On the basis of this investigation, the following islands are
- extremely unlikely to have received fallout from the Bikini or Enewetak
tests at levels higher than the background exposure of 209 mrem/yeer:
Wotto
Ujae
Lae
Lib
Majuro
Namorik
Kusaie
pbc
i
otje
Erikubd
‘Naloelap
Arno
Kili
Kwajalein
Aur
Namu
Jabwot
Ailinglanalap
Mi1i
Narik
Jaluit
Ebor,
and any other islands circumscribed by the above.
The following islands may have received some fall&ut from
muclear tests.
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:
Jem
.
Ai luk
Mejit
The following istands did receive faliout with intensities
ranging from 1 to 2003 R/hr at lJ hr.
They are listed in estimetec
order of decreasing residual activity:
Rongelap
.
Taongi (based on cloud drift only - no survey data available)
Rongerik
Ailinginae
Bikar
Utirik
Taka
WI.
CONCLUSIONS
DOE ARCHIVES
The above estimates, even when corrected for soil migration,
can only be considered preliminary; they are very likely to be upper
bounds. Note that only csi3? has been considered. The addition of
gr90 (a beta-emitter) and ¢60 (which results from weapon debris activation) are necessary in completing the estimates of the total activity
a,
present.