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Chapitre D'ouvrage Année : 2005

Direct effect of aircraft soot emission: a laboratory view

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Direct effect of aviation on the atmosphere is related to the impact of aircraft soot emission on the contrail formation. A new laboratory approach is elaborated to obtain a more complete knowledge on the potential of aircraft-generated particulates to act as contrail nuclei. A comprehensive examination of the morphology, microstructure, and surface che1nistry of engine soot and its laboratory-made surrogate is performed using various experimental techniques. It is found that engine soot particles may be separated in two components: a main fraction and a fraction of impurities. The high concentration of soluble inorganics and organics stimulate a significant water uptake by soot particles at low temperatures. Possible pathways of the cloud condensation model (CCN) /ice nuclei (IN) formation in the plume are suggested. In the cooling plume, the hydrophilic fraction of impurities of aircraft generated soot would nucleate ice in the condensation-freezing mode, whereas the hydrophobic main fraction allows a direct ice deposition at low temperatures. Insoluble aerosols of the aircraft exhaust would increase the background level of ice nuclei in the upper troposphere (UT) causing the cirrus cloud formation.
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hal-00070979 , version 1 (18-05-2020)

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Olga B. Popovicheva, Natalia M. Persiantseva, Natalia K. Shonija, Benjamin Demirdjian, Daniel Ferry, et al.. Direct effect of aircraft soot emission: a laboratory view. Roy G.D.; Frolov S.M.; Starik. A.M. Non Equilibrium Processes: Vol. 2: Plasma, Aerosols, and Atmospheric Phenomena, Torus Press, pp.215-224, 2005. ⟨hal-00070979⟩
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