-3Experience has shown that an atomic device ex-

ploded on the surface distributes about 80 percent of its
fission products on the ground within a few hundred miles
of the burst point. A somewhat larger percentage takes.

part in the close-in fallout from an underground burst,

and a smaller percentage will be scavenged from a near-~
surface burst or tower shot.

The tower shot is, in a sense, a special case
of a surface burst, since the material of the tower it-

self is mixed with the fission products in the fireball
to a greater or lesser degree, depending on the yield.

Experience with tower shots indicates that even in cases
where the fireball does not touch the ground a few percent of the radioactive fission products come down as
close-in fallout.

The fraction which takes part in the close-in
fallout from a surface burst over deep ocean water appears to be somewhere between 20 and 50 percent. This
is less than the fraction of close-in fallout occurring
from a corresponding surface burst over land, due to the
evaporation of many of the drops before they reach the
ground. Presumably this fraction is also affected by
the prevailing humidity and temperature structure of

the atmosphere through which the drops must fall. As

the depth of the water is decreased, the point is
reached where the fireball extends downward to the
bottom and picks up bottom material.
In such shallow
water one would expect a higher percentage of close-in

fallout than in deep water. Experience in the Pacific
indicates that such is indeed the case, and that in fact
there would be very little difference in the fallout
between a large-yield device in very shallow water and
a true surface shot.2/

The second type of fallout is the material

which, though not coarse enough to fall of its own

weight in the first few hours, is, nevertheless, left
in the lower layer of the atmosphere, known as the
troposphere, where ordinary weather phenomena occur.

l/ "Close-In Fallout," W. W. Kellogg, R. R. Rapp, and
S. M. Greenfield, P-822-AEC, March 12, 1956.
(more)

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