A classical theory of the ternary homogeneous nucleation of sulfuric acid—ammonia—water is presented. For NH3 mixing ratios exceeding 1 ppt, the presence of ammonia enhances the binary (sulfuric acid—water) nucleation rate by several orders of magnitude. However, the limiting component for ternary nucleation—as for binary nucleation—is sulfuric acid. The sulfuric acid concentration needed for significant ternary nucleation is several orders of magnitude below that required in binary case

Korhonen, P.

Kulmala, M.

Laaksonen, A.

McGraw, R.

Seinfeld, J. H.

Viisanen, Y.

English

Caltech Authors - Main

Ternary Nucleation of H2SO4, NH3 and H2O
M. Kulmala1, P.Korhonen1'2, A. Laaksonen3, Y. Viisanen2, R. McGraw4
andJ.H.Seinfeld5
Department of Physics, University of Helsinki, Finland
2Air Quality Research, Finnish Meteorological Institute, Helsinki, Finland
3Department of Applied Physics, University ofKuopio, Finland
4Environmental Chemistry Division, Brookhaven National Laboratory, Upton, New York, USA
5
 Division of Engineering and Applied Science and Department of Chemical Engineering, California
Institute of Technology, USA
Abstract. A classical theory of the ternary homogeneous nucleation of sulfuric acid - ammonia - water is
presented. For NHa mixing ratios exceeding 1 ppt, the presence of ammonia enhances the binary (sulfuric
acid -water) nucleation rate by several orders of magnitude. However, the limiting component for ternary
nucleation - as for binary nucleation - is sulfuric acid. The sulfuric acid concentration needed for
significant ternary nucleation is several orders of magnitude below that required in binary case.
INTRODUCTION
Water vapor is the most abundant gaseous species in the atmosphere that may take
part on the new particle formation. However, for the homogenous nucleation process,
in which new particles form from a single species only, its typical concentrations are
far too small. Thus it is generally accepted that the new particle formation in the
atmosphere occurs via homogenous heteromolecular nucleation process, in which two
or more vapor species form new stable particles. In the past the atmospheric new
particle formation was almost always assumed to take place via binary nucleation of
water (H2O) and sulfuric acid (HiSC^) vapors. Field measurements have been shown
that there exists situations where the new particle formation cannot be explained with
this nucleation route alone [1-3]. Although meteorological factors (e.g. mixing) may
play an important role in some cases, researchers have begun to search for additional
mechanisms that may launch nucleation in the atmospheric conditions. Because the
presence of ammonia in the aerosol particles considerably decreases the vapor pressure
of sulfuric acid above the solution surface [4], it has been suggested, that ammonia
(NH3) forms new particles with sulfuric acid [4] or with sulfuric acid and water [5].
We have recently shown theoretically [6] that ternary nucleation is important
phenomena in the atmosphere. Its importance in aerosol dynamics point of view have
also been studied [7]. In this paper we apply the ternary nucleation model on
atmospheric conditions. We also summarize the ternary nucleation theory and also the
thermodynamics used.
CP534, Nucleation and Atmospheric Aerosols 2000:15th Int. 7 Conf., edited by B. N. Hale and M. Kulmala
© 2000 American Institute of Physics 1-56396-958-0/007$ 17.00
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THEORY FOR THE TERNARY NUCLEATION
In the following we focus on the formation of new particles via nucleation of stable
HiO - NHs - EbSCU clusters. The ternary water - ammonia - sulfuric acid solution
nuclei are assumed to be in the liquid phase. The nucleation rate of stable water-
ammonia- sulfuric acid clusters (7) is obtained from
-AG*7 = Cexp(-^— ) (1)
Here C is a kinetic factor. In this study the minimum work for the critical nucleus
formation is determined using the so called revised classical theory. The minimized
Gibbs free energy change (in the limits of capillarity approximation) is obtained from
f f r * 2 < r J / f l (2)
where r* is the critical radius of the cluster and crs/a is the surface tension. The critical
nucleus composition is obtained from the following equations (Arstila et al., 1998):
(3)
where P/ is the ambient partial vapor pressure of species i, PSii is the equilibrium vapor
pressure of species i above the flat solution surface, r is the radius of the cluster and v/
is the partial molecular volume of species i.
When the critical cluster is formed from water, ammonia and sulfuric acid equation (3)
becomes:
/ \ X
-vwln| Pfl2so4 1 = 0
Here subscript w refers to water, h2so4 to sulfuric acid and nh3 to ammonia. From
equations (4) one can solve the composition of the critical cluster by numerical
iteration. When the composition of the cluster is known, the critical radius is obtained
from the Kelvin equation
(5)
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In this context / refers either water or ammonia or sulfuric acid. We have used
recently presented rigorous kinetic factor for the ternary system [8]. In order to solve
the radius and composition of the critical cluster for the systems presented above, one
needs surface tension (surface free energy), density of the solution and equilibrium
vapor pressures of the various species above the flat solution surface. When the
classical nucleation theory is used, the thermodynamical properties of the nucleus are
assumed to be those of bulk substance in question. Our recent paper [6] summarizes
the thermodynamical model.
RESULTS AND DISCUSSION
According to the present knowledge, the nucleation of new aerosol particles in the
atmospheric conditions in significant extent can occur The results of this model study
suggest that nucleation of water - ammonia - sulfuric acid clusters occurs easier than
the nucleation of water - sulfuric acid clusters in the atmospheric conditions. The
results also suggest that the composition of the critical clusters in the atmospheric
conditions is typically that of water - ammonium bisulfate solution. However, the
formed H2O - NH3 - H2SO4 clusters are very small and highly concentrated: in this
study they appear to be supersaturated with respect to ammonium sulfate almost in
every case we have studied [6].
The nucleation rate is a strong function of sulfuric acid concentration, ammonia
concentration and temperature. In Figure 1 the ternary nucleation rate as a function of
temperature is presented. Sulfuric acid concentration is IxlO6 cm"3 and ammonia
concentration 25 pptv. In Figure 2 the ternary nucleation rate as a function of ammonia
concentration is presented. Sulfuric acid concentration is IxlO5 cm"3 and temperature
278.15 K.
10"
o
c
o
••8
CD
10°
10'
275 280 295 300285 290
T(K)
FIGURE 1. Ternary nucleation rate as a function of temperature. Sulfuric acid concentration is IxlO6 cm"3 and
ammonia concentration 25 pptv.
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10"1 10° 101 102
NH3(ppt)
FIGURE 2. Nucleation rate as a function of ammonia concentration. Sulfuric acid concentration is IxlO5 cm"3 and
temperature 278.15 K.
Although the ternary nucleation is able to predict the formation of new 1 nm
particles, it is not able to predict the formation of 3 nm particles. This is due to the fact
that the sulfuric acid concentration needed in ternary nucleation is too small to be able
to explain the growth of 1 nm particles to 3 nm size [7], and some other vapours are
needed for condensation growth.
REFERENCES
1. Covert D.S., Kapustin V.N., Quinn P.K. and Bates T.S., New Particle Formation in the Marine Boundary
Layer. J. Geophys. Res., 97,20581-20589 (1992).
2. Hoppel W.A., Frick G.M. and Fitzgerald J.W., Marine boundary layer measurements of new particle
formation and the effects nonprecipating clouds have on aerosol size distribution. J. Geophys. Res., 99, 14443-
14495 (1994).
3. Makela" J.M., Aalto P., Jokinen V., Pohja T., Nissinen A., Palmroth S., Markkanen T., Seitsonen K.,
Lihavainen H., Kulmala M., Observations of ultrafme aerosol particle formation and growth in boreal forest.
Geophys. Res. Lett., 1219-1222 (1997).
4. Scott W.D. and Cattell F.C.R., Vapor pressure of ammonium sulfates. Atmos. Env., 13, 307-317 (1979).
5. Coffmann DJ. and Hegg. D.A., A Preliminary study of the effect of ammonia on particle nucleation in the
marine boundary layer. J. Geophys. Res., 100,7147-7160 (1995).
6. KorhonenP., Kulmala M., Laaksonen A., Viisanen Y., McGraw R., Seinfeld J.H., Ternary nucleation of
H2SO4, NH3 and H2O in the atmosphere. J. Geophys. Res., 104, 26349-26353 (1999).
7. Kulmala M., Pirjola L., Makela" J.M., Stable sulphate clusters as a source of new atmsopheric particles. Nature,
404, 66-69 (2000).
8. Arstila H., Korhonen P. and Kulmala M., Ternary Nucleation: Kinetics and application to water - ammonia -
hydrochlorid acid system. Technical note, J. Aerosol Sci. 30,131-138 (1999).
114
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Ternary nucleation of H_2SO_4, NH_3 and H_2O

A Preliminary study of the effect of ammonia on particle nucleation in the marine boundary layer.

Marine boundary layer measurements of new particle formation and the effects nonprecipating clouds have on aerosol size distribution.

Nucleation: Kinetics and application to water - ammonia -hydrochlorid acid system. Technical note,

Observations of ultrafme aerosol particle formation and growth in boreal forest.

Stable sulphate clusters as a source of new atmsopheric particles.

Ternary nucleation of H2SO4, NH3 and H2O in the atmosphere.

Vapor pressure of ammonium sulfates.

https://authors.library.caltech.edu/8930/1/KULaipcp00a.pdf

Ternary nucleation of H_2SO_4, NH_3 and H_2O

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