Search Results: "contaminant pathways" OR "radioactivity" OR "models" OR "diet" OR "reindeer/caribou" OR "caesium"

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Yearly intake of 137Cs from various dietary components by the ‘selected’ population of Arctic Sweden Yearly intake of 137Cs from various dietary components by the ‘selected’ population of Arctic Sweden
Integrated deposition density of 90Sr Integrated deposition density of 90Sr
Location of PUNE’s in Arctic Russia Location of PUNE’s in Arctic Russia
Sites where atmospheric testing of nuclear weapons has taken place since 1945 Sites where atmospheric testing of nuclear weapons has taken place since 1945
Annual radiation doses to critical groups from the Loviisa and Olkiluoto NPP’s Annual radiation doses to critical groups from the Loviisa and Olkiluoto NPP’s
Collective doses from the Loviisa and Olkiluoto NPP’s Collective doses from the Loviisa and Olkiluoto NPP’s
Discharges of principle beta-gamma emitters in liquid effluent from Sellafield, 1952-1992 Discharges of principle beta-gamma emitters in liquid effluent from Sellafield, 1952-1992
Discharges of principle alpha emitters in liquid effluent from Sellafield, 1952-1992 Discharges of principle alpha emitters in liquid effluent from Sellafield, 1952-1992
Comparison of doses to critical groups for Sellafield discharges from 1952 to 1993 Comparison of doses to critical groups for Sellafield discharges from 1952 to 1993
Collective dose rates from European nuclear fuel reprocessing plants based on releases up to 1986 Collective dose rates from European nuclear fuel reprocessing plants based on releases up to 1986
Collective dose commitment from nuclear fuel reprocessing activities Collective dose commitment from nuclear fuel reprocessing activities
The system of dams and drainage channels at Mayak The system of dams and drainage channels at Mayak
Changes with time in 90Sr activity concentrations in surface seawater from Greenland waters and the Barents and Kara Seas Changes with time in 90Sr activity concentrations in surface seawater from Greenland waters and the Barents and Kara Seas
An example of a positive feedback loop Warming leads to a decrease in sea ice cover which in turn leads to a decrease in albedo over the ocean, the result of which is further warming and further decreases in the sea ice cover An example of a positive feedback loop Warming leads to a decrease in sea ice cover which in turn leads to a decrease in albedo over the ocean, the result of which is further warming and further [..]
The hydrologic balance in the Arctic is highly dynamic on the seasonal time scale with large and rapid ice melts in the spring On land, this ice and snow melting results in large rapid floods and surges in rivers The hydrologic balance in the Arctic is highly dynamic on the seasonal time scale with large and rapid ice melts in the spring On land, this ice and snow melting results in large rapid floods and [..]

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