waivers granted were not utilized.

For TG 7.5, 14.2 percent exceeded the

MPE, with less than 3 percent covered by waivers

(Reference 17, p.

§0).

The Commander, TG 7.1, soon realized the deteriorating situatiog

and

decided to relieve any TG 7.1 or TG 7.5 individuals exceeding 6.0 RJof
duty and return them to the United States.

This policy greatly ass4sted

the Control Group in minimizing personnel exposures.

Radsafe Monitoring and Instrumentation
The overall radiation protection plan was based on the premise that
Enewetak Atoll was the primary base of operation and Bikini was the

ward shot area (Reference 22, Appendix B).

fFor-

All personnel working at

kini were evacuated from the atoll before each shot (except for the
detonation firing party).*

The ships, with evacuees, were stationedfout-

side of the anticipated fallout area.

All islands near the shot point

were considered too contaminated for reentry until cleared by a radsdafe

survey.
RADSAFE INSTRUMENTATION.

The standard radsafe survey meter used

TU 7 was the AN/PDR-39 ion chamber.*

by

Other instruments in use includgd the

AN/PDR T1B and the AN/PDR-18A or -18B ion chamber, for survey in highly
contaminated areas, and lower range Geiger-Mueller type instruments c@nsisting of various models of the AN/PDR-27, the Beckman MX-5, and the[Nuclear Corporation 2610

(Reference 17, p. 42).

* For the NECTAR shot on Enewetak, no evacuation was necessary.
The
vice was not detonated until it was determined that fallout radiati
would not contaminate the inhabited islands of the atoll.

T The Navy's Bureau of Ships was responsible for procuring and distrib
ting sufficient radiac equipment for all elements of TG 7.3 to have
full complement.

A complete accounting of the types and numbers of

radiac instruments employed by TG 7.3 has not been found.

Evidently

neither the AN/PDR-39 instrument nor the similar AN/PDR~T1B was issu

(Reference ll, p. 11B-1). The primary instrument for TG 7.3 was the
AN/PDR-27F, with the AN/PDR-18A available for use in higher radiatio
fields

(Reference ll, p. 115).

100

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