The Role of Sulfuric Acid in Atmospheric Nucleation

Author:

Sipilä Mikko123,Berndt Torsten1,Petäjä Tuukka2,Brus David45,Vanhanen Joonas2,Stratmann Frank1,Patokoski Johanna2,Mauldin Roy L.6,Hyvärinen Antti-Pekka5,Lihavainen Heikki5,Kulmala Markku27

Affiliation:

1. Leibniz-Institut für Troposphärenforschung e.V., Leipzig 04318, Germany.

2. Department of Physics, 00014 University of Helsinki, Finland.

3. Helsinki Institute of Physics, 00014 University of Helsinki, Finland.

4. Laboratory of Aerosol Chemistry and Physics, Institute of Chemical Process Fundamentals Academy of Sciences of the Czech Republic, Prague 18502, Czech Republic.

5. Finnish Meteorological Institute, Helsinki 00101, Finland.

6. National Center for Atmospheric Research, Boulder, CO 80307, USA.

7. Department of Applied Environmental Science, Stockholm University, Stockholm 10691, Sweden.

Abstract

Little Things Do Matter Gas-phase sulfuric acid is important during atmospheric particle formation, but the mechanisms by which it forms new particles are unclear. Laboratory studies of the binary nucleation of sulfuric acid with water produce particles at rates that are many orders of magnitude too small to explain the concentration of sulfuric acid particles found in the atmosphere. Sipilä et al. (p. 1243 ) now show that gas-phase sulfuric acid does, in fact, undergo nucleation in the presence of water at a rate fast enough to account for the observed abundance of sulfuric acid particles in the atmosphere. These particles, which contain 1 to 2 sulfuric acid molecules each, were not detectable previously, owing to their small size, with diameters as small as 1.5 nanometers.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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