Domanov, Mikhail M; Kontar', Evgeny A; Kosyan, Ruben D; Sapozhnikov, Dmitry A; Shimkus, Kazimir M (1996): Cs-137 and Co-60 isotopes and sedimentation rates in Late Holcene sediments from the Northwestern Black Sea [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.759687, Supplement to: Domanov, MM et al. (1996): Anthropogenic radionuclides in Northwestern Black Sea sediments. Translated from Okeanologiya, 1996, 36(4), 550-555, Oceanology, 36(4), 516-520
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Published: 1996 (exact date unknown) • DOI registered: 2011-05-19
Abstract:
Results of measurements of Cs-137 and Co-60 concentrations in bottom sediments of the Northwestern Black Sea indicate inhomogenity of their distribution both over the studied area and along sediment cores. Intermittency of sediment layers with different concentration of radionuclides in the cores reflects active horizontal movements and redistribution of sediments on the shelf and continental slope. As a result sediment layers dated by the Chernobyl mark as seven years old were found in the 5-7 cm depth layer. Maximum Cs-137 concentration in the surface sedimentary layer on the shelf was 42 mBq/g. Maximum Co-60 concentration of 1320 mBq/g was measured due to a hot particle. No correlation was found between Cs-137 and the Co-60 contents.
Project(s):
Archive of Ocean Data (ARCOD)
Coverage:
Median Latitude: 44.973975 * Median Longitude: 32.160317 * South-bound Latitude: 44.460000 * West-bound Longitude: 31.700000 * North-bound Latitude: 45.500000 * East-bound Longitude: 32.650000
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
- Domanov, MM; Kontar', EA; Kosyan, RD et al. (1996): (Table 1) Concentrations of Cs-137 and Co-60 radionuclides in bottom sediments from the Northwestern Black Sea. https://doi.org/10.1594/PANGAEA.759739
- Domanov, MM; Kontar', EA; Kosyan, RD et al. (1996): (Table 2) Sediment characteristics and sedimentation rates in the Northwestern Black Sea during Late Holocene (0-3 ka). https://doi.org/10.1594/PANGAEA.759683