The Orientation Distribution of Nonspherical Aerosol Particles within a Cloud.

Abstract

Having performed a study on the orientation density function (o.d.f.) of small spheroidal aerosol particles in a general field of an arbitrary strength. It became possible to treat the orientation problem in a turbulent medium. To this end, two interconnected physical models were applied. In the first, The Realizations Model, it was assumed that the turbulent particle field constituted an ensemble of an infinite number of realizations, j, each one of which is characterized by one set of the o.d.f., F(j) (x,t), values. The latter was taken in that model to essentially coincide with previously found solution of the Fokker-Planck equation in the field of the realization. The Micro-turbulence Model, a relation between the so-called turbulent rotational diffusion coefficient of the particles and the physical characteristics of the fluid field was supplied. This coefficient and the Brownian rotational diffusion one, compose the effective diffusion coefficient.

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Document Details

Document Type
Technical Report
Publication Date
Dec 01, 1984
Accession Number
ADA157363

Entities

People

  • I. Gallily

Organizations

  • Hebrew University of Jerusalem

Tags

Communities of Interest

  • C4I

DTIC Thesaurus Topics

  • Aspect Ratio
  • Atmospheric Sciences
  • Boundaries
  • Boundary Layer
  • Coefficients
  • Computational Fluid Dynamics
  • Diffusion
  • Diffusion Coefficient
  • Distribution Functions
  • Equations
  • Experimental Data
  • Layers
  • Orientation (Direction)
  • Particles
  • Simulations
  • Turbulence
  • Turbulent Flow

Readers

  • Aerosol Science/Aerosol Physics
  • Fluid Dynamics.
  • Theoretical Analysis.