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 Encyclopedia of Physical Science and Technology  En001c-14  May 7, 2001  18:25






               288                                                                                        Aerosols


               by (1) an adiabatic expansion of a gas, (2) the mixing of  production rate of embryos in a homogeneous supersatu-
               a warm, moist gas with a cool gas stream, or (3) chemical  rated vapor is
               reactions producing condensable species. In the absence
                                                                                            ∗
                                                                                I = C exp(
G /kT )
               of particles in a condensable vapor, particles are formed
               by homogeneous nucleation on molecular clusters in a  where 
G is the free energy of formation of critical-sized
                                                                          ∗
               supersaturated vapor. When vapor supersaturation takes  embryos that do not evaporate and C is a rate factor. Ac-
               place in a multicomponent system, mixed particles may  cording to the theory as presented in 1935 by Becker and
                                                                                                2
                                                                                             2
               form from heteromolecular nucleation. When particles ex-  Doring, 
G =−16πσ  3  m /3(kT ) ln S. The rate factor
                                                                           ∗
               ist in a supersaturated vapor mixture, they act as nuclei  is
               for condensation. Perhaps the best known of these pro-                    2/3       1/2
                                                                                2p 0 (n A m )  σ m
               cesses is the formation of clouds in the earth’s atmosphere  C =          1/2
               by water condensation on dust or water-soluble aerosol           (2πm A kT )   kT
               particles.                                        wheren A ismolesofcondensateAandm A isthemolecular
                 The theory of nucleation begins with the consideration  mass of condensate A.
               of vapor–liquid equilibrium. The vapor pressure p 0 over a  The heteromolecular production of particles in a vapor
               flat liquid surface at equilibrium is given by the Clapeyon  mixture is estimated from a model similar to the homoge-
               equation,                                         neous case above. However, the production rate depends
                                         H                       on the energy of formation of mixed embryos, the compo-
                                d ln p 0
                                      =                          sition of which depends on the thermodynamic properties
                                 dT      T  2
                                                                 of the mixture.
               where H is the molar heat of vaporization and   the gas  If particles (or ions) are already present in a supersat-
               constant. At saturation, the vapor pressure p 0 is its equi-  urated vapor, nucleation will take place preferentially on
               librium value at the temperature of the liquid beneath the  these particles at supersaturations far smaller than for the
               vapor. Condensation may take place when the vapor is  homogeneous vapor. In this case, nucleation takes place
               supersaturated or when the supersaturation ratio  heterogeneously on the existing nuclei at a rate depen-
                                                                 dent on the free energy of a condensate cap forming on or
                                S = p/p 0 > 1
                                                                 around the nucleus. Heterogeneous nuclei always occur in
                 The vapor pressure over a pure liquid droplet at equi-  the earth’s atmosphere. They are crucial to the formation
               librium p s depends on its radius of curvature. The Kelvin  of water clouds and to the formation of ice particles in
               equation gives this relationship as:              supercooled clouds.

                                  p s   2σ m
                               ln     =
                                  p 0    RkT                       2. Growth Laws
                 Thus, a supersaturation ratio greater than unity is ex-  The droplet current I calculated by nucleation models
               pected for small droplets at equilibrium with a condens-  represents a limit of initial new phase production. The
               able vapor. The logarithm of this ratio is proportional to  initiation of condensed phase takes place rapidly once a
               the product of the particle surface free energy σ times the  critical supersaturation is achieved in a vapor. The phase
               molecular volume of the liquid ( m ) and inversely propor-  change occurs in seconds or less, normally limited only
               tional to the particle radius R.                  by vapor diffusion to the surface. In many circumstances,
                 The rate of formation of new particles by nucleation is  we are concerned with the evolution of the particle size
               given in terms of a theory for the production of clusters of  distribution well after the formation of new particles or the
               molecules (embryos) in a supersaturated vapor. The pro-  addition of new condensate to nuclei. When the growth or
               duction of embryos follows from considering a population  evaporation of particles is limited by vapor diffusion or
               of molecules and agglomerates of molecules in a homoge-  molecular transport, the growth law is expressed in terms
               neous vapor. There is an energy barrier to producing large  of vapor flux equation, given by Maxwell’s theory, or
               agglomerates that depends on the free energy of formation                      2
                                                                               n∂    n4π D AB R  m (p ∞ − p s )
               of a cluster containing a given number of molecules. As
                                                                       I( , t) =   =
               the supersaturation of a vapor is increased, the free energy     ∂t            kT
               of formation passes through a maximum value such that  Other growth processes are also derived from theory.
               a critical level is attained. Beyond the critical value, em-  They include those associated with chemical reactions to
               bryos of critical size are generated that are stable and grow.  form condensed species taking place either at the parti-
               The “steady” rate of production of embryos of critical size  cle surface or within the particle volume. The growth by
               represents the expected production of new particles. The  surface reactions or a vapor diffusion-limited process is
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