1975Journal of the Atmospheric SciencesRequires access

Transfer of Particles in Nonisotropic Air Turbulence

M. Caporaloni, Francesco Tampieri, F. Trombetti, O. Vittori

Open publisher page 291 citations

Abstract

The inertia of particles is the basis of the present model of particle “dry deposition” from a turbulent fluid. The basic physical concepts of particle thermal motion as described by Einstein are herein extended to describe the particle motion in nonisotropic turbulence in terms of a “turbophoretic” velocity. The particle transfer from the turbulent fluid to a collecting black surface is therefore described in terms of a differential motion describing the chain of “inertial flights” undergone by the particle under the gradient of turbulence velocity component in the direction of the collecting surface. This model of dry deposition shows satisfactory agreement with experimental values of particle deposition velocity as a function of particle size.

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What this paper is about

The inertia of particles is the basis of the present model of particle “dry deposition” from a turbulent fluid. The basic physical concepts of particle thermal motion as described by Einstein are herein extended to describe the particle motion in nonisotropic turbulence in terms of a “turbophoretic” velocity. The particle transfer from the turbulent fluid to a collecting black surface is therefore described in terms of a differential motion describing the chain of “inertial flights” undergone by the particle under the gradient of turbulence velocity component in the direction of the collecting surface. This model of dry deposition shows satisfactory agreement with experimental values of particle deposition velocity as a function of particle size.

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Available abstract

The inertia of particles is the basis of the present model of particle “dry deposition” from a turbulent fluid. The basic physical concepts of particle thermal motion as described by Einstein are herein extended to describe the particle motion in nonisotropic turbulence in terms of a “turbophoretic” velocity. The particle transfer from the turbulent fluid to a collecting black surface is therefore described in terms of a differential motion describing the chain of “inertial flights” undergone by the particle under the gradient of turbulence velocity component in the direction of the collecting surface. This model of dry deposition shows satisfactory agreement with experimental values of particle deposition velocity as a function of particle size.

Key concepts: Turbulence, Particle (ecology), Mechanics, Physics, Particle deposition, Magnetosphere particle motion, Classical mechanics, K-epsilon turbulence model

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