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Non-hydrostatic models for wave propagation, breaking, and run-up.

机译:用于波传播,破裂和加速的非流体静力学模型。

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摘要

This dissertation develops a series of non-hydrostatic pressure wave models based on the finite element free surface flow model, CCHE2D, for simulating propagation, breaking, and run-up of coastal wave processes.;The first non-hydrostatic formulation presented in this dissertation directly introduces a non-hydrostatic pressure module into CCHE2D. An edge-based pressure allocation method is implemented, and a depth-integrated vertical momentum equation is introduced. The depth-integrated horizontal momentum equations are solved for a provisional velocity field, and then the non-hydrostatic pressure is obtained by satisfying the divergence-free velocity field condition, subsequently the velocity field is corrected by the non-hydrostatic pressure. Finally the free surface elevation is computed by the depth-integrated continuity equation.;Next, a depth-integrated non-hydrostatic model for simulating nearshore wave processes is developed by solving a depth-integrated vertical momentum equation and the conservation form of the shallow water equations including extra non-hydrostatic pressure terms. A pressure projection method and the divergence-free velocity field condition are used together to solve the non-hydrostatic pressure. To resolve discontinuous flows, involving breaking waves and hydraulic jumps, a momentum conservation advection scheme is developed. In addition, the model is implemented with a simple but efficient wetting and drying algorithm to deal with the moving shoreline.;The depth-integrated non-hydrostatic pressure models, which assume a linear distribution of the vertical pressure, have limitations in certain applications (e.g., propagation of highly dispersive waves). A multi-layer non-hydrostatic model is developed by adding more layers to the aforementioned second depth-integrated non-hydrostatic model. The multi-layer model is capable of resolving more realistic vertical flow structures and better representing the wave dynamics.;Finally, a well validated depth-integrated non-hydrostatic model is applied to simulate a wide range of coastal wave processes. These numerical tests further evaluate the non-hydrostatic model from different aspects of engineering practice. In particular, they demonstrate the efficiency of non-hydrostatic models for coastal wave modeling, and they also reveal the great potential of non-hydrostatic models to simulate real-life coastal wave processes.
机译:本文基于有限元自由表面流模型CCHE2D,开发了一系列非静水压力波模型,用于模拟海岸波过程的传播,破裂和上升。直接将非静水压力模块引入CCHE2D。实现了基于边缘的压力分配方法,并引入了深度积分的垂直动量方程。对临时速度场求解深度积分的水平动量方程,然后通过满足无散度速度场条件获得非静水压力,随后用非静水压力校正速度场。最后,通过深度积分的连续性方程计算出自由表面高程。接着,通过求解深度积分的垂直动量方程和浅水区的养护形式,建立了一个模拟近岸波浪过程的深度积分非静水模型。等式,包括额外的非静水压力项。压力投影法和无散度速度场条件一起用于解决非静水压力。为了解决不连续的流动,包括浪潮和水力跳跃,开发了动量守恒平流方案。此外,该模型还通过简单但有效的润湿和干燥算法来实现,以处理运动中的海岸线。;假设垂直压力呈线性分布的深度集成非静水压力模型在某些应用中存在局限性(例如高色散波的传播)。通过向上述第二深度集成非静水模型增加更多的层来开发多层非静水模型。多层模型能够解析更真实的垂直流结构,并更好地表示波浪动力学。最后,采用经过充分验证的深度集成非静水模型来模拟各种沿海波浪过程。这些数值测试从工程实践的不同方面进一步评估了非静液压模型。特别是,他们展示了非静水模型在海浪建模中的效率,并且还揭示了非静水模型在模拟现实生活中的沿海波过程中的巨大潜力。

著录项

  • 作者

    Wei, Zhangping.;

  • 作者单位

    The University of Mississippi.;

  • 授予单位 The University of Mississippi.;
  • 学科 Civil engineering.
  • 学位 Ph.D.
  • 年度 2014
  • 页码 152 p.
  • 总页数 152
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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