Settling velocity of small inertial particles in homogeneous isotropic turbulence from high-resolution DNS

被引:52
|
作者
Rosa, Bogdan [1 ]
Parishani, Hossein [2 ]
Ayala, Orlando [3 ]
Wang, Lian-Ping [4 ,5 ]
机构
[1] Natl Res Inst, Inst Meteorol & Water Management, 61 Podlesna St, PL-01673 Warsaw, Poland
[2] Univ Calif Irvine, Dept Earth Syst Sci, Irvine, CA 92697 USA
[3] Old Dominion Univ, Dept Engn Technol, 214 Kaufman Hall, Norfolk, VA 23529 USA
[4] Univ Delaware, Dept Mech Engn, Newark, DE 19716 USA
[5] Huazhong Univ Sci & Technol, State Key Lab Coal Combust, Wuhan 430074, Peoples R China
基金
美国国家科学基金会;
关键词
Settling velocity; Inertial particles; Cloud droplets; Turbulence; DNS; DIRECT NUMERICAL SIMULATIONS; CELLULAR-FLOW FIELDS; HEAVY-PARTICLES; PREFERENTIAL CONCENTRATION; SEDIMENT TRANSPORT; AEROSOL-PARTICLES; CLOUD DROPLETS; NONLINEAR DRAG; MOTION; COLLISION;
D O I
10.1016/j.ijmultiphaseflow.2016.04.005
中图分类号
O3 [力学];
学科分类号
08 ; 0801 ;
摘要
The gravitational settling velocity of small heavy particles in a three-dimensional turbulent flow remains a controversial topic. In a homogeneous turbulence of zero mean velocity, both enhanced settling velocity and reduced settling velocity have been reported relative to the still-fluid terminal velocity. Dominant mechanisms for enhanced settling include the preferential sweeping and particle-particle hydrodynamic interactions. The reduced settling could result from loitering (falling particles spend more time in the regions with upward flow), vortex trapping, and drag nonlinearity. Here high-resolution direct numerical simulations (DNS) are used to investigate the settling velocity of non-interacting small heavy particles, for an extended range of flow Taylor microscale Reynolds numbers (up to R-lambda = 500) with varying particle terminal velocity (relative to the Kolmogorov velocity) and particle inertia, by changing the particle-to fluid density ratio and energy dissipation rate. For the parameter regimes considered here, the preferential sweeping has a dominant effect leading to an increase of the average settling velocity relative to the terminal velocity; and this increase is mainly governed by particle Froude number (the ratio between the particle inertial response time and the residence time of the particle in a Kolmogorov eddy) and its magnitude depends linearly on the square root of the energy dissipation rate. The reduction of settling due to loitering rarely occurs in a homogeneous turbulence without organized large-scale vortical structures, but is found to emerge only if the particle horizontal motions are blocked (thus removing the preferential sweeping effect), as shown in Good et al. (2014). The DNS results were used to develop a parameterization that relates the settling velocity to the particle inertia (St), Froude number, and R-lambda. Finally, sensitivities of the DNS results to the large-scale forcing method and to the drag nonlinearity are also briefly discussed. (C) 2016 Elsevier Ltd. All rights reserved.
引用
收藏
页码:217 / 231
页数:15
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