On the basis of this investigation, the following is,
ands are
- extremely unlikely to have received fallout from the Bikini f" Enewetak
tests at levels higher than the background exposure of 200 mfem/year:
Wotto
pbc
Aur
Lib
Me juro
‘Haloelap
Arno
AilinBlanateap
Mili
Ujae
Lae
otje
Erikud
Namorik
Kusaie
Kili
Kwajalein
Namu
Jabwok
Narik
Jalui
Ebon
and any other islands circumscribed by the above.
The following islands may have received some fallbutl
muciear tests.
from
It is unlikely that the intensities would have resulted
in an exposure of more than 2 rem the first year; subsequent] annual
exposures would have been less than background:
Jemo
Ai luk
Meji
The following islands did receive fallout with intemsities
ranging from 1 to 2090 R/hr at J hr.
They are listed ines jmatec
order of decreasing residual activity:
Rongelap
Taongi (based on cloud drift only - no survey data
Rongerik
Ailinginae
Bikar
Utirik
Taka
TI.
vailable)
DOE ARCHIVES
CONCLUSIONS
The above estimates, even when corrected for soil
gration,
can only be considered preliminary; they are very likely td be upper
bounds.
Note that only ¢s29? has been considered.
The addi tion of
sr2° (a beta-emitter) and co? (which results from weapon
bris acti-
vation) are necessary in completing the estimates of the tat al activity
owtny
present.