School of Jet Propulsion, Beihang University, Beijing 100191, People's Republic of China.
J Acoust Soc Am. 2010 Mar;127(3):1251-7. doi: 10.1121/1.3291001.
A time evolution analysis is presented for the interaction between the instability waves, shock cells, and screech tones based on the authors' previous numerical simulation database. An attachment and reinforcement process of the upstream propagating screech waves with the downstream hydrodynamic waves is identified and recognized as part of the screech loop. The first five shock cells are recognized as the effective sound source region. Through an analysis of the phase variation in the dominant pressure fluctuations for several typical Mach number screeching jets, it is found that the total number of the instability waves and the upstream feedback sound waves in the effective source region can be identified as 5 for the A1, B, and D modes and 6 for A2 and C modes, respectively. A screech tone frequency prediction formula is thus proposed based on this relation. The predicted screech wavelengths or Strouhal numbers of cold and hot jets all agree well with the experimental data by other researchers, except for a small discrepancy for the B mode. It is also noticed that the measured two A0 modes by Ponton et al. [NASA Technical Memorandum No. 113137, Langley Research Center (1997)] can be classified to A1 and A2 modes, respectively, according to the proposed formula.
提出了一种基于作者先前数值模拟数据库的不稳定性波、激波单元和啸叫声相互作用的时变分析方法。识别并确认上游传播的啸叫声与下游流体动力波的附着和增强过程是啸叫声环的一部分。前五个激波单元被认为是有效的声源区域。通过对几个典型马赫数啸叫射流主要压力脉动的相位变化进行分析,发现有效声源区域中不稳定性波和上游反馈声波的总数可以分别确定为 A1、B 和 D 模式的 5 个,以及 A2 和 C 模式的 6 个。因此,提出了一个基于此关系的啸叫声频率预测公式。所预测的冷、热射流的啸叫声波长或斯特劳哈尔数与其他研究人员的实验数据吻合良好,除了 B 模式存在较小的差异。还注意到,根据所提出的公式,Ponton 等人测量的两个 A0 模式[NASA 技术备忘录 No. 113137,兰利研究中心(1997 年)]可以分别归类为 A1 和 A2 模式。