Discontinuous Galerkin methods for a dispersive wave hydro-sediment-morphodynamic model

Discontinuous Galerkin methods for a dispersive wave hydro-sediment-morphodynamic model
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DOI:
10.1016/j.cma.2021.113684
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发表时间:
2020-10
期刊:
ArXiv
影响因子:
--
通讯作者:
Kazbek Kazhyken;J. Videman;C. Dawson
Kazbek Kazhyken;J. Videman;C. Dawson
中科院分区:
其他
文献类型:
--
作者:
Kazbek Kazhyken;J. Videman;C. Dawson

文献摘要

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提出了一种色散波水力沉积物形态动力学模型,该模型是通过用 Green-Naghdi 方程中的色散项补充浅水水力沉积物形态动力学 (SHSM) 方程而开发的。提出了一种基于二阶Strang算子分裂的模型数值求解算法。该模型分为两部分,(1)SHSM 方程和(2)色散校正部分,使用不连续伽辽金有限元方法对其进行离散。这种分裂技术提供了一种工具来动态选择问题域中不应用分散项的区域,例如色散波模型不再有效的波破碎区域。提供了可以处理干湿和检测波浪破碎的算法,并提供了许多数值示例来验证所开发的数值求解算法。模拟结果表明,只要正确校准悬浮物和床质输送的经验模型,该模型就能够正确预测沉积物输送和床层形态动力学过程。此外,所开发的模型能够准确捕获直至斜流区的流体动力学和波浪色散效应,并且其应用适合于色散波效应普遍存在的模拟。
A dispersive wave hydro-sediment-morphodynamic model developed by complementing the shallow water hydro-sediment-morphodynamic (SHSM) equations with the dispersive term from the Green–Naghdi equations is presented. A numerical solution algorithm for the model based on the second-order Strang operator splitting is presented. The model is partitioned into two parts, (1) the SHSM equations and (2) the dispersive correction part, which are discretized using discontinuous Galerkin finite element methods. This splitting technique provides a facility to select dynamically regions of a problem domain where the dispersive term is not applied, e.g. wave breaking regions where the dispersive wave model is no longer valid. Algorithms that can handle wetting–drying and detect wave breaking are provided and a number of numerical examples are presented to validate the developed numerical solution algorithm. The results of the simulations indicate that the model is capable of predicting sediment transport and bed morphodynamic processes correctly provided that the empirical models for the suspended and bed load transport are properly calibrated. Moreover, the developed model is able to accurately capture hydrodynamics and wave dispersion effects up to swash zones, and its application is justified for simulations where dispersive wave effects are prevalent.