Discontinuous Galerkin simulator of shallow vortical flow with turbulence

IF 4 2区 环境科学与生态学 Q1 WATER RESOURCES
Georges Kesserwani, Xitong Sun , Mahya Hajihassanpour , Mohammad Kazem Sharifian
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引用次数: 0

Abstract

Shallow vortical flow can often occurs past (un)submerged topographies, prevailing in quasi-steady states with turbulence. Practically, vortical flow is represented by the two-dimensional (2D) Reynolds-Averaged Navier–Stokes equations, including the two-equation k-ε turbulent model (RANS-k-ε), and are commonly resolved by finite difference/volumes second-order accurate solvers. Such RANS-k-ε solvers, in addition to needing a fine resolution, require adding artificial treatments–extrinsic (unlocalised) reconstructions of wet-dry fronts with slope-limiting–that can impact the vortical eddy predictions. The second-order discontinuous Galerkin (DG2) solver intrinsically integrates the wet-dry fronts and uses localised slope-limiting; resulting in an implicit large eddy simulator with the shallow water equations (DG2-SWE) that can only simulate uncompounded eddies. A novel DG2 solver of RANS-k-ε (DG2-RANS-k-ε) is devised for simulating a wider range of vortical eddies, by: first, transforming the 5×5 advective-diffusive RANS-k-ε system into a 13×13 advection-dominated system; second, extending the DG2 formulation to the 13×13 system, with adaptation of its robustness treatments for the mean-flow variables; and, last, adding a new combination of stability/positivity-preserving treatments for turbulent-flow quantities. The DG2-RANS-k-ε solver is evaluated for simulating five experimental benchmarks using coarse, medium and fine resolutions. Results show that DG2-RANS-k-ε can reproduce compound eddies from the medium resolution, and that DG2-RANS (without k-ε) can better reproduce laminar wakes. Using the medium resolution reduces runtimes by 7-fold and running on the GPU further reduce runtimes by 2-to-6-fold. The code, including simulation setup files, is open-source within a new release of the LISFLOOD-FP hydraulic modelling environment (https://doi.org/10.5281/zenodo.7628739), with documentation and demonstration videos (https://www.seamlesswave.com/DG2_RANS).
含湍流的浅涡旋不连续伽辽金模拟器
浅涡旋流经常发生在(非)淹没地形,盛行于准稳定状态与湍流。实际上,涡旋流由二维(2D) reynolds - average Navier-Stokes方程表示,包括两方程k-ε湍流模型(ranss -k-ε),通常由有限差分/体积二阶精确求解器来求解。这样的ransk -ε解算器除了需要精确的分辨率外,还需要添加人工处理——具有坡度限制的干湿锋面的外在(非局部)重建——这可能会影响涡旋的预测。二阶不连续伽辽金(DG2)解算器本质上集成了干湿锋面并使用了局部坡限;由此产生了一个隐式的大涡流模拟器,该模拟器具有浅水方程(DG2-SWE),只能模拟非复合涡流。本文设计了一种新的ransk -ε DG2求解器(DG2- ransk -ε),用于模拟更大范围的涡旋,方法是:首先,将5×5平流扩散的ransk -ε体系转化为13×13平流主导的体系;其次,将DG2公式扩展到13×13系统,并对平均流量变量进行了鲁棒性处理;最后,为湍流量添加了一种新的稳定性/正性保护处理组合。对dg2 - ranss -k-ε求解器在粗、中、细分辨率下模拟五种实验基准进行了评价。结果表明,dg2 - ranss -k-ε能在中等分辨率下再现复合涡流,不含k-ε的dg2 - ranss能更好地再现层流尾迹。使用中等分辨率可以减少7倍的运行时间,在GPU上运行可以进一步减少2到6倍的运行时间。代码,包括仿真设置文件,在LISFLOOD-FP水力建模环境(https://doi.org/10.5281/zenodo.7628739)的新版本中是开源的,并带有文档和演示视频(https://www.seamlesswave.com/DG2_RANS)。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Advances in Water Resources
Advances in Water Resources 环境科学-水资源
CiteScore
9.40
自引率
6.40%
发文量
171
审稿时长
36 days
期刊介绍: Advances in Water Resources provides a forum for the presentation of fundamental scientific advances in the understanding of water resources systems. The scope of Advances in Water Resources includes any combination of theoretical, computational, and experimental approaches used to advance fundamental understanding of surface or subsurface water resources systems or the interaction of these systems with the atmosphere, geosphere, biosphere, and human societies. Manuscripts involving case studies that do not attempt to reach broader conclusions, research on engineering design, applied hydraulics, or water quality and treatment, as well as applications of existing knowledge that do not advance fundamental understanding of hydrological processes, are not appropriate for Advances in Water Resources. Examples of appropriate topical areas that will be considered include the following: • Surface and subsurface hydrology • Hydrometeorology • Environmental fluid dynamics • Ecohydrology and ecohydrodynamics • Multiphase transport phenomena in porous media • Fluid flow and species transport and reaction processes
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