Migration of radionuclides following shallow land burial
Description:
A study of radionuclide migration was conducted at a facility used from 1944 to 1949 for the shallow land burial of radwaste produced during operations with two reactors and related nuclear research. It is situated in glacial drift 45 m thick. Underlying the drift is a generally level Silurian dolomite bedrock 60 m thick. The thickness of the drift decreases as the surface slopes downhill (north) until the dolomite reaches the surface and forms the bed of a river, 700 m to the north. This study…
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Date:
January 1, 1980
Creator:
Sedlet, J. & Golchert, N.W.
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Partner:
UNT Libraries Government Documents Department