In-Situ Measurement of Liberation of a Dissolved Gas in Unsteady Cavitating Flow in Water

Daiki Makii, H. Sasaki, Y. Iga
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引用次数: 1

Abstract

Cavitation is a phenomenon in which phase change occurs in a liquid by pressure decrease due to flow acceleration. The phase change is caused by mainly evaporation of the liquid but sometimes by liberation of dissolved non-condensable gas in the liquid. In particular, unsteady cavitation causes vibration, noise, erosion and performance deterioration, which has been a serious problem in the development of fluid machinery. Therefore, it is important to research the characteristics of cavitation generation and develop methods to suppress or control it. In the current CFD (computational fluid dynamics) model of cavitating flow, the saturated vapor pressure has been used as a criterion for determining the cavitation generation or disappearance based on the idea of phase equilibrium, however it is well known that these calculation results don’t agree well with experimental results. For example, it is reported that the cavitation inception pressure is higher than its saturated vapor pressure in water. This is predicted to be resulting from the generation of gaseous cavitation which is caused by liberation of dissolved air, however this has not been taken into consideration in the current CFD model. Here, liberation of non-condensable gas is supposed to be treated by MD (molecular dynamics) then it is not suitable for CFD. Thus, in order to develop a more accurate CFD model for cavitating flow, it is necessary to develop a macroscopic and coarse-grained model of liberation should be developed, which may be related to flow dynamic-stimulation of the unsteady flow field with cavitation. In the present study, we focus attention on relationship between liberation of dissolved gas and unsteadiness of cavitation. Experiment is conducted in high-temperature water cavitation tunnel in which in-situ measurement of the amount of dissolved oxygen can be performed during the operation with cavitation. The variation of dissolved oxygen is used as one of the indexes of liberation of dissolved non-condensable gas during the experiment. The degree of cavitation unsteadiness is judged by calculation based on the FFT (Fast Fourier Transform) of the downstream fluctuation pressure and the RMS (root mean square) of brightness value using images taken with a high-speed camera. In addition, in order to eliminate the factors of dissolved gas liberation other than cavitation unsteadiness, the mainstream pressure, the mainstream temperature and volume of the cavity are made to be equal, respectively. Under the above preconditions, the time evolution of dissolved oxygen amount is measured in several kinds of cavitating flow fields around NACA0015 and NACA16012 hydrofoils.
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水中非定常空化流动中溶解气体解离的原位测量
空化现象是由于流动加速导致压力降低而导致液体发生相变的现象。相变主要是由液体的蒸发引起的,但有时是由液体中溶解的不可冷凝气体的释放引起的。特别是非定常空化引起的振动、噪声、侵蚀和性能恶化,已成为流体机械发展中的一个严重问题。因此,研究空化产生的特征并开发抑制或控制空化的方法具有重要意义。在目前的CFD(计算流体力学)空化流模型中,基于相平衡的思想,将饱和蒸汽压作为判断空化产生或消失的判据,但众所周知,这些计算结果与实验结果不太吻合。例如,据报道,空化起始压力高于其在水中的饱和蒸汽压。据预测,这是由溶解空气的释放引起的气体空化产生的结果,但在目前的CFD模型中尚未考虑到这一点。在这里,不可冷凝气体的释放被认为是由分子动力学(MD)处理的,因此它不适合CFD。因此,为了建立更精确的空化流CFD模型,有必要建立一个宏观的、粗粒度的解放模型,这可能与非定常流场的空化流动动力刺激有关。在本研究中,我们重点研究了溶解气体的释放与空化非定常的关系。实验在高温水空化隧道中进行,可在空化操作过程中对溶解氧进行现场测量。在实验过程中,溶解氧的变化作为溶解不凝气体释放的指标之一。利用高速相机拍摄的图像,通过对下游波动压力的快速傅里叶变换和亮度值的均方根值进行计算,判断空化不稳定程度。此外,为了消除空化不稳定以外的溶解气体释放因素,将空腔的主流压力、主流温度和主流体积分别设置为相等。在上述前提条件下,测量了NACA0015和NACA16012水翼周围几种空化流场中溶解氧量的时间演变。
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