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Dependence of the ion fractionation coefficient in sea aerosols on the rate of evaporation from the sea surface

M.R. Kuznetsova, E.V. Karavaeva, V.A. Tverdislov

Moscow University Physics Bulletin 1992. 47. N 5. P. 82

  • Article
Annotation

It is shown that the difference between the chemical composition of sea aerosols and that of sea water may be due to irreversible processes of heat and mass exchange between the ocean and the atmosphere. These processes may cause changes in the chemical composition of the ocean surface microlayer, which generates aerosols.

Rissian citation:
М.Р. Кузнецова, Е.В. Караваева, В.А. Твердислов.
Зависимость коэффициента фракционирования ионов в морских аэрозолях от интенсивности испарения с поверхности моря.
Вестн. Моск. ун-та. Сер. 3. Физ. Астрон. 1992. № 5. С. 85.
Authors
M.R. Kuznetsova, E.V. Karavaeva, V.A. Tverdislov
Department of Physics of Atmosphere and Mathematical Geophysics, Faculty of Physics, Moscow State University, Leninskie Gory, Moscow, 119992, Russia
Issue 5, 1992

Moscow University Physics Bulletin

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