Email this article Contribution of Ion Exchange Transformation of the Adsorbed Complex of Atmospheric Aerosols to the Formation of Seawater Salt Composition
- Authors: Savenko V.S.1, Savenko A.V.2
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Affiliations:
- Faculty of Geography, Moscow State University
- Faculty of Geology, Moscow State University
- Issue: Vol 59, No 4 (2019)
- Pages: 500-503
- Section: Marine Chemistry
- URL: https://bakhtiniada.ru/0001-4370/article/view/149897
- DOI: https://doi.org/10.1134/S0001437019040155
- ID: 149897
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Abstract
Data were summarized on the total exchange capacity and the composition of adsorbed complex of terrigenous aerosols generated in the arid and semiarid land areas. The calculations showed that the changes in composition of the adsorbed complex of aerosols during the interaction with seawater resulted in an additional supply of 2.64–4.86 mln t/year of dissolved Ca2+ along with the removal of 2.45–4.51, 0.73–1.34, and 0.08–0.14 mln t/year of dissolved Na+, K+, and Mg2+, respectively.
About the authors
V. S. Savenko
Faculty of Geography, Moscow State University
Email: Alla_Savenko@rambler.ru
Russian Federation, Moscow
A. V. Savenko
Faculty of Geology, Moscow State University
Author for correspondence.
Email: Alla_Savenko@rambler.ru
Russian Federation, Moscow
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