Abstract
We report on the observation of gravity-capillary wave turbulence on the surface of a fluid in a high-gravity environment. By using a large-diameter centrifuge, the effective gravity acceleration is tuned up to 20 times Earth’s gravity. The transition frequency between the gravity and capillary regimes is thus increased up to one decade as predicted theoretically. A frequency power-law wave spectrum is observed in each regime and is found to be independent of the gravity level and of the wave steepness. While the timescale separation required by weak turbulence is well verified experimentally regardless of the gravity level, the nonlinear and dissipation timescales are found to be independent of the scale, as a result of the finite size effects of the system (large-scale container modes) that are not taken currently into account theoretically.
- Received 24 April 2019
- Revised 12 July 2019
DOI:https://doi.org/10.1103/PhysRevLett.123.244501
© 2019 American Physical Society
Physics Subject Headings (PhySH)
Synopsis
Probing Wave Turbulence at High Gravity
Published 10 December 2019
A wave experiment in a centrifuge reveals how the size of the fluid container strongly influences turbulent behavior.
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