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A numerical three-dimensional non-cohesive earthen dam breach model.

机译:三维三维非粘性土坝破坏模型。

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摘要

A numerical three-dimensional dam breach model is developed for the non-cohesive earthen dam overtopping breach problem. The breach location can be anywhere along the dam. The topography of the entire dam site is considered. Three kinds of phenomena are modeled: vertical erosion of the dam face or breach channel where the flow surface is above the eroded soil surface; undercutting of the breach channel sides followed by sudden collapse of the undercut soil; and possible sudden collapse of sides of breach channel entrances upon loss of local stability. Transport of sediment is limited to the transport capacity.; A hybrid-type of the total variation diminishing finite-difference scheme with first-order in time and second-order in space is proposed to calculate outflow through a varying-geometry breach channel by solving two-dimensional shallow water equations. The source term is formulated to represent the bottom and side slopes, and a flux limiter is proposed. This scheme is shown to accurately reproduce supercritical, subcritical, and transcritical flows for the following analytical or experimental cases: one-dimensional theoretical dam break with initially dry and initially wet beds; steady flow over a bump; hydraulic jump; one-dimensional dam break with a bottom slope; and two-dimensional dam break with bottom and side slopes. Results show that our scheme has a good capability to calculate dam-breach outflows from a varying-geometry breach channel.; The model is tested using one field test from the IMPACT project funded by the European Commission and data from two historically breached dams. Results show that our three-dimensional model accurately predicts the peak breach discharge rate and the final breach width for these cases. Both the breach location and reservoir shape have a significant effect on the peak breach discharge and the outflow hydrograph shape. The real shape of the breach channel during the breach process is successfully modeled.; The overtopping dam-breach problem with multiple breach locations under wind and wave actions is modeled. Intermittent wave overtopping and erosion are simulated. The dam initially breaches at one location and in some cases may breach at additional locations. Both the wind speed and wind direction can change the final breach shape and breach outflow hydrograph and the number of breaches for a particular reservoir.
机译:针对非粘性土坝过顶破坏问题,建立了三维三维大坝破坏模型。突破口的位置可以在大坝的任何地方。考虑整个坝址的地形。对三种现象进行了建模:坝面或冲沟的垂直侵蚀,其中流动面在侵蚀的土壤面以上;缺口通道侧的底切,然后底切土突然倒塌;失去局部稳定性后,违规通道入口的侧面可能突然坍塌。沉积物的运输受到运输能力的限制。提出了一种混合形式的总变化量递减的有限差分方案,该方案具有一阶时间和二阶空间,通过求解二维浅水方程来计算通过变化几何形状破坏通道的流出量。源项用公式表示底部和侧面的斜率,并提出了通量限制器。在以下分析或实验情况下,该方案显示出可以精确地重现超临界,亚临界和跨临界流:一维理论溃坝,初始为干床,初始为湿床;稳定地流过颠簸;液压跳跃一维有底坡的溃坝;以及带有底部和侧面坡度的二维溃坝。结果表明,我们的方案具有良好的计算能力,可以计算出来自不同几何形状破坏通道的水坝破坏流量。该模型使用来自欧洲委员会资助的IMPACT项目的一次现场测试以及来自两个历史悠久的大坝的数据进行了测试。结果表明,我们的三维模型可以准确预测这些情况下的峰值违规排放率和最终违规宽度。断口位置和储层形状对断口峰流量和出水水位线形状均具有显着影响。在突破过程中,突破通道的真实形状已成功建模。对在风浪作用下具有多个破口位置的水坝溃决问题进行了建模。模拟了间歇波的越过和侵蚀。大坝最初在一个位置突破,在某些情况下可能在其他位置突破。风速和风向都可以改变最终的缺口形状和缺口流出水位图以及特定水库的缺口数量。

著录项

  • 作者

    Wang, Zhengang.;

  • 作者单位

    Utah State University.;

  • 授予单位 Utah State University.;
  • 学科 Engineering Civil.
  • 学位 Ph.D.
  • 年度 2005
  • 页码 208 p.
  • 总页数 208
  • 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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