Sediments collected from the Techa River at Nadirov Bridge were analys
ed for Tc-99. The maximum concentration was found at a depth of 14-18
cm. This layer was sedimented around 1950, i.e. at a time when the max
imum releases of waterborne radionuclides occurred to the river from t
he MAYAK plutonium production plant in the Urals. The vertical distrib
ution of Tc-99 in sediments followed that of Cs-137, and the mean rati
o between Tc-99 and Cs-137 in the sediments at the time of discharge w
as 0.41 x 10(-3). Laboratory experiments showed that Tc-99 under anoxi
c conditions, e.g. when organic material is decomposing, will be retai
ned br sediments. (C) 1997 Elsevier Science Ltd.