FLIT
发表于 2025-3-23 10:30:32
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固执点好
发表于 2025-3-23 16:43:49
Radioactive monitoring principles for marine ecosystems,ot conducted on a routine basis. Institutes of the Former Soviet Union carried out some observations in the Barents and Kara Seas. Other countries sponsored periodic surveys in the Norwegian, North, Irish and Baltic Seas. These surveys provided time series observations on the dynamics of radioactive
好忠告人
发表于 2025-3-23 20:34:14
Conclusion, mammals and fish occupying the upper trophic levels are key organisms for investigating radio-biogeochemical processes in the northern seas and for estimating cumulative effects of environmental radiation. Through our own prolonged research on the ecological impacts from environmental radiation com
Nutrient
发表于 2025-3-23 22:57:05
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类似思想
发表于 2025-3-24 05:38:50
The benthic zone,m on the flux of pollutants from the coastal and pelagic zones is quite evident. The northern seas with shelf depths to 300–600 m are a large reservoir to which radioactive material of different origin is delivered by numerous pathways.
碳水化合物
发表于 2025-3-24 07:30:05
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使厌恶
发表于 2025-3-24 11:40:26
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Malleable
发表于 2025-3-24 15:08:10
History and Methods,ioactivity from Western European nuclear facilities (Kautsky 1980, 1986; Vakulovsky et al. 1985; Nies and Nielsen 1996; Nies et al. 1997, 1998) (Fig. 1.1). The Norwegian Institute of Marine Research investigated the contamination of marketable fish species in the zone of direct impact of the Novaya Zemlya nuclear tests.
cauda-equina
发表于 2025-3-24 19:15:48
Transfer and assimilation of radionuclides in marine ecosystems,mation of contaminants in the marine environment (Izrael end Tsyban 1989; Izrael 1998). According to this approach, every marine ecosystem contains a determinable volume of material (e.g. seawater, sediment, biota) and, therefore, the assimilation capacity of each ecosystem is also finite.
SPER
发表于 2025-3-24 23:30:40
Book 2004ansfer and accumulation of radionuclides in marine sediment and biota of the Northern European seas. Much of the information has been derived through many decades of investigation carried out by the Murmansk Marine Biological Institute. This book presents the original works, augmented and complement