Composition of aerosols collected in the Western Russian Arctic in August-September 1991, supplement to: Shevchenko, Vladimir P; Lisitzin, Alexander P; Kuptsov, Vladimir M; van Malderen, H; Martin, Jean-Marie; van Grieken, R; Huang, W W (1999): Composition of aerosols in the surface boundary layer of the atmosphere over the seas of the Western Russian Arctic. Translated from Okeanologiya, 1999, 39(1), 142-151, Oceanology, 39(1), 128-136

In August-September 1991 during the SPASIBA expedition (Scientific Program on the Arctic and Siberian Aquatorium) aboard R/V Yakov Smirnitzky in the Laptev Sea ten samples of aerosols were collected by nylon nets. A combined approach including various analytical techniques, such as single-particle a...

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Bibliographic Details
Main Authors: Shevchenko, Vladimir P, Lisitzin, Alexander P, Kuptsov, Vladimir M, van Malderen, H, Martin, Jean-Marie, van Grieken, R, Huang, W W
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA - Data Publisher for Earth & Environmental Science 1999
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.760761
https://doi.pangaea.de/10.1594/PANGAEA.760761
Description
Summary:In August-September 1991 during the SPASIBA expedition (Scientific Program on the Arctic and Siberian Aquatorium) aboard R/V Yakov Smirnitzky in the Laptev Sea ten samples of aerosols were collected by nylon nets. A combined approach including various analytical techniques, such as single-particle analysis, instrumental neutron activation analysis, and atomic absorption spectrophotometry, was used to study composition of the samples. Mass concentration of coarse-grained (>0.001 mm) insoluble fraction of aerosols ranged from 80 to 460 ng/m**3. In all the samples remains of land vegetation were found to be the dominant component. Organic carbon content of the aerosols ranged from 23 to 49%. Inorganic part of the samples was represented mainly by alumosilicates and quartz. Anthropogenic ''fly ash'' particles were observed in all the samples. Temporal variations of element concentrations resulted from differences in air masses entering the studied area.