The contribution of fluvial discharge and global fallout of Cs-137 and merc
ury to sedimentation fluxes in Lake Shinji and Lake Nakaumi, Japan, was stu
died. The fluvial flux through soil erosion accounted for 11 to 27% of accu
mulated Cs-137 in the sediments in the 1950's and 1960's, which were the pe
riods of the most extensive atmospheric input, and for 90 to 100 % in the 1
990's. The vertical profiles of mercury concentrations in the lake sediment
s studied showed a maximum between 1959 and 1963, which was originated most
ly from the extensive use of mercury-agrochemicals in paddyfieids of the wa
tershed in the past. These findings are representative examples of long-ter
m contamination of lake sediments caused by the contaminated ground soil er
osion. (C) 1999 Elsevier Science Ltd. All rights reserved.