Numerical study of instability mechanism in the air-core vortex formation process

• Published in: Engineering applications of computational fluid mechanics 2023-12, Vol.17 (1)
• Main Authors: Kan, Kan, Xu, Yuhang, Li, Zhixiang, Xu, Hui, Chen, Huixiang, Zi, Dan, Gao, Qiang, Shen, Lian
• Format: Article
• Language: English
• Subjects: Air-core vortex; Attenuation; counterrotating pair; Flow stability; Fluid flow; Hydroelectric power stations; Intake pipes; Large eddy simulation; Surface stability; Two phase flow; Velocity gradient; Vortices; Vorticity; water level fluctuation; Water level fluctuations; wave
• ISSN: 1994-2060; 1997-003X
• DOI: 10.1080/19942060.2022.2156926

Air-core vortices are a ubiquitous phenomenon in the intakes of hydropower stations. Due to the transient and instability of two-phase vorticial flow, the prediction of air-core vortex formation is challenging, and understanding of the instability mechanism remains elusive. In this study, the large eddy simulation (LES) method and a coupled level-set and volume-of-fluid (CLSVOF) method are performed to study air-core vortex formation in a benchmark reservoir with a horizontal intake pipe. The process of air-core vortex formation can be classified into an inception stage, an instability stage, and a stability stage. In the instability stage, the surface vortex repeatedly goes through the process of inception, enhancement, attenuation, and extinction. The movement of the counterrotating secondary vortices and water surface level fluctuation plays a negative role in air-core vortex formation. The additional motion generated by the counterrotating pair drives the pair to the back wall. The main vortex undergoes attenuation due to the stretching/tilting effects induced by the secondary vortex. Water level fluctuations briefly increase the submergence depth, which in turn reduces the vertical velocity gradient and vertical vorticity, destabilizing the vortex. The perturbation of the air-core vortex by water level fluctuations is present only at the beginning of the instability stage.