KINEMATICS AND RETURN FLOW IN A CLOSED WAVE FLUME

Proceedings of the International Conference on Coastal Engineering

John H. Nath¹  Jerald D. Ramsden² 

[1] Department of Civil Engineering, Oregon State University;W. M. Keck Laboratory, California Institute of Technology

关键词: wave flume;    closed flume;    wave kinematics;    return flow;   

DOI  :  10.9753/icce.v21.%p

学科分类：建筑学

来源: Coastal Engineering Research Council

【 摘 要 】

Stokes (1847) showed that finite amplitude progressing waves cause a net drift of fluid, in the direction of wave motion, which occurs in the upper portion of the water column. In a closed wave flume this drift must be accompanied by a return flow toward the wave generator to satisfy the conservation of mass. This study presents Eulerian velocity and water surface measurements soon after the onset of wave motion from 12 locations in a large scale flume. Waves with .67 < kh < 2.29 and .09 < H/h < .39 were produced in a water depth of 3.5 meters. Superimposing the return flow theory of Kim (1984) with seventh order stream function theory is shown to improve the velocity predictions. The measured return flows are a function of time and depth and agree with Kim's theory as a first approximation. The mean water surface set-down agrees with the theory of Brevik (1979) except for the nearly deep water waves.

【 授权许可】

Unknown