3

being returnedto theseislands. It became appar-

ent that a special vessel was needed. and in 1973
the AEC arranged for the Army to provide an

LCU(landing craft utility) based and maintained
at Kwajalein (with AEC funding). This vessel,

though small andslow, has the distinct advantage
that it can be beached,so that ship-to-shore trans-

wardthe district centers, and the ‘‘homeislands”

are left with children and old people. A recent survey on Rongelap showed thatofits 167 people,
115 were <15 years old and 30 were >50. The
flux is great: during any given field trip up to 30
people maybearriving or leaving.
The district has opened up to foreign travel.

fer of equipment and personnel by small boatis
unnecessary. Three 30-ft air-conditioned trailers

Majuro has a jetairport, paved roads,electricity,

as a “sleeper,” one containing a whole-body
counter (shadow-shield lead assembly andelectronic equipment), and oneset upforclinical examinations with a doctor’s office, a small labora-

demand,dissatisfaction is more vocal.

have been placed on the tank deck, one equipped

tory, and an x-ray facility. The LCU with these
trailers is now in full use and affords tremendous
improvements in the operations.
Examination facilities at Utirik consist of several

Butler-type buildings left by a weather station
group. On Rongelap several examinationtrailers
have beeninstalled so that the schoolhouse need

no longer be used. Examinations trailers have also
been installed on Ebeye and Majuro.
Major events in the Marshall Islands related to
the surveys, includingthe political problems of the
past few years, are summarized in Appendix 1.
Before and after each survey, village meetings
have always been held on Rongelap and Utirik to
inform the peopleofthe objectives of the examinations, the findings, and recommended treatments.
Because of the language barrier, the people did
not always understand the need for the examinations, or their results. Every effort is now being
madeto correct this. Preparation of a questionand-answer booklet on theeffects of the fallout

and treatment on the Rongelap and Utirik people
was recommended by the Congress of Micronesia;
such a booklet has been printed at BNLfor the
Trust Territory Health Services andis being dis-

tributed; it should do much to correct manyof the

former misconceptions (see Appendix 4).
During the 20 years covered by these reports
drastic changes have occurred in the Marshall
Islands District.
The population more than doubled from 1948
to 1973,the total going from ~ 10,000 to ~ 25,000.
The increases were most dramatic on Majuro (go-

ing from 1,200 to 10,300) and on Ebeye (going
from 750 to 5,000). On the outer islands the total

population changedless (Rongelap, 100 to 167;

Utirik, 126 to 217), but the age distribution became abnormal. Youngadults have gravitated to-

S006 102

and telephones. Expectationsare rising, and when
public services fail to keep pace with increasing
The atmospheric bomb tests ended in 1958.
Kwajalein was abandoned as a Navy Base in 1960

and was made part of the Army’s missile test

range. For the visiting medical teams, loss of Navy

assistance in transportation has increased the
logistic problems, but the continuing supportof
the Army Base has been invaluable.

The people of Rongelap and Utirik have always

been most friendly and cordial to the medical

team. Except for political interference with the
1972 examinations, the people have always been

cooperative.

:

Il. Initial Findings
A. DOSE ASSESSMENT
1. Source

The radiation exposure of the Marshallese was

due entirely to fallout, since the detonationsite

was too far awayfor thermal, blast, or direct irra-

diation effects. (In constrast, direct effects were re-

sponsibleforail the injuries from the atomic bombs
in Hiroshima and Nagasaki, with little or no fall-

out.) The fireball from the 1954 Bravo device,
detonated from a tower, touched the surface of the

earth at Bikini, and large amounts of material
were drawn up and mixed with fission products in
the bombcloud. Because of an unpredicted shift
in the winds in the upper atmosphere, fallout was
deposited in a cigar-shaped area 20 to 40 miles
wide extending ~200 miles to the east of Bikini
(see Figure 1). The radioactivity was dueto fission
products and some neutron-induced isotopes; the
fallout contained little fissile material. The radiation was therefore almost entirely from gamma
andbetarays of varying energy from numerous
fission radioisotopes. The timeafter detonation
whenfallout began was estimated as 4 to 4 hr at
Rongelap, ~7 hr at Rongerik, and 22 hr at Utirik

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