PTseA his)
hsTrae
4a
ye
a,
itiaca Botte
ale ne dee
2 adc
tnd, ait
a -ananietaranbhtceanniniimnanabiaiamsss:
‘
UB
i
a
i
wee
S
=35-
.
5 fon products.
Por filtered well water the decay rate for
® same period was similar, r= t
-1.39.
Another observation
es increased
that the padioactivity of the fresh-water sampl
P
Island
south to north with the activity of the Rongelap
) ple being 1/4, 1/6, and 1/10 of the activity of the freshPer samples from Eniaetok, Labaredj, and Kabelle Islands,
bpectively.