On the basis of this investigation, the following islands are
. extremely unlikely to have received fallout from the Bikini or Enewstak
tests at levels higher than the background exposure of 200 mrem/yeer:
Wotto
poibeiadiee
Ujae
Lae
Lib
Majuro
Namorik
otje
Erikud
Maloelap
Arno
Kili
Kusaie
Kwajalein
Aur
Namu
Jabwot
Ajilinglanalap
Mili
Nar ik
daluit
Ebon
and any other islands circumscribed by the above.
The following islands may have received some falldut from
nuclear tests.
It is unlikely that the intensities would have resulted
in an exposure of more than 2 rem the first year; subsequent annua)
exposures would have been Jess than background:
Jemo
Ailuk
Mejit
The following islands did receive fallout with intensities
ranging from 1 to 2999 R/hr at J hr.
They are listed in estimatec
order of decreasing residual activity:
Rongelap
Taongi (based on cloud drift only - no survey data availadle)
Rongerik
Ailinginae
Bikar
Utirik
‘Jaka
TTI.
~ 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 cst3? has been considered. The addition of
gr? (a beta-emitter) and 606° (which results from weapon debris acti-
vation) are necessary in completing the estimates of the total activity
wey
present.
36