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Numerical investigation of long-term planform dynamics and stability of river meandering on fluvial floodplains

机译:河流漫滩长期曲折河道动力学和稳定性的数值研究

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摘要

A mathematical model for river meandering and floodplain development is presented under the assumption of constant channel width, which combined Johanneson and Parker (1989) linear theory for flows in river bends and a conceptual depositional model from Howard (1992). A new bank erosion model is also developed, which takes into consideration of the nonlinearity in near-bank velocity and the outer bank height. Simulations reproduce the long-term behavior of river meandering and floodplain evolution in a way very similar to their natural processes. Based on the simulation results, stability of river meandering dynamics is discussed and the concept of filtration effect is introduced to highlight meandering rivers' capability to filter out arbitrarily applied planform disturbance. Simulations are also carried out to investigate the influence of the velocity nonlinearity and the outer bank height in bank erosion model, as well as their combinations. Results show that the consideration of velocity nonlinearity in bank erosion model leads to highly upstream-skewing geometry of fully developed river meanders, as well as a slower downstream migration of meander trains. The influence of nonlinearity in bank erosion model is much smaller than the influence of bank height, which reduces the bank migration rate exponentially in the newly introduced bank erosion model. The outer bank height consideration tends to decelerate the downstream migration rate of river meanders and accelerate lateral expansion of the floodplain as well. Consequently, a broader floodplain is generated compared with simulations without bank height considerations.
机译:在恒定河道宽度的假设下,提出了一个河道蜿蜒和洪泛区发展的数学模型,该模型结合了Johanneson和Parker(1989)的关于河弯流量的线性理论和一个来自Howard(1992)的概念性沉积模型。还开发了一种新的堤岸侵蚀模型,该模型考虑了近堤岸速度和外堤岸高度的非线性。模拟以与自然过程非常相似的方式再现了河流蜿蜒和漫滩演变的长期行为。在模拟结果的基础上,讨论了河流蜿蜒动力学的稳定性,并引入了过滤效果的概念,以突出蜿蜒河流过滤掉任意应用的平面扰动的能力。还进行了仿真研究,以研究速度非线性和堤岸高度对堤岸侵蚀模型及其组合的影响。结果表明,在河岸侵蚀模型中考虑速度非线性会导致充分发展的河道蜿蜒曲折的高度几何形状,并导致河曲列车的下游游移速度变慢。堤岸侵蚀模型中非线性的影响远小于堤岸高度的影响,在新引入的堤岸侵蚀模型中,堤岸迁移率呈指数下降。考虑外岸高度往往会减缓河曲下游的迁移速度,并加速洪泛区的横向扩展。因此,与不考虑堤岸高度的模拟相比,生成了更宽泛的洪泛区。

著录项

  • 来源
    《Geomorphology》 |2011年第4期|p.195-207|共13页
  • 作者单位

    Research Institute for Sediment in River and Coastal Engineering, School of Civil Engineering, Tianjin University, Tianjin 300072, China;

    Research Institute for Sediment in River and Coastal Engineering, School of Civil Engineering, Tianjin University, Tianjin 300072, China;

    School of Engineering and Material Science, Queen Mary, University of London, London E1 4NS, UK;

    The First Survey and Design Institute for Navigational Works of the Transportation Ministry of China, Tianjin 300222, China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    river meandering floodplain numerical simulation bank erosion deposition stability;

    机译:河道曲折漫滩数值模拟堤岸冲淤稳定性;

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