On the effect of heat of phase transformations on the rate of diffusion processes in drop clouds / B. Sh. Beritashvili, Yu. A. Dovgaliuk.

On the basis of simultaneous solution of equations of diffusion growth and thermal balance of a drop, a formula is given for calculating the rate of its condensation growth and evaporation taking into account the emission of latent heat of condensation, the curvature of the drop surface and the mass...

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Main Authors: Beritashvili, B. Sh (Author), Dovgali︠u︡k, I︠U︡. A. (Author)
Corporate Author: Air Force Cambridge Research Laboratories (U.S.)
Format: Government Document Book
Language:English
Published: L.G. Hanscom Field, Bedford, Massachusetts : Air Force Cambridge Research Laboratories, Air Force Systems Command, United States Air Force, 1971.
Series:AFCRL ; 71-278.
Translations (Air Force Cambridge Research Laboratories (U.S.)) ; no. 92.
Subjects:

MARC

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245 1 0 |a On the effect of heat of phase transformations on the rate of diffusion processes in drop clouds /  |c B. Sh. Beritashvili, Yu. A. Dovgaliuk. 
264 1 |a L.G. Hanscom Field, Bedford, Massachusetts :  |b Air Force Cambridge Research Laboratories, Air Force Systems Command, United States Air Force,  |c 1971. 
300 |a vi, 13 pages :  |b illustrations ;  |c 28 cm. 
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490 1 |a AFCRL ;  |v 71-0278. 
490 1 |a Translations ;  |v No. 92. 
500 |a "7 April 1971." 
500 |a AD0724105 (from http://www.dtic.mil) 
500 |a AFCRL Research Library. 
500 |a Translated from Tiflis. Zakavkazskii Naucho-lssledovatel'skii, Gidrometeorologicheskii Institut. Trudy, Leningrad V. 21, Number 27, pp. 35-44, 1967. 
500 |a "Translated by Transtek Associates, P.O. Box 339, Reading, Mass." 
504 |a Includes bibliographical references (page 13) 
520 |a On the basis of simultaneous solution of equations of diffusion growth and thermal balance of a drop, a formula is given for calculating the rate of its condensation growth and evaporation taking into account the emission of latent heat of condensation, the curvature of the drop surface and the mass of matter dissolved in it. Formulae introduced earlier by other authors are particular cases of the obtained expression. The analysis of the given formula allows one to evaluate the optimum sizes of particles of certain salts which influence drop clouds. 
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