期刊
INTERNATIONAL JOURNAL OF MULTIPHASE FLOW
卷 119, 期 -, 页码 56-71出版社
PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.ijmultiphaseflow.2019.07.001
关键词
Particle-turbulence interaction; Sand-laden turbulent boundary layer; Large-scale motions; Particle image/tracking velocimetry
类别
资金
- National Natural Science Foundation of China [11490552, 11672020, 11721202]
Simultaneous two-phase particle image/tracking velocimetry (PIV/PTV) measurements are conducted on a particle-laden turbulent boundary layer (TBL) over a horizontal smooth-flat plate under net sedimentation conditions. Dilute desert sand grains with a median diameter of 203 mu m and bulk volume fraction of O(10(-5)) are used as the discrete phase, and the characteristic Reynolds number of the TBL is relatively high (Re-tau = 5500 based on the friction velocity u(tau) and boundary layer thickness delta). The two-dimensional velocity filed in the streamwise/wall-normal plane is measured by four CCD cameras aligned along the streamwise direction, which resolves a wide spectrum of the scales, ranging from small-scale energetic eddies to large-scale motions (LSMs) in the TBL. An improved phase separation algorithm and discrete particle matching method are developed for two-phase measurements. The results presented here provide new information concerning the effect of high-inertia particles with a dilute concentration on wallbounded turbulence, especially at high Re. Analysis of the velocity spectrum of the gas phase reveals, for the first time, that the presence of sand grains with a size on the order of the Kolmogorov length scale attenuates turbulence fluctuation by suppressing small-scale sweep-ejection cycles in the near-wall region. A critical layer (y/delta=0.12 or y(+) = 670) is found to partition the streamwise evolution of both the local concentration and the streamwise mean velocity of the sand grains into a non-equilibrium nearwall region and a quasi-parallel outer region. In addition, a balance between the strength and probability between the sweep and ejection events of sand grains is reached at this layer. Such a critical layer might be a good indicator of the upper bound of the particle saltation process, in which LSMs are believed to play a significant role. (C) 2019 Elsevier Ltd. All rights reserved.
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