SPECIATION OF SOME HEAVY METALS IN BOTTOM SEDIMENTS OF THE OB AND YENISEI ESTUARINE ZONES

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dc.contributor.author Demina L.L.
dc.contributor.author Politova N.V.
dc.contributor.author Levitan M.A.
dc.date.accessioned 2024-11-09T08:38:26Z
dc.date.available 2024-11-09T08:38:26Z
dc.date.issued 2006
dc.identifier https://www.elibrary.ru/item.asp?id=13530454
dc.identifier.citation Geochemistry International, 2006, 44, 2, 182-195
dc.identifier.issn 0016-7029
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/46460
dc.description.abstract The speciation of Fe, Mn, Zn, Cu, Co, Ni, Cr, Pb, and Cd was studied in 52 samples of bottom sediments collected during Cruise 49 of the R/V Dmitrii Mendeleev in estuaries of the Ob and Yenisei rivers in the southwestern Kara Sea. Immediately after sampling, the samples were subjected to on-board consecutive extraction to separate metal species according to their modes of occurrence in the sediments: (1) adsorbed, (2) amorphous Fe-Mn hydroxides and related metals, (3) organic + sulfide, and (4) residual, or lithogenic. The atomic absorption spectroscopy of the extracts was carried out at a stationary laboratory. The distribution of Fe, Zn, Cu, Co, Ni, Cr, Pb, and Cd species is characterized by the predominance of lithogenic or geochemically inert modes (70-95% of the bulk content), in which the metals are bound in terrigenous and clastic mineral particles and organic detritus. About half of the total Mn amount and 15-30% Zn and Cu is contained in geochemically mobile modes. The spatiotemporal variations in the proportions of metal species in the surface layer of sediments along the nearly meridional sections and through the vertical sections of bottom sediments cores testify that Mn and, to a lesser extent, Cu are the most sensitive to changes in the sedimentation environment. The role of their geochemically mobile species notably increases under reducing conditions. © Pleiades Publishing, Inc. 2006.
dc.title SPECIATION OF SOME HEAVY METALS IN BOTTOM SEDIMENTS OF THE OB AND YENISEI ESTUARINE ZONES
dc.type Статья
dc.identifier.doi 10.1134/S0016702906020078


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