements and simulations of the examined section of the Nida River.
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来源期刊
CiteScore
0.40
自引率
25.00%
发文量
1
审稿时长
50 weeks
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