Resonance of an object floating within a surface wavefield
Sébastien Kuchly, Wilson Reino, Kyle McKee, Stéphane Perrard, Giuseppe Pucci, Antonin Eddi
TL;DR
We investigate the resonance of a buoyant cylinder in a gravity-wave field, focusing on its natural heave frequency and how it depends on radius $R$, height $h$, and the density ratio $\rho/\rho_w$. Using impulsive vertical perturbations and surface-field reconstruction with Fast Checkerboard Demodulation, the authors extract a Lorentzian resonance peak at frequency $f_0$ and a damping parameter $\mu$, with $f_0$ approximately following $f_0 \approx \frac{1}{2\pi}\sqrt{\frac{\rho_w g}{\rho h}}$ in the simple limit and showing $f_0 \propto (hR)^{-0.22}$ experimentally. In an external wavefield, the floater radiates and diffracts incident waves, and the transverse emission is minimized when the forcing frequency is near $f_0$, with $f_{\min} \approx f_0$. The results provide a framework for understanding energy redistribution in larger systems such as sea-ice floes and inform modeling of wave–structure interactions in coastal engineering.
Abstract
We examine the interaction between floating cylindrical objects and surface waves in the gravity regime. Since the impact of resonance phenomena associated with floating bodies, particularly at laboratory scales, remains underexplored, we focus on the influence of the floats' resonance frequency on wave emission. First, we study the response of floating rigid cylinders to external mechanical perturbations. Using an optical reconstruction technique to measure surface wave fields in both space and time, we study the natural resonance frequency of floats with different sizes. The results indicate that the resonance frequency is influenced by the interplay between the cylinder geometry and the solid-to-fluid density ratio. Second, these floating objects are placed in an incoming wave field. These experiments demonstrate that floats diffract incoming waves, while radiating secondary waves that interfere with the incident wavefield. Minimal wave generation is observed at resonance frequencies. These findings can provide insights for elucidating the behavior of larger structures, such as sea ice floes, in natural wave fields.
