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Yue-Jin Hu

Publications and source records attributed to Yue-Jin Hu.

2 recordsLinked to original sources

The Impact of Turbulence on Hydroacoustic Waves

Traditional research suggests that when sound waves pass through a turbulent region, scattering occurs, causing the incident wave to attenuate and wave parameters to fluctuate. In contrast, our previous paper reported a new phenomenon in which turbulence causes changes in the amplitude of sound waves, a change that cannot be explained by scattering or resonance (HU, K.X, & HU, Y. J. 2025. Hydroacoustic Absorption and Amplification by Turbulence. arXiv:2512.07920). This work presents a more in-depth investigation into the impact of turbulence on hydroacoustic waves, including phase changes, amplification factors and the temporal evolution of the acoustic wave. Experiments indicate that turbulence simultaneously changes both the amplitude and phase of acoustic waves. The total phase shift along the entire pipe equals the sum of the phase shifts of the segments. Both the amplification factor and the phase shift due to turbulence vary periodically with frequency. In pipe flow, after the valve is closed, the temporal evolution of the acoustic waves during the subsequent turbulence decay process can be classified into six types. Acoustic waves with frequencies below and above specific thresholds are essentially unaffected by turbulence. In addition, vortices and unsteady flow in the laminar state do not cause changes in the amplitude and phase of sound waves, showing the essential difference between turbulent fluctuations and the two.

physics.flu-dyn

Hydroacoustic Absorption and Amplification by Turbulence

Acoustic waves propagating through fluid media are significantly influenced by turbulence. This paper experimentally investigates the influence of underwater turbulence on the propagation characteristics of acoustic waves, revealing that acoustic waves can be absorbed or amplified at frequencies far exceeding the turbulent fluctuation frequency. The maximum observed attenuation or amplification of received signals exceeds 60%, with no spectral broadening. The amplification factor depends on the wave frequency rather than its amplitude. The study covers two flow conditions: pipe flow and free jet, driven by either a pump or hydraulic head difference. The frequency range generated by the hydroacoustic transducers covers 60 kHz to 4.4 MHz, while the wave propagation directions both parallel and perpendicular to the mean flow are considered. For each case, the amplitudes of all frequency components simultaneously decreases or increases under turbulence, with no new spectral components appearing. Turbulent fluctuations without mean motion can still alter the wave amplitude, while laminar flow has no effect on acoustic signals. Comparison with conventional theories and experiments indicates that mechanisms such as bubbles, resonance, scattering, or viscous dissipation cannot explain the observed phenomena. This indicates that there exists an incompletely understood new mechanism in the interaction between turbulence and acoustic waves.

physics.flu-dyn