Composition of surface layer bottom sediments from the Kem' River estuary, White Sea, supplement to: Demina, Lyudmila L; Filip'eva, K V; Shevchenko, Vladimir P; Novigatsky, Alexander N; Filippov, Alexander S (2005): Geochemistry of the bottom sediments in the mixing zone of the Kem' River with the White Sea. Translated from Okeanologiya, 2005, 45(6), 851-865, Oceanology, 45(6), 805-818
Based on grain-size, mineralogical and chemical analyses of samples collected in cruises of R/V Ekolog (Institute of Northern Water Problems, Karelian Research Centre of RAS, Petrozavodsk) in 2001 and 2003 regularities of chemical element distribution in surface layer bottom sediments of the Kem...
| Main Authors: | , , , , |
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| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
PANGAEA - Data Publisher for Earth & Environmental Science
2005
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| Subjects: | |
| Online Access: | https://dx.doi.org/10.1594/pangaea.762830 https://doi.pangaea.de/10.1594/PANGAEA.762830 |
| Summary: | Based on grain-size, mineralogical and chemical analyses of samples collected in cruises of R/V Ekolog (Institute of Northern Water Problems, Karelian Research Centre of RAS, Petrozavodsk) in 2001 and 2003 regularities of chemical element distribution in surface layer bottom sediments of the Kem' River Estuary in the White Sea were studied. For some toxic elements labile and refractory forms were determined. Correlation analysis was carried out and ratios Me/Al were calculated as proxies of terrigenous contribution. Distribution of such elements as Fe, Mn, Zn, Cr, Ti was revealed to be influenced by natural factors, mainly by grain size composition of bottom sediments. These metals have a tendency for accumulation in fine-grained sediments with elevated organic carbon contents. Distribution of Ni is different from one of Fe, Mn, Zn, Cr, Ti. An assumption was made that these distinctions were caused by anthropogenic influence. |
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