Experimental study on characteristics of turbulence and sediment transport produced by wind-induced water waves

Abstract

Many researchers and engineers have shown great interest in mass transfer processes produced by wind-induced waves. Such waves contribute significantly to the transfer of environmental materials such as marine debris and sediment, and the turbulence occurring beneath the waves further complicates wave-induced mass transport. The phase cycle of wave motion is generally considered to be a key determinant of mean flow and turbulence. In aqueous environmental engineering, this relationship is a crucial one to investigate, since turbulence is also related to mass transport. To address this question, we measured the time-series of instantaneous velocity vectors by particle image velocimetry (PIV) in a laboratory flume to reveal the turbulence structure induced by wave motion. In a wavelet analysis free of specific assumptions, we were able to decompose the instantaneous velocity data into mean current, wave motion, and turbulence components. This analysis allowed for the objective evaluation of the shear stresses related to wave energy and turbulence energy production. <p>Furthermore, we found significant phase characteristics of energy transfer among mean-velocity, wave, and turbulence components. In order to examine the diffusion and convection properties induced by wind-waves, we also conducted tracking analysis of imaginary sediment markers. Our results support the conclusion that mass transfer induced by wind-waves impacts the entire range of water depths, at least in relatively shallow aqueous environments.

Turbulence Affected by Submerged Auqatic Vegetation under Wind- induced Flow

“…Because the micro-breaking of wave and their shape is strongly influenced by wind stress, previous proposed methods like phase averaging and moving average technique are not applicable in this experiment. This study employed spectral analysis to separate waveinduced velocity within instantaneous velocities (Sanjou and Sugihara 2023). Assuming that velocities within a specific frequency range are exclusively induced by wind wave, while the remaining frequencies originate from turbulence, separation of these contributions is achieved through filtering method.…”