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Development, implementation, and verification of hp discontinuous Galerkin models for shallow water hydrodynamics and transport.

机译:hp不连续Galerkin模型在浅水流体动力学和运输中的开发,实施和验证。

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摘要

Shallow water hydrodynamic and transport equations are used to describe many free surface flow and transport processes in the deep ocean, coastal ocean, estuaries, rivers, open channels, and coastal floodplain. In many practical applications, these equations must be solved on domains with geometrically complex vertical and horizontal boundaries introduced by both the bathymetry/topography and the coastline. Finite element methods are a natural choice for such problems given the ease with which unstructured grids can be implemented; however, there are well known problems associated with solving these equations using the standard Galerkin method.; The discontinuous Galerkin (DG) finite element method offers a solution strategy to solve the numerical difficulties associated with these equations. The main advantages of DG methods for shallow water flow and transport are: their ability to capture smooth physically damped solutions to wave propagation problems; their ability to handle advection dominated flows and sharp gradients including problems with hydraulic jumps or bores (discontinuities); their inherent elemental mass and momentum conservation properties, which make them ideal for coupling flow and transport models; and the ease with which both h (grid) and p (polynomial order) refinement, and also adaptivity can be implemented.; In this dissertation, robust, accurate, computationally efficient, and flexible one- and two-dimensional hp DG finite element models for shallow water hydrodynamics, passive transport, and sediment transport are developed, implemented, and verified. The performance of the models is demonstrated and rigorously assessed by examining a number of test cases including linear and highly nonlinear problems, both uncoupled and coupled transport problems, idealized coastal modeling applications, problems with discontinuities or shocks, and full-scale applications. Through systematic h and p convergence studies the dual paths to convergence of the method are demonstrated for both linear and highly nonlinear problems where it is observed that standard h-refinement for a fixed p leads to optimal convergence rates of p + 1, while exponential convergence is observed for p-refinement on a fixed mesh. Additionally, the efficiency and effectiveness of h- and p-refinement, a variety of time stepping schemes, and a simple p-adaptive algorithm are investigated with the goal of obtaining highly accurate solutions in the most efficient manner possible.
机译:浅水流体动力方程和运输方程用于描述深海,沿海海洋,河口,河流,明渠和沿海洪泛区的许多自由地表流动和运输过程。在许多实际应用中,必须在由测深法/地形和海岸线引入具有几何复杂的垂直和水平边界的域上求解这些方程式。考虑到可以轻松实现非结构化网格,有限元方法是解决此类问题的自然选择。但是,使用标准的Galerkin方法求解这些方程存在一些众所周知的问题。不连续Galerkin(DG)有限元方法提供了一种解决方案,可以解决与这些方程式相关的数值困难。 DG方法在浅水流动和输送中的主要优点是:具有捕获波浪传播问题的平滑物理阻尼解的能力;他们处理对流为主的流量和陡坡的能力,包括水力跃迁或井眼(间断)问题;它们固有的元素质量和动量守恒特性,使其成为耦合流动和运输模型的理想选择;可以轻松实现h(网格)和p(多项式阶数)的细化,以及自适应性。本文针对浅水流体动力学,被动输运和泥沙输运,建立了鲁棒,准确,计算高效,灵活的一维和二维hp DG有限元模型。通过检查许多测试案例(包括线性和高度非线性问题,非耦合和耦合运输问题,理想化的海岸建模应用,不连续性或冲击性问题以及全面应用)来证明并严格评估了模型的性能。通过系统的h和p收敛研究,针对线性和高度非线性问题都证明了该方法收敛的双重路径,其中观察到针对固定p的标准h细化导致p + 1的最优收敛速度,而指数收敛在固定网格上观察p细化。此外,还研究了h和p细化的效率和有效性,各种时间步长方案以及简单的p自适应算法,旨在以最有效的方式获得高度精确的解决方案。

著录项

  • 作者

    Kubatko, Ethan.;

  • 作者单位

    University of Notre Dame.;

  • 授予单位 University of Notre Dame.;
  • 学科 Engineering Civil.
  • 学位 Ph.D.
  • 年度 2006
  • 页码 245 p.
  • 总页数 245
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 建筑科学;
  • 关键词

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