{"title":"Investigation of cloud cavitating flow in a venturi using Adaptive Mesh Refinement (AMR)","authors":"Dhruv Apte, Mingming Ge, Olivier Coutier-Delgosha","doi":"arxiv-2409.02369","DOIUrl":null,"url":null,"abstract":"Unsteady cloud cavitating flow is detrimental to the efficiency of hydraulic\nmachinery like pumps and propellers due to the resulting side-effects of\nvibration, noise and erosion damage. Modelling such a unsteady and highly\nturbulent flow remains a challenging issue. In this paper, cloud cavitating\nflow in a venturi is calculated using the Detached Eddy Simulation (DES) model\ncombined with the Merkle model. The Adaptive Mesh Refinement (AMR) method is\nemployed to speed up the calculation and investigate the mechanisms for vortex\ndevelopment in the venturi. The results indicate the velocity gradients and the\ngeneralized fluid element strongly influence the formation of vortices\nthroughout a cavitation cycle. In addition, the cavitation-turbulence coupling\nis investigated on the local scale by comparing with high-fidelity experimental\ndata and using profile stations. While the AMR calculation is able to predict\nwell the time-averaged velocities and turbulence-related aspects near the\nthroat, it displays discrepancies further downstream owing to a coarser grid\nrefinement downstream and under-performs compared to a traditional grid\nsimulation . Additionally, the AMR calculations is unable to reproduce the\ncavity width as observed in the experiments. Therefore, while AMR promises to\nspeed the process significantly by refining grid only in regions of interest,\nit is comparatively in line with a traditional calculation for cavitating\nflows. Thus, this study intends to provide a reference to employing AMR as a\ntool to speed up calculations and be able to simulate turbulence-cavitation\ninteractions accurately.","PeriodicalId":501125,"journal":{"name":"arXiv - PHYS - Fluid Dynamics","volume":"104 1","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2024-09-04","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"arXiv - PHYS - Fluid Dynamics","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/arxiv-2409.02369","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
Abstract
Unsteady cloud cavitating flow is detrimental to the efficiency of hydraulic
machinery like pumps and propellers due to the resulting side-effects of
vibration, noise and erosion damage. Modelling such a unsteady and highly
turbulent flow remains a challenging issue. In this paper, cloud cavitating
flow in a venturi is calculated using the Detached Eddy Simulation (DES) model
combined with the Merkle model. The Adaptive Mesh Refinement (AMR) method is
employed to speed up the calculation and investigate the mechanisms for vortex
development in the venturi. The results indicate the velocity gradients and the
generalized fluid element strongly influence the formation of vortices
throughout a cavitation cycle. In addition, the cavitation-turbulence coupling
is investigated on the local scale by comparing with high-fidelity experimental
data and using profile stations. While the AMR calculation is able to predict
well the time-averaged velocities and turbulence-related aspects near the
throat, it displays discrepancies further downstream owing to a coarser grid
refinement downstream and under-performs compared to a traditional grid
simulation . Additionally, the AMR calculations is unable to reproduce the
cavity width as observed in the experiments. Therefore, while AMR promises to
speed the process significantly by refining grid only in regions of interest,
it is comparatively in line with a traditional calculation for cavitating
flows. Thus, this study intends to provide a reference to employing AMR as a
tool to speed up calculations and be able to simulate turbulence-cavitation
interactions accurately.
非稳定云气蚀流会产生振动、噪音和侵蚀破坏等副作用,从而影响泵和螺旋桨等液压机械的效率。对这种不稳定的高湍流进行建模仍然是一个具有挑战性的问题。本文使用分离涡模拟(DES)模型结合梅克尔模型计算文丘里管中的云空化流。采用自适应网格细化(AMR)方法加快了计算速度,并研究了文丘里管中涡流发展的机制。结果表明,速度梯度和广义流体元素对整个空化循环中涡流的形成有很大影响。此外,通过与高保真实验数据比较和使用剖面站,研究了局部尺度上的空化-湍流耦合。虽然 AMR 计算能够很好地预测喉部附近的时均速度和湍流相关方面,但由于下游网格细化较粗,它在更下游显示出差异,与传统网格模拟相比表现不佳。此外,AMR 计算无法再现实验中观察到的空腔宽度。因此,虽然 AMR 可通过仅在感兴趣的区域细化网格来显著加快计算过程,但相对而言,它与传统的空化流计算方法并不一致。因此,本研究旨在为利用 AMR 作为工具加快计算速度并准确模拟湍流与空化相互作用提供参考。