Spatial variability of aerosol organic component in the ground layer and in the free atmosphere
N.G. Voronetskaya1, G.S. Pevneva1, A.K. Golovko1, A.S. Kozlov2, M.Yu. Arschinov3, B.D. Belan3, D.V. Simonenkov3, G.N. Tolmachev3
1Institute of Petroleum Chemistry of the Siberian Branch of the RAS, 3, Academichesky ave., Tomsk, 634021, Russia
2V.V. Voevodsky Institute of Chemical Kinetics and Combustion of the Siberian Branch of the RAS, 3 Institutskaya str., 3, 630090, Novosibirsk, Russia
3V.E. Zuev Institute of Atmospheric Optics of Siberian Branch of the Russian Academy of Science, 1, Academician Zuev square, Tomsk, 634021, Russia
Keywords: атмосферный аэрозоль, состав, углеводороды, н-алканы, atmospheric aerosol, composition, hydrocarbons, n-alkanes
Abstract
In work, the composition of alkanes of a linear structure in tests of the atmospheric aerosols, which are selected from a board of the Tu−134 Optic airborne-laboratory in the free atmosphere (500−8500 m) and in the ground layer of air (2 m) near JR-STATION project towers is investigated. It is shown that a homological number of n−alkanes of aerosol tests which are selected from a plane laboratory board, make compounds of 12−28 atoms of carbon, and tests, which are selected in the ground layer — compounds of 14−30 atoms of carbon in a molecule.
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