Prediction of the Cavitation over a Twisted Hydrofoil Considering the Nuclei Fraction Sensitivity at 4000 m Altitude Level
Abstract
:1. Introduction
2. Numerical Methods
2.1. Numerical Method for Turbulent Flow
2.2. Cavitation Model
2.3. Vapor Volume Fraction
3. Case and Setup
3.1. Important Dimensionless Parameters
3.2. Flow Domain of Hydrofoil
3.3. CFD Setup
4. Numerical-Experimental Verification
5. Cavitation Vapor Proportion at Different Altitudes
5.1. Variation Law
5.2. Sensitivity Analysis
6. Flow Behaviors Considering Altitude Level
6.1. Pressure Distribution Law on Foil Surface
6.2. Turbulent Flow around Foil
6.3. Development of Cavitation at Halt- = 4000 m
7. Conclusions
- (1)
- With the decreasing of cavitation coefficient Cσ, the scale of cavitation continually increases and the increasing is quicker and quicker. The nuclei volume fraction fvnuc has obvious influence on cavitation. The size of cavitation is different at different altitude levels. If the altitude is higher within 0~4000 m, the fvnuc is lower and the size of cavitation is smaller. The difference of the size of cavitation among altitude levels is bigger when Cσ is small. That is, the sensitivity Δfcav is high. On the contrary, the relative sensitivity Δfcav*, which is the ratio between Δfcav and the absolute cavitation fraction fcav, is high when Cσ is large. When Cσ is 1.071, the Δfcav* between 0 m and 4000 m altitudes is about 4.6%. When Cσ increases to 2.713, the Δfcav* can be up to about 22.8%. It means that the cavitation volume fraction sensitivity should be considered in judging the inception cavitation of water pumps and hydro-turbines in the plateau environment.
- (2)
- For this twisted hydrofoil, the installation angle and flow incidence angle are different at different spans. The incoming flow will cause local high pressure on the lower surface of hydrofoil. There will be a local low pressure site on the foil upper surface due to flow separation. This low pressure will cause cavitation. From sidewall to mid-span, the installation angle increases and the minimum pressure decreases. With the decreasing of Cσ, the size of cavitation extends along the spanwise direction, streamwise direction and thickness direction. The growth rate is high in the spanwise (cavity width) and streamwise (cavity length) directions and low in thickness direction. When the size of cavitation is large enough, it will be broken by backflow-jet flow. A tail generates and the cavity becomes relatively unstable.
Author Contributions
Funding
Institutional Review Board Statement
Informed Consent Statement
Data Availability Statement
Conflicts of Interest
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Altitude Halt | Nuclei Volume Fraction fvnuc |
---|---|
0 m | 5 × 10−4 |
1000 m | 4.38 × 10−4 |
2000 m | 3.88 × 10−4 |
3000 m | 3.48 × 10−4 |
4000 m | 3.01 × 10−4 |
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Luo, H.; Tao, R. Prediction of the Cavitation over a Twisted Hydrofoil Considering the Nuclei Fraction Sensitivity at 4000 m Altitude Level. Water 2021, 13, 1938. https://doi.org/10.3390/w13141938
Luo H, Tao R. Prediction of the Cavitation over a Twisted Hydrofoil Considering the Nuclei Fraction Sensitivity at 4000 m Altitude Level. Water. 2021; 13(14):1938. https://doi.org/10.3390/w13141938
Chicago/Turabian StyleLuo, Hongying, and Ran Tao. 2021. "Prediction of the Cavitation over a Twisted Hydrofoil Considering the Nuclei Fraction Sensitivity at 4000 m Altitude Level" Water 13, no. 14: 1938. https://doi.org/10.3390/w13141938
APA StyleLuo, H., & Tao, R. (2021). Prediction of the Cavitation over a Twisted Hydrofoil Considering the Nuclei Fraction Sensitivity at 4000 m Altitude Level. Water, 13(14), 1938. https://doi.org/10.3390/w13141938