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The Forms of Occurrence of Trace Elements in Natural Waters of the Aquatic Formations of the Moscow Canal and the Volga–Baltic System

Authors
  • Lipatnikova, O. A.1
  • Lubkova, T. N.1
  • 1 Department of Geology, Moscow State University, Moscow, 119991, Russia , Moscow (Russia)
Type
Published Article
Journal
Moscow University Geology Bulletin
Publisher
Pleiades Publishing
Publication Date
Mar 01, 2021
Volume
76
Issue
2
Pages
215–222
Identifiers
DOI: 10.3103/S0145875221020058
Source
Springer Nature
Keywords
Disciplines
  • Article
License
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Abstract

AbstractBased on previously obtained hydrochemical data on the reservoirs of the Moscow Canal, the Uglich, Rybinsk, Sheksna, Vytegra, and Belousovo reservoirs along with Lake Onega, thermodynamic calculations were carried out for the forms of the occurrence of trace elements in the waters of these basins. It has been shown that the prevailing forms were represented by free ions for Sr, Ba, Fe, Mn, Zn, Ni, Co, and Cd, fulvate complexes for Cu, as well as carbonate and fulvate complexes for Pb.

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