dc.creatorReyes Aspé, Francisco
dc.creatorTorrejón, Vicente
dc.creatorFalcón Beas, Claudio
dc.date.accessioned2020-05-08T22:40:53Z
dc.date.available2020-05-08T22:40:53Z
dc.date.created2020-05-08T22:40:53Z
dc.date.issued2020
dc.identifierPhysical Review E 101, 033106 (2020)
dc.identifier10.1103/PhysRevE.101.033106
dc.identifierhttps://repositorio.uchile.cl/handle/2250/174618
dc.description.abstractWe report on the enhancement of the hydrodynamic damping of gravity waves at the surface of a fluid layer as they interact with a turbulent vortex flow in a sloshing experiment. Gravity surface waves are excited by oscillating horizontally a square container holding our working fluid (water). At the bottom of the container, four impellers in a quadrupole configuration generate a vortex array at moderate to high Reynolds number, which interact with the wave. We measure the surface fluctuations using different optical nonintrusive methods and the local velocity of the flow. In our experimental range, we show that as we increase the angular velocity of the impellers, the gravity wave amplitude decreases without changing the oscillation frequency or generating transverse modes. This wave dissipation enhancement is contrasted with the increase of the turbulent velocity fluctuations from particle image velocimetry measurements via a turbulent viscosity. To rationalize the damping enhancement a periodically forced shallow water model including viscous terms is presented, which is used to calculate the sloshing wave resonance curve. The enhanced viscous dissipation coefficient is found to scale linearly with the measured turbulent viscosity. Hence, the proposed scheme is a good candidate as an active surface gravity wave dampener via vortex flow reconfiguration.
dc.languageen
dc.publisherAmerican Physical Society
dc.rightshttp://creativecommons.org/licenses/by-nc-nd/3.0/cl/
dc.rightsAttribution-NonCommercial-NoDerivs 3.0 Chile
dc.sourcePhysical Review E
dc.subjectShallow-water model
dc.subjectSurface
dc.titleWave damping of a sloshing wave by an interacting turbulent vortex flow
dc.typeArtículo de revista


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