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INSTRUMENTATION,

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DATA COLLECTION AND ANALYSIS

A high pressure ionization chamber and a y-ray spectrometer system were used to obtain’ in situ exposure rates and
spectra.
The spectra were then analyzed to determine the
individual exposure rates contributed by each major y-ray
emitting isotope in the soil.
Because of the bulk and
weight of the analyzer system, ionization chamber, and
related power supplies, and the resultant difficulty in trarsporting the equipment from the ship via small boats to the
shore and thence in many cases through heavy brush to a
survey site, these types of measurements were limited to 16
sites on the three major islands.
In ail some 29 field
spectra were abtained.
A small scintillation counter survey meter and a number
of rugged G-M counter survey meters were used to extend the
total exposure rate measurements over these islands and to
survey the smaller islands.
Although the data obtained with

these instruments is less accurate for a particular location,

their use enabled us to extend our measurements over a fairly
large area convenientiy and consequently obtain a more
complete picture of the variation of radiation levels across
the major islands and from island to island.
In addition to these measurements, thermoluminescent
dosimeters were placed at a large number of locations on
Bikini and Eneu Islands at the beginning of the survey and
collected about ten days later and returned to the United
States for readout.
These passive dosimeters were employed
to provide an independent check on the data obtained with
the other instrumentation.
Soil samples were also taken at various locations
exhibiting unusually high or low activity.
All of these
samples were returned to the United States for laboratory
analysis, however, several were also spectrally analyzed on

our 4 in. x 4 in.

NaI(T1) detector aboard ship to obtain

identification of the major y-ray emitters in the sample.
At several locations a complete depth profile set of SQibtay
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