Speciation of metals in bottom sediments from the south Kara Sea and Ob and Yenisei estuarine zones

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 "Dmitry Mendeleev" to the estuaries of the Ob and Yenisei rivers and to the southwest Kara Sea. Immediately after sampling the samples were subjected to...

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Bibliographic Details
Main Authors: Demina, Lyudmila L, Levitan, Mikhail A, Politova, Nadezhda V
Format: Dataset
Language:English
Published: PANGAEA 2006
Subjects:
Archive of Ocean Data
ARCOD
BC
Box corer
DM49
DM49-4394-1
DM49-4395-1
DM49-4396-1
DM49-4397-2
DM49-4398-1
DM49-4399-1
DM49-4401-3
DM49-4406-1
DM49-4408-1
DM49-4409-1
DM49-4410-1
DM49-4411-1
DM49-4412-1
DM49-4413-1
DM49-4413-3
DM49-4414-2
DM49-4415-2
DM49-4416-1
DM49-4417-2
DM49-4418-1
Dmitry Mendeleev
GC
Grab
Gravity corer
Kara Sea
Men4400-1
Men4402-1
SPASIBAIII
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.725841
https://doi.org/10.1594/PANGAEA.725841
Description
Summary: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 "Dmitry Mendeleev" to the estuaries of the Ob and Yenisei rivers and to the southwest 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. Atomic absorption spectroscopy of the extracts was carried out at a stationary laboratory. Distribution of Fe, Zn, Cu, Co, Ni, Cr, Pb, and Cd species is characterized by predominance of lithogenic or geochemically inert modes (70-95% of bulk contents), in which the metals are bound in terrigenous and clastic mineral particles and organic detritus. About half of total Mn amount and 15-30% of Zn and Cu are contained in geochemically mobile modes. Spatiotemporal variations in proportions of the metal species in the surface layer of sediments along sub-meridional sections and through vertical sections of bottom sediment cores testify that Mn and, to a lesser extent, Cu are the most sensitive to changes in sedimentation environment. The role of their geochemically mobile species notably increases under reducing conditions.

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