Convection of multi-scale motions in turbulent boundary layer by temporal resolution particle image velocimetry
Convection of multi-scale motions in turbulent boundary layer by temporal resolution particle image velocimetry
复制标题
时间分辨率粒子图像测速研究湍流边界层多尺度运动对流
DOI:
10.1080/14685248.2022.2071429
复制
发表时间:
2022
影响因子:
1.9
通讯作者:
Nan Jiang
中科院分区:
文献类型:
--
作者:
Ziye Fan;Zhanqi Tang;Xingyu Ma;Nan Jiang
Experiments of particle image velocimetry (PIV) in the turbulent boundary layer athave been conducted to investigate the convection characteristic of turbulent structure and the validity of Taylor’s hypothesis. Views of(, the boundary layer thickness) were captured by four streamwise-arranged cameras. Distributions of streamwise turbulent kinetic energy on a streamwise scale were investigated by continuous-wave transform, and scales were found where the portion of streamwise turbulent kinetic energy approaches maximum. Fluctuating velocities (instant velocity minus average velocity on time dimension) were divided into large-scale motion (LSM) and small-scale motion (SSM) portions, bounded by. Convection velocities of LSM and SSM are determined by the spatiotemporal correlation method, and they are larger than local average velocities in near-wall regions, but smaller than local average velocities in wake regions. Statistical characteristics between velocity fields reconstructed by Taylor’s hypothesis and original fields were compared by the autocorrelation method, and the reconstructed field’s patterns are longer than original field’s patterns, while their heights do not have clear distinction. The correlation of original velocity fields and reconstructed fields shows that LSM can hold on overand SSM overin streamwise convection separation for regions of, given a threshold value (correlation coefficientC= 0.6).