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I.

EXTERNAL GAMMA RADIATION

Gamma dose rates were taken periodically on several islands in
the Pacific over a time ranging from about two days to over two years.
The attached map is an estimate of the gamma dose rates at three feet
above the ground at D+ 1 (one day after the detonation).

A very rough

approximation of the degree of contamination may be made by dividing
these readings by four to arrive at units of gamma megacuries per

square mile.

(The beta to gamma ratio varies with time but at one

day may be near unity, so these values may also be thought of beta
activities.)

However, the gamma dose rates do indicate the relative

degrees of contamination on the islands and therefore are useful in this
respect when evaluating the data in subsequent sections of this report.
Graph One shows the decay with time of gamma dose rates on
the Island of Rongelap.

Similar decay curves were found on other

islands in the Atoll and in nearby Atolls (Ailinginae and Rongerik).

The decay of activity of mixed fission products is assumed to follow
(tame) 7°" principle.

atoms.

This is intended to apply to disintegrations of

However, in estimating the reduction of gamma dose rates above

a plane with time there must be considered the changing numbers and
energy spectra of gamma photons released per disintegration, and the
effects of weathering.

When computing the infinity radiation doses from

fallout that occurs within afew hours after detonation, integration of
the (time )71** curve gives a fair approximation since most of this total
dose is accumulated during the early periods when this curve lies near
the theoretical gamma decay curve.

However, in extrapolating by (time)7??

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