Deposition of Dispersed Particles in Isotropic Turbulent Flow

Particle deposition in turbulent flow depends on diffusional migrations and gravitational forces. However, the rate of this process occurs differently in vertical and horizontal flows. Therefore, some new expressions were suggested for these two types of flow in this article. Moreover, impact of the coalescence and break‐up phenomena on deposition was investigated. Suggested equations were compared with the experimental data taken from the literature and a good agreement was recorded.

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