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author Shul'kin, Vladimir M
Bogdanova, Natalia N
author_facet Shul'kin, Vladimir M
Bogdanova, Natalia N
collection Datos científicos de ciencias marinas y ambientales
contents Changes in concentration levels and speciation of heavy metals during sedimentation on example of a typical semi-closed bay, where bottom sediments have formed due to river run-off, are under consideration. It is shown that due to desorption of mobile manganese, zinc and copper entered the bay with river suspended matter, their total contents in bottom sediments decrease and percentages of lithogenic forms increase. Contents and speciation of iron in bottom sediments are determined by its participation in coagulation of river colloids in the mixing zone and by mechanical differentiation of sedimentary material.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_778160
institution PANGAEA
language en
publishDate 1984
publisher PANGAEA
record_format pangaea
spellingShingle (Table 1) Grain size composition and heavy metal speciations in bottom sediments of the Ussuri Bay, Sea of Japan
Shul'kin, Vladimir M
Bogdanova, Natalia N
Archive of Ocean Data; ARCOD; Atomic absorption spectrometry (AAS); Calculated; Copper; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Event label; GC; Grab; GRAB; Grain size analysis after Petelin (1967, Nauka, Moscow); Gravity corer; Iron; Latitude of event; Longitude of event; Manganese; SHB80-4; SHB80-5; SHB80-6; SHB80-7; SHBUB-1; SHBUB-2; SHBUB-4; SHBUB-5; SHBUB-6; Size fraction < 0.001 mm, clay; Size fraction > 0.100 mm; Size fraction 0.010-0.001 mm; Size fraction 0.100-0.010 mm; Sum; Ussuri Bay, Sea of Japan; Zinc
Changes in concentration levels and speciation of heavy metals during sedimentation on example of a typical semi-closed bay, where bottom sediments have formed due to river run-off, are under consideration. It is shown that due to desorption of mobile manganese, zinc and copper entered the bay with river suspended matter, their total contents in bottom sediments decrease and percentages of lithogenic forms increase. Contents and speciation of iron in bottom sediments are determined by its participation in coagulation of river colloids in the mixing zone and by mechanical differentiation of sedimentary material.
title (Table 1) Grain size composition and heavy metal speciations in bottom sediments of the Ussuri Bay, Sea of Japan
topic Archive of Ocean Data; ARCOD; Atomic absorption spectrometry (AAS); Calculated; Copper; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Event label; GC; Grab; GRAB; Grain size analysis after Petelin (1967, Nauka, Moscow); Gravity corer; Iron; Latitude of event; Longitude of event; Manganese; SHB80-4; SHB80-5; SHB80-6; SHB80-7; SHBUB-1; SHBUB-2; SHBUB-4; SHBUB-5; SHBUB-6; Size fraction < 0.001 mm, clay; Size fraction > 0.100 mm; Size fraction 0.010-0.001 mm; Size fraction 0.100-0.010 mm; Sum; Ussuri Bay, Sea of Japan; Zinc
url https://doi.org/10.1594/PANGAEA.778160