Published in

American Geophysical Union, Geophysical Research Letters, 17(29), p. 1-1-1-4, 2002

DOI: 10.1029/2001gl014115

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Can soot particles emitted by airplane exhaust contribute to the formation of aviation contrails and cirrus clouds?

Journal article published in 2002 by Carine Alcala-Jornod, Hubert van den Bergh, Michel J. Rossi ORCID
This paper is made freely available by the publisher.
This paper is made freely available by the publisher.

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Abstract

[1] Flame soot samples taken as surrogates for aviation soot have been generated under two limiting conditions of combustion in a rich and lean flame resulting in grey and black soot, respectively. Absolute mean surface residence times tau(s) of H2O adsorbed on soot ranging from 400 to 150 ms have been measured for black soot at 243 K and for grey soot at 193 K, respectively. The kinetic parameters for desorption of H2O adsorbed on grey and black soot are E-a = 7 +/- 0.5 and 9 +/- 0.6 kcal/mol, logA/ s(-1) = 8.8 +/- 0.5 and 8.5 +/- 0.5, respectively. We conclude that soot aerosol may be coated with H2O molecules in a sulfur-free pathway once the particles have cooled down to 500 K in the plume of aviation exhaust.