High-resolution 3D computation of time-periodic long-wake flows with the Carrier-Domain Method and Space–Time Variational Multiscale method with isogeometric discretization

IF 3.7 2区 工程技术 Q1 MATHEMATICS, INTERDISCIPLINARY APPLICATIONS Computational Mechanics Pub Date : 2024-02-12 DOI:10.1007/s00466-023-02419-3
Yang Liu, Kenji Takizawa, Tayfun E. Tezduyar
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Abstract

The Carrier-Domain Method was introduced for high-resolution computation of time-periodic long-wake flows. The cost-effectiveness of the method makes such computations practical in 3D. A short segment of the wake domain, the carrier domain, moves in the free-stream direction, from the beginning of the long wake domain to the end. The data at the moving inflow plane comes from the time-periodic data computed at an earlier position of the carrier domain. With the high mesh resolution that can easily be afforded over the short domain segment, the wake flow patterns can be carried, with superior accuracy, far downstream. Computing the long-wake flow with a high-resolution moving mesh that covers a short segment of the wake domain at any instant during the computation would certainly be far more cost-effective than computing it with a high-resolution fixed mesh that covers the entire length. We present high-resolution 3D computation of time-periodic long-wake flow for a cylinder and a wind turbine, both computed with isogeometric discretization and the Space–Time Variational Multiscale method. In the isogeometric discretization, the basis functions are quadratic NURBS in space and linear in time. The cylinder flow is at Reynolds number 100. At this Reynolds number, the flow has an easily discernible vortex shedding period. The wake flow is computed up to 350 diameters downstream of the cylinder, far enough to see the secondary vortex street. In the wind turbine long-wake flow computation, the velocity data at the inflow boundary of the wake domain comes from an earlier wind turbine computation, with the turbine rotor having a diameter of \({126}\,\hbox {m}\), extracted by projection from a plane located \({10}\,\hbox {m}\) downstream of the turbine. The wake flow is computed up to \({482}\,\hbox {m}\) downstream of the wind turbine. In both the cylinder and wind turbine wake flow computations, the flow patterns obtained with the full domain and carrier domain show a near-perfect match, clearly demonstrating the effectiveness and practicality of the Carrier-Domain Method in high-resolution 3D computation of time-periodic long-wake flows.

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利用载波域法和等几何离散的时空变异多尺度法高分辨率三维计算时周期长波流
载流子域法是一种用于高分辨率计算时间周期性长波流的方法。该方法的成本效益使三维计算成为现实。唤醒域的一小段,即载流子域,沿自由流方向从长唤醒域的起点移动到终点。移动的流入平面上的数据来自载流域早期位置上计算的时间周期数据。由于短域段的网格分辨率较高,因此能以极高的精度将尾流流型带到下游。使用高分辨率移动网格计算长波流,在计算过程中的任何瞬间都能覆盖短波域段,其成本效益肯定远远高于使用覆盖整个长度的高分辨率固定网格计算长波流。我们介绍了圆柱体和风力涡轮机时周期性长波流的高分辨率三维计算,计算均采用等距离散法和时空变异多尺度法。在等距离散法中,基函数在空间上是二次方 NURBS,在时间上是线性的。气缸流动的雷诺数为 100。在此雷诺数下,流动有一个容易辨别的涡流脱落期。尾流的计算范围为圆筒下游 350 直径处,足以看到次级涡街。在风力涡轮机长涡流计算中,涡流域流入边界的速度数据来自之前的风力涡轮机计算,涡轮机转子直径为({126}\\hbox {m}\),从位于涡轮机下游的平面({10}\\hbox {m}\)投影提取。风轮机下游的尾流一直计算到({482}\\hbox {m}\)。在气缸和风轮机尾流计算中,全域和载波域得到的流型几乎完全吻合,清楚地表明了载波域方法在高分辨率三维计算时周期性长尾流中的有效性和实用性。
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来源期刊
Computational Mechanics
Computational Mechanics 物理-力学
CiteScore
7.80
自引率
12.20%
发文量
122
审稿时长
3.4 months
期刊介绍: The journal reports original research of scholarly value in computational engineering and sciences. It focuses on areas that involve and enrich the application of mechanics, mathematics and numerical methods. It covers new methods and computationally-challenging technologies. Areas covered include method development in solid, fluid mechanics and materials simulations with application to biomechanics and mechanics in medicine, multiphysics, fracture mechanics, multiscale mechanics, particle and meshfree methods. Additionally, manuscripts including simulation and method development of synthesis of material systems are encouraged. Manuscripts reporting results obtained with established methods, unless they involve challenging computations, and manuscripts that report computations using commercial software packages are not encouraged.
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