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arXiv 2602.22008physics.flu-dynphysics.ao-ph
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振荡网格强迫对流湍流中惯性颗粒湍流热扩散的实验研究

Experimental study of turbulent thermal diffusion of inertial particles in a convective turbulence forced by oscillating grids

Ben-Gurion University of the Negev(内盖夫本-古里安大学)

E. Elmakies, O. Shildkrot, N. Kleeorin, A. Levy, I. Rogachevskii

AI总结:

通过振荡网格强迫对流湍流实验,研究惯性固体颗粒的湍流热扩散现象,发现有效漂移速度与理论预测一致,且惯性颗粒(直径10 μm)的漂移速度是非惯性颗粒(0.7 μm)的1.5-2.5倍。

摘要:

我们在实验室实验中研究了惯性固体颗粒在由空气中的一个或两个振荡网格强迫的对流湍流中的湍流热扩散现象。湍流热扩散导致颗粒湍流通量的非扩散贡献,该贡献用指向平均流体温度梯度相反方向的有效漂移速度来描述。对于惯性颗粒,该有效漂移速度取决于斯托克斯数和雷诺数。实验中,使用粒子图像测速(PIV)系统测量流体速度和惯性颗粒的空间分布,并通过配备12个热电偶的温度探头在多个位置测量温度场。温度和颗粒数密度空间分布的测量表明,由于湍流热扩散,在平均温度最小值附近形成了惯性颗粒的大尺度团簇。实验中,由湍流热扩散引起的有效漂移速度导致惯性颗粒(直径10 μm)形成大尺度团簇,该速度是非惯性颗粒(直径0.7 μm)的1.5-2.5倍,具体取决于湍流水平。这与理论预测一致。

英文摘要:

We investigate the phenomenon of turbulent thermal diffusion of inertial solid particles in laboratory experiments with convective turbulence forced by one or two oscillating grids in the air. Turbulent thermal diffusion causes a non-diffusive contribution to turbulent flux of particles described in terms of an effective drift velocity directed opposite to the gradient of the mean fluid temperature. For inertial particles, this effective drift velocity depends on the Stokes and Reynolds numbers. In the experiments, fluid velocity and spatial distribution of inertial particles are measured using a Particle Image Velocimetry (PIV) system, and the temperature field is measured in many locations by a temperature probe equipped with 12 thermocouples. Measurements of temperature and particle number density spatial distributions have demonstrated the formation of large-scale clusters of inertial particles in the vicinity of the mean temperature minimum due to turbulent thermal diffusion. In the experiments, the effective drift velocity caused by turbulent thermal diffusion that results in the formation of large-scale clusters of inertial particles (having the diameter $10 μm$) is in 1.5 -- 2.5 times larger than that for noninertial particles (having the diameter $0.7 μm$) depending on the level of turbulence. This is in agreement with the theoretical predictions.

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