Brief Report

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.

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

Science News of the Faculty of Physics, Lomonosov Moscow State University

This new information publication, which is intended to convey to the staff, students and graduate students, faculty colleagues and partners of the main achievements of scientists and scientific information on the events in the life of university physicists.