Koukina, S E; Korneeva, Galina A; Bek, T A (2010): Composition of littoral bottom sediments from the Kandalaksha Bay (Whire Sea), labile and lithogenic forms of metals [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.764038, Supplement to: Koukina, SE et al. (2010): Forms of metals in the littoral sediments in Kandalaksha Bay of the White Sea in the Russian Arctic. Translated from Okeanologiya, 2010, 50(6), 926-932, Oceanology, 50(6), 877-883, https://doi.org/10.1134/S000143701006007X
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Published: 2010 (exact date unknown) • DOI registered: 2011-09-16
Abstract:
According to results of a comparative study carried out on sediment sampled from littoral zones of small inlets in the Kandalaksha Bay (White Sea) metals (Fe, Mn, Cu, Zn, Pb, Cr, and Li) occur mainly in biogeochemically stable mineral incorporated forms that comprise 77-99% of total metal concentrations. Average percentages of labile forms easily extracted by weak acid of total concentrations are 3.2% for Fe, 2.0% for Mn, 1.7% for Cr, 5.6% for Pb, 5.8% for Zn, 6.5% for Cu, and is negligible for Li. Concentrations of the most studied trace metals are below the threshold level according to environmental quality guidelines (sediment analysis). The percentages of metal forms evidence natural origin of elevated concentrations of both Zn and Cr in studied sediments.
Project(s):
Archive of Ocean Data (ARCOD)
Coverage:
Median Latitude: 66.531297 * Median Longitude: 33.144509 * South-bound Latitude: 66.470800 * West-bound Longitude: 32.828200 * North-bound Latitude: 66.593200 * East-bound Longitude: 33.473700
Event(s):
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
2 datasets
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Datasets listed in this publication series
- Koukina, SE; Korneeva, GA; Bek, TA (2010): (Table 1) Grain size compositions and organic carbon contents in bottom sediments of the Kandalaksha Bay. https://doi.org/10.1594/PANGAEA.764034
- Koukina, SE; Korneeva, GA; Bek, TA (2010): (Table 2) Concentrations of labile and lithogenic forms of metals in dry matter of bottom sediments from the Kandalaksha Bay. https://doi.org/10.1594/PANGAEA.764036