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health and safety laboratory - Digital Collections

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I I I<br />

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I I<br />

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I<br />

I I<br />

I I<br />

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SUMMARY<br />

While the gummed film network fulfilled its original purpose of de<br />

lineating fallout patterns, this report has been devoted to the extension of<br />

QQ<br />

the p activity measurements to the estimation of Sr7 deposition <strong>and</strong> infinity<br />

gamma dose. The computations have been based on a simple model, but yield<br />

90<br />

Sr estimates that are generally within a factor of two from measured values.<br />

It would be possible to improve the gummed film estimates by adopting<br />

a more sophisticated model, but the added cost would not be justified. The<br />

present results have required much greater effort than was expected <strong>and</strong> have<br />

appeared more slowly than was hoped.<br />

90<br />

The gummed film Sr estimates are lower in most cases than the<br />

measured values at nearby sampling sites. The deviation is probably a com<br />

bination of many effects:<br />

1. The estimate of Sr yield may be low, particularly for fraction<br />

ated, debris, where long range fallout is enriched in this nuclide.<br />

2. The gummed film efficiency is variable <strong>and</strong> is probably lowest<br />

during heavy rainfalls when a large fraction of the Sr^O is<br />

deposited.<br />

3. The gummed film efficiency continues to decrease in the absence<br />

of large scale tests, for the percentage of long-lived Sr^° <strong>and</strong><br />

Cs 1^ increases <strong>and</strong> their retention is poor.<br />

4. The present model is poor during periods of repeated high yield<br />

tests, as there is no delay'included for arrival time from either<br />

the troposphere or stratosphere. The debris is thus always con<br />

sidered to be fresher than the actual fallout.<br />

The results presented in this report have some value in the absence<br />

of direct measurements. While it is not possible to evaluate all situations,<br />

the data may be used for geographic interpolation between stations where Sry<br />

*»<br />

results are available. It is also possible to make reasonable estimates for<br />

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