Wave damping of a sloshing wave by an interacting turbulent vortex flow

被引:1
作者
Reyes, Francisco [1 ]
Torrejon, Vicente [1 ]
Falcon, Claudio [1 ,2 ]
机构
[1] Univ Chile, Fac Ciencias Fis & Matemat, Dept Fis, Casilla 487-3, Santiago, Chile
[2] Millenium Nucl Soft Smart Mech Metamat, Santiago, Chile
关键词
SHALLOW-WATER MODEL; SURFACE;
D O I
10.1103/PhysRevE.101.033106
中图分类号
O35 [流体力学]; O53 [等离子体物理学];
学科分类号
070204 ; 080103 ; 080704 ;
摘要
We 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.
引用
收藏
页数:6
相关论文
共 24 条
[1]  
Anderson JG, 2000, J SOUND VIB, V232, P839, DOI 10.1016/jsvi.1999.2248
[2]  
[Anonymous], COURSE THEORETICAL P
[3]  
[Anonymous], 1964, HOUILLE BLANCHE, DOI DOI 10.1051/LHB/1964038
[4]  
Boyev A. G., 1971, IZV AS ATMOS OCEAN P, V7, P31
[5]   Existence of global weak solutions for a 2D viscous shallow water equations and convergence to the quasi-geostrophic model [J].
Bresch, D ;
Desjardins, B .
COMMUNICATIONS IN MATHEMATICAL PHYSICS, 2003, 238 (1-2) :211-223
[6]   Wave-Vortex Interactions in Fluids and Superfluids [J].
Buhler, Oliver .
ANNUAL REVIEW OF FLUID MECHANICS, 2010, 42 :205-228
[7]   Global measurement of water waves by Fourier transform profilometry [J].
Cobelli, Pablo Javier ;
Maurel, Agnes ;
Pagneux, Vincent ;
Petitjeans, Philippe .
EXPERIMENTS IN FLUIDS, 2009, 46 (06) :1037-1047
[8]   Laboratory investigation of damping of gravity-capillary waves on the surface of turbulized liquid [J].
Ermakov, S. A. ;
Kapustin, I. A. ;
Shomina, O. V. .
IZVESTIYA ATMOSPHERIC AND OCEANIC PHYSICS, 2014, 50 (02) :204-212
[9]   Wave-vortex interaction [J].
Falcon, Claudio ;
Fauve, Stephan .
PHYSICAL REVIEW E, 2009, 80 (05)
[10]   MEASUREMENTS OF SURFACE-WAVE DECAY DUE TO UNDERWATER TURBULENCE [J].
GREEN, T ;
PAQUIN, JE ;
MEDWIN, H .
NATURE-PHYSICAL SCIENCE, 1972, 237 (77) :115-&