SLIDE 10
Analysis of samples.
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Soil samples were analyzed for

127, 129; I, 125g, Sb; 137gg

The methods used for neutron activation analysis were

described by Braver (Br74) and Keisch (Ke65). Todine was separated from soils
according to the method of Studier (St62). Once separated, the iodine was
irradiated with neutrons in a nuclear reactor, purified to reduce levels of

interfering nuclides and then measured by gamma spectroscopy (Br80).

In order

to perform quality control, comparison samples containing known amounts of
1257 1275 and 1297 were irradiated with each set of fodine samples isolated

from Marshall Islands' soil.

Following irradiation the Llodine samples were further purified and then
precipitated onto the detecting media.
The number of atoms of activated

nuclide were determined by gamma spectroscopy measurements of the
radioactivity produced in the soil sample and in a comparison sample.

The

number of initial comparison atoms and resulting comparison activity were used

to determine a production ratio. The production ratio was applied to the soil
sample activity and the number of atoms of activated nuclide per gram of soil

was estimated.
Corrections to the soil activity were made based on results
for soil sample blanks, comparison sample blanks and method yield.
Individual
counting errors were normally less than 5% although a few samples approached

20%. A least squares fitting was performed on results for nuclide soil
activity per unit soil mass vs days post detonation using linear, exponential,
logarithmic and power function models. Sample results varied from their best

fit value by as mich as a factor of 9 and by an average factor of 2.5 over the

period 1955 to 1977.

The best fitting function was determined based on a comparison, gf the
coefficient of determination for each modé hy Functions used with
I results
for Rongelap soil are plotted here. For
I soil results, the best fitting
function was exponential. All four fitting functions were generally useful in
predicting soil activity per gram at times after 600 days post BRAVO for all

nuclides.

Significant departure between functions occurs during the period

several hours out to one year post BRAVO. For example, at 0.5 days the
difference between,fhe exponential and power function estimates spans 5 orders
of magnitude for
I.

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