The role of collective effects on settling velocity enhancement for inertial particles in turbulence

被引:31
|
作者
Huck, P. D. [1 ,2 ]
Bateson, C. [1 ]
Volk, R. [2 ]
Cartellier, A. [3 ]
Bourgoin, M. [2 ]
Aliseda, A. [1 ]
机构
[1] Univ Washington, Dept Mech Engn, Seattle, WA 98105 USA
[2] Univ Claude Bernard, Univ Lyon, ENS Lyon, CNRS,Lab Phys, F-69007 Lyon, France
[3] Univ Grenoble Alpes, LEGI, F-38058 Grenoble, France
基金
美国国家科学基金会;
关键词
geophysical and geological flows; multiphase and particle-laden flows; particle/fluid flow; HOMOGENEOUS ISOTROPIC TURBULENCE; HEAVY-PARTICLES; PREFERENTIAL CONCENTRATION; AEROSOL-PARTICLES; 2-WAY INTERACTION; SOLID PARTICLES; FLOW-FIELDS; SUSPENSION; DROPLETS; LADEN;
D O I
10.1017/jfm.2018.272
中图分类号
O3 [力学];
学科分类号
08 ; 0801 ;
摘要
A particle-laden homogeneous isotropic turbulent flow is studied experimentally to understand the role of collective effects (e.g. particle-particle aerodynamic interactions caused by local particle accumulation) on the settling velocity of inertial particles (Stokes number: 0.3 < St < 0.6). Conditional averaging of the particle vertical velocity on the local concentration identifies three settling regimes: modest enhancement by single particle-turbulence interactions in low concentration regions, rapid settling velocity increases in clusters at intermediate concentrations and saturation of the settling enhancement at large concentrations. The latter effect, associated with four-way coupling, displays qualitative agreement with simulations in the literature and is a new experimental observation. Fluctuations up to an order of magnitude larger than the background volume fraction are measured using Voronoi analysis. A model is developed following a classic volume-averaged multiphase flow methodology to provide an interpretation of the three settling regimes and quantitative predictions consistent with the measurements.
引用
收藏
页码:1059 / 1075
页数:17
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