In the framework of the second Swiss forest soil inventory, Cs-137-activity
from 172 sites was measured systematically for the first time in the topmo
st soil layer (0-5 cm) and represented on a map. The spatial distribution o
f Cs-137 contamination was similar to the pattern observed in 1986 from dos
e equivalent measurements following the Chernobyl nuclear power plant accid
ent. Forest soils from regions with high precipitation in 1986 showed a hig
her Cs-137 activity than regions with low precipitation. At sites with high
caesium activities it was possible to discriminate between Cs-137 originat
ing from global fallout of the fifties and sixties and Cs-137 from the Cher
nobyl accident. The results indicate that radiocaesium persists in the top
soil layers and is recycled in forest ecosystems.