se
mation*of sr,

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Measurements have been made to determine the existing

levels at the earth's surface, the quantity stored in the stratosphere, and
the deposition rate.

Samples of fallout have been taken from the soil and

vegetation, by gummed tape and pot-type collectors on the ground,and by
air-filter samplers at the surface and in the troposphere and stratosphere
(References 8, 23, 39, 40, 41, 42, 43, 44, 45),
Based on this work, it was estimated in the fall of 1956 that the

sr 7° levels were about 22 me /mi? in the midwestern section of the United
States, 15-17 me /mi* for similar latitudes elsewhere and perhaps 3-4

mc/mi® for the rest of the world (References 38, 39 }»

The total amount /

in the stratospheric reservoir, if uniformly distributed over the area of
the globe, would increase these figures by about 12 me/mi*,

The deposi-

tion rate of the stored material was considered to be around 10% per
annum,

It was further estimated that if these levels were maintained for

fifteen years the concentration in the human skeleton would be about 1%
of the maximum permissible (Reference 24),
The quantity of radioactivity in the storage reservoir was estimated by summation of the contributions of all the bursts through Operation
REDWING which have deposited debris in the stratosphere,

The available

fraction of the weapon was determined by subtracting the local and intermediate fallout from the total,

The intermediate fallout is thought to

SAN BRONO FRG

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