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首页> 外文期刊>Proceedings of the Institution of Civil Engineers >Numerical modelling of braided streams in unsteady flow
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Numerical modelling of braided streams in unsteady flow

机译:非恒定流中辫状流的数值模拟

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Braided streams with vegetation growth under unsteady water supply conditions were reproduced using horizontal two-dimensional bed deformation numerical analysis. The effects of both vegetation and the unsteady characteristics of the water supply on the dynamic characteristics of braided streams are investigated. The mechanisms of stream lengthening and the decrease in the number of streams under unsteady flow conditions are discussed. To avoid complete transitions of bed configurations during a flood, tested hydraulic conditions were restricted to those with short-period hydrographs. The results show that wavelengths of submerged bars under unsteady water supply conditions are shorter than those under steady conditions. The results further suggest that both sediment deposition at higher locations and the formation of islands primarily cause stream lengthening under unsteady flow conditions. The wavelength of submerged bars was not a primary cause. Sediment is deposited in smaller channels during floods; the bed at riffles is eroded during low flows. These phenomena force water to flow into larger streams. Consequently, the number of streams decreases under unsteady flow conditions. Furthermore, the presence of vegetation enhances sediment deposition at higher locations and this contributes to a decrease in the number of streams under the condition that vegetation on islands is not completely washed away by floods.
机译:使用水平二维床变形数值分析,再现了在非恒定供水条件下具有植被生长的辫状流。研究了植被和供水的不稳定特性对辫状流动力特性的影响。讨论了在非恒定流动条件下的流延长和流数量减少的机理。为了避免洪水期间河床构造的完全过渡,将测试的水力条件限制为使用短期水文测量的条件。结果表明,在不稳定的供水条件下,浸没棒的波长要比稳定条件下的短。结果进一步表明,在非稳定流动条件下,较高位置的沉积物沉积和岛状物的形成均会引起流延长。浸没棒的波长不是主要原因。洪水期间沉积物沉积在较小的河道中;在低流量下,浅滩的床被侵蚀了。这些现象迫使水流入更大的溪流。因此,在不稳定流动条件下,流的数量减少。此外,在岛上的植被没有被洪水冲走的情况下,植被的存在增加了较高位置的沉积物沉积,这有助于减少溪流的数量。

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