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1 1 11<br />

1<br />

stations having only gummed film sampling by the use of a regional Pot/Gummed<br />

Film factor. As an example, the following table was developed from the north<br />

ern hemisphere stations where pot data were collected.<br />

Average Pot/Gummed Film Ratios for the Northern Hemisohere<br />

1 11I11ii<br />

Month 1957 1938<br />

Jan, 1.4 1.6<br />

Feb. 1.3 1.8<br />

Mar, 1.2 1.1<br />

Apr. 1.4 1.0<br />

May .9 1.6<br />

June 1.0 2.4<br />

July 1.1 1.2<br />

Aug. .7 2.1<br />

Sept. .5 2.3<br />

Oct. .7 2.0<br />

Nov. 1.3 2.0<br />

Dec. 1.1 2.5<br />

Mean Ratio 1.0 1.8<br />

These average ratio factors can still yield<br />

Ig59<br />

2.1<br />

2.0<br />

2.8<br />

2.1<br />

1.6<br />

2.5<br />

2.6<br />

1.9<br />

1.5<br />

2.1<br />

2.4<br />

3.5<br />

2.3<br />

only an approximation <strong>and</strong><br />

while the second is approximately T+0 * 7^ for the first year <strong>and</strong> T * therei<br />

iiii<br />

probably hold only for the northern hemisphere.<br />

There is some justification for applying the<br />

finity gamma dose data as well. Most of the errors<br />

same factors to the incan<br />

be divided into two<br />

classes , poor collection of fission products <strong>and</strong> those involved in the model<br />

90<br />

computation. Poor collection would affect the Sr <strong>and</strong> 7 dose values equally.<br />

The computation model is equivalent except for the<br />

QO<br />

factors of % Sr , <strong>and</strong> of<br />

7 disintegrations per p dpm. The first is approximately at T * function,<br />

after. Thus, the average Pot/Film ratio may be a reasonable correction factor<br />

There has been no attempt in this report to<br />

90<br />

distribution of Sr 7 . The data do not warrant this , as soil <strong>and</strong> pot analyses<br />

are more reliable for this purpose.<br />

depict the geographical<br />

- 31 -

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