LATERAL DIFFUSIVE MIGRATION OF MASSIVE PARTICLES IN HIGH-VELOCITY VERTICAL PIPE-FLOW OF MODERATELY DENSE GAS-SOLID SUSPENSIONS

Citation
P. Zamankhan et al., LATERAL DIFFUSIVE MIGRATION OF MASSIVE PARTICLES IN HIGH-VELOCITY VERTICAL PIPE-FLOW OF MODERATELY DENSE GAS-SOLID SUSPENSIONS, Physical review. E, Statistical physics, plasmas, fluids, and related interdisciplinary topics, 56(3), 1997, pp. 2972-2980
Citations number
43
Categorie Soggetti
Physycs, Mathematical","Phsycs, Fluid & Plasmas
ISSN journal
1063651X
Volume
56
Issue
3
Year of publication
1997
Part
A
Pages
2972 - 2980
Database
ISI
SICI code
1063-651X(1997)56:3<2972:LDMOMP>2.0.ZU;2-W
Abstract
Transport processes involved In a gas-particle flow, comprised of sphe rical particles with a narrow size distribution suspended in a turbule nt gas, are investigated theoretically on the basis of the recently de veloped Enskog theory for multicomponent dense mixtures of slightly sm ooth inelastic spherical particles [P. Zamankhan, Phys. Rev. E 52, 487 7 (1995)]. The generalized Boltzmann equation of the previous work is modified to incorporate the relevant forces exerted upon individual pa rticles including the drag force by the relative gas motion. Extending the method of moments of Grad [Commun. Pure Appl. Math. 2, 331 (1949) ]. the modified Boltzmann equation is solved to obtain the nonequilibr ium velocity distribution function for particles of each size. By taki ng the monodisperse limit, a basic equation is derived for the treatme nt of the problem of lateral diffusive migration of solids in an assem bly composed of separate equisized spherical particles traveling in a fully developed, turbulent upward flow of a gas within a vertical pipe . At moderately high solid concentrations, where the random component of the particle velocity is generated mainly by particle-particle coll isions, the particle diffusivity and the thermal diffusion coefficient are found to increase with the square root of the granular temperatur e, a term that measures the energy of the random motion of the particl es.